HomeMy WebLinkAbout20120182 Ver 1_Mitigation Plan draft final_20120104Confluence Engineering, PC
16 Broad Street
Asheville, NC 28801
828.255.5530
TRANSMITTAL
Date: November 30, 2011
To: Julie Cahill, EEP
5 Ravenscroft Dr.
Asheville, NC 28801
Subject: Hogan Creek Mitigation Project
DENR Contract Number 090856601
H U C 03040101
Surry County, North Carolina
No. Date Description
1 12/11 r)df of Draft Final Mitiaation Plan
Julie — thanks for the comments on the Draft Mitigation Plan, sent on November
18. We have revised the document to address the comments and we trust that
the revisions do not warrant further explanation. Please note that some of the
information in the appendices has changed, notably the geomorphic summary
tables and the cover sheet of the preliminary plans.
If you have any questions or comments before sending to the agency review
team, please call me at 255.5530, x 19.
Thanks.
Andrew Bick, PE
MITIGATION PLAN — DRAFT FINAL
Hogan Creek Stream Mitigation Project
Surry County, North Carolina
EEP Project No. 94708
Upper Yadkin River Basin
Cataloging Unit 03040101
Prepared for:
r"';J
Fcowstem
..-',n a ement
PROGRAM
NC Department of Environment and Natural Resources
Ecosystem Enhancement Program
1652 Mail Service Center
Raleigh, NC 27699 -1652
December 2011
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
MITIGATION PLAN — DRAFT FINAL
Hogan Creek Stream Mitigation Project
Surry County, North Carolina
EEP Project No. 94708
Upper Yadkin River Basin
Cataloging Unit 03040101
Prepared for:
E ios stem
anmement
PROGRAM
NC Department of Environment and Natural Resources
Ecosystem Enhancement Program
1652 Mail Service Center
Raleigh, NC 27699 -1652
Prepared by:
Confluence Engineering, PC
16 Broad Street
Asheville, NC 28801
828.255.5530
December 2011
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
EXECUTIVE SUMMARY
The NCDENR Ecosystem Enhancement Program (EEP) provides off -site compensatory wetland and
stream mitigation to private sector, state government agencies, municipalities, schools, military bases and
other applicants through its In Lieu Fee Programs. EEP is proposing the Hogan Creek Stream Mitigation
Project (project) to help fulfill stream mitigation requirements accepted by this program for the Upper
Yadkin River Basin (CU 03040101). Through this project, EEP proposes to restore and enhance
approximately 4,109 linear feet (LF) of Hogan Creek and three unnamed tributaries (UTs), provide
livestock fencing and alternative water sources to keep livestock out of the streams, remove invasive
plant species across the project, establish native riparian buffers, and preserve approximately 5,673 LF of
relatively un- impacted forested streams. Based on preliminary estimates from the design proposed in this
Mitigation Plan, the Hogan Creek Stream Mitigation Project will net 4,994 stream mitigation credits
through a combination of restoration, enhancement I and II, and preservation.
This Mitigation Plan describes specific project goals and objectives as they relate to EEP's programmatic
goals (watershed planning -based mitigation), provides baseline data on the existing conditions of Hogan
Creek and its UTs at the project site, and describes the methodologies that were used develop the
preliminary design. The Mitigation Plan also outlines the performance standards and monitoring protocol
that will be used to evaluate the project's success, and it details long term management strategies for
protecting and maintaining the restoration site in perpetuity.
This Mitigation Plan has been written in conformance with the requirements of the following:
• Federal rule for compensatory mitigation project sites as described in the Federal
Register Title 33 Navigation and Navigable Waters Volume 3 Chapter 2 Section § 332.8
paragraphs (c)(2) through (c)(14).
• EEP In -Lieu Fee Instrument signed and dated July 28, 2010
These documents govern EEP operations and procedures for the delivery of compensatory mitigation.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
TABLE OF CONTENTS
1.0
RESTORATION PROJECT GOALS AND OBJECTIVES ....................................... ..............................1
2.0
SITE SELECTION .......................................................................................................... ..............................2
2.1
DIRECTIONS TO SITE .......................................................................................................... ..............................2
2.2
HISTORICAL CONDITIONS AND FUTt?RE LAND USE TRENDS .............................................. ..............................2
2.3
SITE MODIFICATIONS, STRESSORS AND ECOLOGICAL SERVICES ........................................ ..............................9
2.4
E\-OLUTIONARY TRENDS ................................................................................................... ..............................9
2.5
PROJECT SITE PHOTOGRAPHS ............................................................................................ .............................12
3.0
SITE PROTECTION INSTRUMENT ........................................................................... .............................14
4.0
BASELINE INFORMATION ......................................................................................... .............................16
5.0
DETERMINATION OF CREDITS ............................................................................... .............................17
6.0
CREDIT RELEASE SCHEDULE ................................................................................ .............................18
6.1
INITIAL ALLOCATION OF RELEASED CREDITS ................................................................... .............................18
6.2
SUBSEQUENT CREDIT RELEASES ....................................................................................... .............................18
7.0
MITIGATION WORK PLAN ......................................................................................... .............................19
7.1
TARGET STREA1\IS ............................................................................................................. .............................19
7.2
TARGET PLANT CO1\I1\IUNITIES ......................................................................................... .............................20
7.3
DESIGN METHODOLOGY AND DATA ANALYSES ............................................................... .............................20
7.3.1 Design Discharge .............................................................................................. .............................20
7.3.2 Sediment Transport ........................................................................................... .............................21
7.3.3 Cross Section ..................................................................................................... .............................21
7.3.4 Plan and Profile .................................................................................................. .............................22
7.3.5 In- Stream Structures ......................................................................................... .............................23
8.0
MAINTENANCE PLAN ................................................................................................ .............................23
9.0
PERFORMANCE STANDARDS ................................................................................. .............................24
10.0
MONITORING REQUIREMENTS ............................................................................... .............................25
11.0
LONG -TERM MANAGEMENT PLAN ........................................................................ .............................25
12.0
ADAPTIVE MANAGEMENT PLAN ............................................................................ .............................26
13.0
FINANCIAL ASSURANCES ....................................................................................... .............................26
14.0
DEFINITIONS ................................................................................................................. .............................26
15.0
REFERENCES ............................................................................................................... .............................27
APPENDIX A: SITE PROTECTION INSTRUMENTS
APPENDIX B: BASELINE INFORMATION
APPENDIX C: MITIGATION WORK PLAN DATA AND ANALYSES
APPENDIX D: PRELIMINARY PLANS
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
1.0 RESTORATION PROJECT GOALS AND OBJECTIVES
The EEP develops River Basin Restoration Priorities (RBRP) to guide its restoration activities within each
of the state's 54 cataloging units. RBRPs delineate specific watersheds that exhibit both the need and
opportunity for wetland, stream and riparian buffer restoration. These watersheds are called Targeted
Local Watersheds (TLWs) and receive priority for EEP planning and restoration project funds.
The 2009 Upper Yadkin RBRB Restoration Priorities
(www.nceep.net /services /restplans /Upper Yadkin RBRP 2009.pdf identified the Candiff Creek /Hogan
Creek 14 -digit HUC 03040101110060 as a TLW due to water quality and habitat impacts from past and
present agricultural practices. Agriculture is the primary land use in the watershed (41 % agriculture land
cover) and the RBRP identified non - forested buffers and livestock operations as major stressors to water
quality. There are 26 permitted animal operations and 25% of the watershed has non - forested riparian
buffers. The site assessment phase of the project identified other stressors as well, including bank
erosion, sediment deposition, disconnection of the streams and floodplains, and exotic plant species.
The project was identified as an opportunity to improve water quality and aquatic and terrestrial habitats
within the TLW. In addition to being within an EEP TLW, the upper Hogan Creek subwatershed has been
identified as a priority area for stream restoration and agricultural BMPs as part of EEP's initial Ararat
River Local Watershed Planning (LWP) effort (EcoEngineering, 2008).
The project goals address stressors identified in the TLW and LWP priority subwatershed, and include the
following:
• Improve water quality in Hogan Creek and the UTs through reductions in sediment and nutrient
inputs from local sources;
• Create conditions for dynamic equilibrium of water and sediment movement between the supply
reaches and project reaches;
• Promote floodwater attenuation and secondary functions associated with more frequent and
extensive floodwater contact times;
• Improve in- stream habitat by increasing the diversity of bedform features;
• Enhance and protect native riparian vegetation communities; and
• Reduce fecal, nutrient, and sediment loads to project streams by promoting and implementing
livestock best management practices.
The project goals will be addressed through the following project objectives:
• Restoration of the dimension, pattern, profile of approximately 2,493 LF (proposed) of Hogan
Creek and two UTs;
• Restoration of the dimension and profile (Enhancement 1) of approximately 1,200 LF of Hogan
Creek;
• Limited channel work coupled with livestock exclusion and /or invasive species control
(Enhancement 11) on approximately 416 LF along two UT;
• Livestock exclusion fencing and alternative water source installations;
• Invasive plant species control measures across the entire project wherever necessary; and
• Preservation of approximately 5,673 LF relatively un- impacted forested streams in permanent
conservation easement.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
1
2.0 SITE SELECTION
2.1 Directions to Site
The Hogan Creek project site (Figure 1) is located southeast of Level Cross in Surry County, North
Carolina. The site is accessed from 1 -77 north out of Statesville. Turn east off 1 -77 at exit 85 (NC 268
Bypass) and travel approximately 3 miles to the intersection with NC 268. Turn east and travel
approximately 12 miles to a south turn onto Miller Gap Road (SR2088). The site is located approximately
2 miles south of NC 268 on Miller Gap Road, which bisects the project site at the bridge over Hogan
Creek. The project site is bordered to the north by Trajan Trail, to the south by Anderson Road, and to
the west by Siloam Road. Latitude and longitude for the site are 36.321609 N and 80.602389 W,
respectively.
2.2 Historical Conditions and Future Land Use Trends
Reference is made in the following discussions to project reaches and design stationing as shown on the
attached preliminary plans (Appendix D). The project site falls within two parcels owned by Marion
Chilton and Marion H. Chilton, Jr. encompassing a total of 179 acres. The Chiltons currently operate a
cattle farm on the two parcels. The majority of the cattle operations take place on a 25 -acre field with
barns on the northeast side of Miller Gap Road and on a 13 -acre field on the opposite side of the road.
The site also includes seven 1 to 3 -acre fields scattered around the parcels that are accessed by farm
paths. The total cleared area measures approximately 56 acres (about one -third of the total land area).
Based on a review of an aerial photograph of the project site from 1966 (Figure 6), the left floodplain of
Hogan Creek upstream of Miller Gap Road and both floodplains downstream of the road have been
maintained as field or pasture for over 50 years. A row of mature trees, generally one stem wide, has
been present along the left bank of Hogan Creek upstream of the road and on both banks downstream of
the road during this period. Aerial photographs from 1966 through 2010 (Figures 4 through 6) indicate
that land use practices and the extent of cleared land at the project site have remained consistent over
the past five decades.
Based on the series of aerial photographs, the right bank of Hogan Creek between the upstream project
limits and the confluence with UT2 has been forested over this same time period, as has the UT1 valley
and the upstream 90 percent of the UT3 valley. The age of the trees (estimated at roughly 50 years for a
12 -inch diameter oak, growth factor of 4) in these upland areas supports this conclusion.
The existing Hogan Creek crossing at Miller Gap Road is a triple 7 -foot by 9.5 -foot CMP arch culvert with
concrete headwalls. Based on the relatively large size and good condition of the crossing, it appears to
have been constructed within the past twenty years. The alignment of Miller Gap Road has not changed
since at least 1966.
Invasive plant species, particularly kudzu, are a significant problem at the site. Hogan Creek between
Stations 20 +00 and 30 +00 and UT2 between Stations 10 +00 and 15 +50 are the reaches most severely
impacted; kudzu is the dominant ground cover and has infested most of the canopy trees in these areas.
A recent infestation of kudzu was noted encroaching into the wooded upstream reach of UT3.
In October 2006, Surry County issued Land Use Plan 2015 which describes growth, land use changes
and future development policies through 2015. The Hogan Creek site is located in a rural land use area
and this land use classification extends four miles or more in all directions from the site, inclusive of the
Hogan Creek project catchment (Figure 2). According to the 2015 plan, the best use of land within the
Hogan Creek watershed will be agriculture, low density residential, forestry and other similar practices.
Technical Memorandum Task 2, Upper Yadkin Basin Local Watershed Plan (EcoEngineering, 2008)
identified the Hogan Creek sub - watershed as a high priority for stream restoration because of its low
population density and agricultural land uses. Current and projected future land use for this watershed
supports an investment in restoration at this site.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
I" fL w
KEY:
R - RESTORATION
EI - ENHANCEMENTI
EII - ENHANCEMENT II
P - PRESERVATION
SEMENT
780UNDARY
w
0'
400° 800' 12W
PARCEL
W R1 (EI) \
HOG (R)
1
� HOGAN R3 (R)
U. 31(R)
9"r
:Ell) UT3-(P)
I
f
IMAGE DATE: 2010
As Shown Hogan Creek Restoration Figure 1: Site Vicinity Map
Surry County, NC
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
3
NIJ
. tN�
1
1-
,��� Hill.
rckss
Q I �
6 C
1�
D B. DARY - }
Z�L
PAk6EL BOUNDARY ✓. ,� � } / J e
If
®r
-
-
rr �� •n_,
is � •. � it -•4�;, �_�' _1 �� � � �a � _ ^ T
Scale: 1" = 2,000' Hogan Creek Restoration Figure 2: Watershed Map
Surry County, NC
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
4
3$119471
36' IV SW'
Soil Map--Surry Ccunty, Ncrtb Carol ina
[Hogan Creek Site]
Map Sale. 5.8,690 if priniaa or T .4c (8.6'x ' 1" I —L
de L
N Meters
0 e11 100 200 390 w
F991
0 200 400 800 1,200
USDA Natural Resources Web Soil Survey 9176!2017
Conservation Service National Cooperative Sail Survey Page t of 3
V1- I P1421
36'18'.f'
Scale: As Shown Hogan Creek Restoration Surry Figure 3: Soils Map
County, NC
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
Scale: As Shown Hogan Creek Restoration Surry Figure 4: Current Conditions
County, NC (2010 Aerial)
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
Scale: As Shown Hogan Creek Restoration Surry Figure 5: Historical Conditions
County, NC (1982 Aerial)
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
J
1
h
A6
f
i
i
• 7
r � �
Site Location
a
r�
Legend
:4
Parcels f
0 500
1,000 2,000 3,000
Map Production Date -
August 2011
Feet
Scale: As Shown
Hogan Creek Restoration
Figure 6: Historical Conditions
Surry County, NC
(1966 Aerial)
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
2.3 Site Modifications, Stressors and Ecological Services
Throughout the project area site modifications have diminished the ecological services provided by
riparian buffers and adjacent floodplains. Farming operations over the past several decades have
deforested riparian buffers, a water quality and habitat stressor identified for this TLW. The creeks and
adjacent floodplain areas have also been impacted by levee construction. A prominent levee, measuring
up to 3 feet above the adjacent floodplain, exists along the left bank of Hogan Creek Reach 1 and on the
right bank in Reach 2. Another levee, aligned perpendicular to Hogan Creek near Station 21 +20, is
present on the left floodplain; the landowners indicted that this perpendicular levee was constructed
several decades ago to provide flood relief to the downstream reach.
Three -foot high levees are present on both banks of UT3 between a culvert on a farm road at Station
10 +20 and the confluence with Hogan Creek. In addition to restricting floodplain access on UT3, the
levees constitute a significant pinch point in the Hogan Creek floodplain. Judging from the low sinuosity
of this downstream reach relative to the sinuosity of the less disturbed upstream reach, the alignment of
UT3 appears to have been straightened when the levees were constructed.
Widespread bank erosion, identified as a major stressor in this TLW, is visible throughout Hogan Creek
and within the impacted reaches of the UTs. A clear -span bridge is present on a farm road over UT2
near station 14 +00 and erosion on the left bank of UT2 threatens the stability of this road near station
10 +50.
A well supplies water to cattle adjacent to Hogan Creek Reach 2 and livestock fencing is present along
the left bank of Hogan Creek between the upstream property line and station 16 +50, along both banks
within Reach 2 and on UT2 upstream of Station 12 +50. However, cattle have direct access to Hogan
Creek Reach 1 and the downstream end of UT2, exacerbating bank erosion and allowing direct nutrient
and fecal inputs to the stream. Table 1 provides a summary of stressors and ecological services needing
enhancement in this project area.
Table 1. Stressors and Proposed Ecological Service Enhancements
Stressor
Ecological Services Needing Enhancement
Levees disconnecting streams
from floodplains
Flood attenuation, fine sediment storage, maintenance of
stable channel bed and banks
Bank erosion and mid - channel
sediment deposition
Equilibrium sediment transport, maintenance of in- stream riffle
and pool habitats
Buffer deforestation
Filtration of runoff, thermal regulation, input of organic matter
Invasive, exotic vegetation
Riparian buffer habitat, species diversity
Direct livestock access to streams
Protection of water quality from nutrient inputs.
2.4 Evolutionary Trends
Reach 1 of Hogan Creek generally flows through the low point of its valley, and judging by valley
topography, it does not appear that the channel position within the valley was altered significantly during
the levee construction activities. It does appear that the bankfull channel alignment and cross sectional
dimensions were modified enough to create bank stability and sediment transport problems. In Reach 2
of Hogan Creek, the topography indicates that the low point of the valley is 60 to 80 feet south of the
current channel alignment; it appears that the channel was shifted north at some time prior to 1966. This
conclusion is supported by data from three hand auger borings in the low area of the right floodplain,
which encountered gravel indicative of the one -time creek bed at depths of 3 to 4 feet below existing
grade.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
Hogan Creek appears to be near the midpoint of a trend from a C -type steam to an F -type stream, as
evidenced by the following (refer to project site photographs, section 2.5):
• Bank erosion;
• Leaning and fallen trees;
• Channel cross sectional areas up to twice the estimated bankfull areas;
• Bank heights up to twice the bankfull depth; and
• Mid - channel sediment bars.
Bedrock is visible in the channel bed throughout much of Hogan Creek and the tributaries. Exposed
rocks appear to be gneisses and schists. The Soil Survey of Surry County indicates most of the rock in
the area strikes northeast- southwest and dips northwest. This attitude of the rock is not apparent from
surface observations of the stream pattern or topography; the shape and alignment Hogan Creek and
tributary valleys appear to have been governed by rocky hillsides, which are evident in the topography.
Soils on the Hogan Creek floodplain are mapped as the Colvard series, described in the soil survey as a
fine sandy loam originating from recent alluvium with a depth to bedrock generally more than 5 feet. Soils
in the tributary valleys are mapped as the Fairview series, described as a clayey loam and the product of
in -situ weathering; the depth to bedrock in the Fairview series is indicated to be more than 5 feet. The
soil survey provides general information about soils but it cannot describe reach -scale historic alluvial
deposits, isolated bedrock outcrops and other geologic influences.
The aforementioned bedrock has prevented channel down - cutting; incised channel conditions are the
result of the levees, which have restricted floodplain access and confined flows greater than bankfull to
within the channel. The confinement of these large flows has lead to bank erosion, which in turn has lead
to channel widening, mid - channel sediment deposition and loss of near -bank vegetation. Left unchecked,
this process of widening and mid - channel deposition will likely continue as leaning trees fall and expose
erodible soils. The evolutionary trend suggests that the stream will migrate laterally and breach the
levees until the system eventually reaches equilibrium with its water and sediment supply. Evidence of
this process at work can be found in a short meander bend between Stations 21 +00 and 24 +00.
Observations of recent bank slumping and review of aerial photographs (1982 and 2010) indicate that the
channel has eroded roughly 10 feet into the left bank. This response of lateral migration is evident in an
area that is devoid of mature trees and their stabilizing root masses. Similar meander bends would likely
be evident elsewhere, if not for some remaining mature trees on the banks. Appendix C includes an
inventory drawing showing areas of significant bank erosion, tree falls, debris jams, and mid - channel and
lateral bars. Judging by the fresh conditions of the wood, most of the tree falls shown on the inventory
appear to have occurred within the last year or two. In the 14 months since the initial site visit, new tree
falls have been observed in both reaches of Hogan Creek and bars have shifted in size and shape; these
are both indications that the stream is not close to reaching a state of dynamic equilibrium.
UT1, UT2 and UT3 are similar to each other in terms of valley and channel slope. Each of these
tributaries has formed a sinuous pattern within a confined valley. The belt widths of these streams
appear to be governed by bedrock at the valley walls. Observations of bank soil profiles in Hogan Creek
reveal a buried topsoil layer is present about 2 feet below existing grade, indicating that the Hogan Creek
valley was subjected to significant aggradation, likely from surface erosion following initial land
disturbances in the 19th century. Under this scenario, the tributaries were also subjected to this
aggradation process and observations of fine - grained soils in the tributary banks generally support this
idea. The highly sinuous tributary patterns may be a response to large volumes of deposited sediment
filling the valleys. The forest in the upstream reaches of these tributaries appears to have recovered
significantly since initial disturbance and the streams are generally stable, aided by deep rooted
vegetation and frequent bedrock outcrops at the valley walls.
Over the downstream 100 LF of UT1, the stream makes a tight meander bend through a highly incised
reach (bank heights at least twice the bankfull maximum depth) as the tributary reaches its confluence
with Hogan Creek. Observations of active bank erosion indicate that this downstream reach is likely to
avulse without intervention.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
10
Upstream of station 6 +50 on UT2, the stream is highly sinuous and generally stable, with isolated bank
erosion at the outside of some meander bends. Between stations 6 +50 and 11 +00, the valley is confined
topographically and by the aforementioned farm road, which was constructed on the left hill slope. Bank
erosion near Station 10 +50 has caused the partial collapse of the road and a 40 -foot length of fencing
along the road is currently suspended in air. Between Stations 11 +00 and the confluence with Hogan
Creek, the UT2 channel is incised with bank heights of twice the bankfull maximum depth, and the buffer
is dominated by kudzu. The reach of UT2 downstream of Station 10 +00 lacks the appropriate
geomorphic characteristics and buffer vegetation to heal itself without first causing widespread bank
erosion.
Instability within the UT3 system begins upstream of an 18 -inch culvert on a farm road near station
10 +20; the banks immediately upstream of the culvert are unstable, apparently due to culvert effects on
flow. Downstream of the culvert, bank heights are up to 4 feet higher than the estimated bankfull
maximum depth due to the aforementioned levees. This high level of incision has resulted in a very low
frequency of floodplain access and flows reaching levee elevations are producing bed shear stress more
than twice that estimated for bankfull. The downstream reach of UT3 will not regain floodplain access
and heal to a stable dimension, pattern and profile without the removal of the levees and restoration of
the appropriate geomorphic characteristics.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
11
2.5 Project Site Photographs
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
12
r
Hogan Creek, looking downstream from
Agricultural field and levee looking downstream
station 12 +50; bank erosion and mid - channel
along left bank of Hogan Creek from station
bar deposition; March 8, 2011
14 +00; March 8, 2011
,k.
pia
Hogan Creek, looking downstream from
Hogan Creek, looking downstream at station
station 16 +00; leaning trees, bank erosion;
22 +50; lateral migration, mid - channel bar
mid - channel bar; September 12, 2011
deposition; October 18, 2010
r.
ti •a
Hogan Creek, looking downstream from
Hogan Creek, looking downstream from station
station 27 +25; buffer deforestation and
33 +75; narrow buffers; levee on right bank;
kudzu infestation; March 8, 2011
March 8, 2011
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
12
Hogan Creek looking downstream from
station 35 +00; bank erosion and mid - channel
deposition; April 8, 2011
UT1 looking upstream from station'! 0+00 at
downstream end of preservation reach;
April 8, 2011
UT2, looking downstream from station
10 +50; bank erosion threatening farm road
on left; April 8, 2011
UT1 looking downstream from station'! 0+00;
bank erosion at confluence with Hogan Creek;
March 8, 2011
UT2, looking downstream from station 12 +50;
buffer deforestation and kudzu infestation;
March 8, 2011
UT3, looking downstream from station 11 +00.
Straightened channel with levees on both banks;
March 8, 2011
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
13
3.0 SITE PROTECTION INSTRUMENT
The land required for the construction, management, and stewardship of this mitigation project includes
portions of the following parcels. A copy of the land protection instrument(s) will be included in Appendix
A upon completion of the documents.
Table 2: Summary of Project Land Parcels and Site Protection Instruments
Parcel
Site
Deed Book
Acreage
ID
Landowner
PIN
County
Protection
and Page
protected
Instrument
Number
Parcel A
Chilton, Marion
5924 -00 -80 -2896
Surry
Conservation
TBD
17.4 ac
Easement
Parcel 131
Chilton, Marion H. Jr.
5923 -00 -79 -9259
Surry
Conservation
TBD
13.5 ac
Easement
All site protection instruments require 60 -day advance notification to the Corps and the State prior to any
action to void, amend, or modify the document. No such action shall take place unless approved by the
State.
Figure 7 shows the current parcel boundaries and the proposed conservation easement boundaries.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
14
_* I 'r ;
r -
A L
a'� f PARCEL BOUNDA
y F \ \
EASEMENT\ HOGAN CREEK
BOUNDARY
L
UT1 ^- ,
awl
9
r�
VT2
e�
r
If
w
0' 400' 800' 1200'
z IMAGE DATE: 2010'
Scale: As Shown Hogan Creek Restoration Figure 7: Site Protection
Surry County, NC Instrument Boundaries
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
15
4.0 BASELINE INFORMATION
Table 3: Project Baseline Information
Project Name Hogan Creek Restoration
County Surry
Project Area (acres) 40 (conservation and temporary construction easements)
Project Coordinates (latitude and longitude) 36.321609 N, 80.602389 W
Project Watershed Summary Information
Physiographic Province Piedmont
River Basin Yadkin
USGS Hydrologic Unit 8 -digit 03040101
USGS Hydrologic Unit 14 -digit 03040101110060
DWQ Sub -basin Pee Dee River Subbasin 03 -07 -02
Project Drainage Area (acres) 1,514 ac (2.37 mil)
Project Drainage Area Percentage of Impervious Area 0.4%
CGIA Land Use Classification Managed Herbaceous Cover, Broadleaf Deciduous Forest Land
Reach Summary Information
Parameters
Reach 1
Hogan Creek
Reach 2
Hogan Creek
Main Stem
UT1
Main Stem
UT2
UT3
Existing length of reach (LF)
2,128
876
1,395
2,983
1,223
Valley classification (Rosgen)
VIII
VIII
VI
VI
VI
Drainage area (acres)
1,479
1,514
60
81
18
NCDWQ stream identification score
40
37
31
31.5
32.5
NCDWQ Water Quality Classification
C
C
C
C
C
Morphological Description (Rosgen
stream type)
C4
C4
E4b
E4b
G4
Evolutionary trend
C -F
C -F
Eb -G
Eb -G
Eb -G
Underlying mapped soils
CsA
CsA
CsA, FsE
FsE
FsE
Drainage class
well drained
well drained
well drained
well drained
well drained
Soil Hydric status
not hydric
not hydric
not hydric
not hydric
not hydric
Slope
0.007
0.005
0.031
0.021
0.030
FEMA classification
AE
AE
Not in SFHA
Not in SFHA
Not in SFHA
Native vegetation community
Felsic Mesic
Forest
Felsic Mesic
Forest
Felsic Mesic
Forest
Felsic Mesic
Forest
Felsic Mesic
Forest
Percent composition of exotic
invasive vegetation
40
10
<10
40
20
Wetland Summary Information
Parameters
Wetland 1
Wetland 2
Wetland 3
Wetland 4
Size of Wetland (acres)
0.09
0.02
0.13
0.1
Wetland Type (non- riparian, riparian
riverine orriparian non - riverine)
riparian non - riverine
riparian non - riverine
riparian non - riverine
riparian non - riverine
Mapped Soil Series
CsA
CsA and FsE
CsA and FsE
CsA and FsE
Drainage class
well drained
well drained
well drained
well drained
Soil Hydric Status
not hydric
not hydric
not hydric
not hydric
Source of Hydrology
Creek ( oxbow)
Toe seep
Toe seep
Impoundment
Hydrologic Impairment
none
none
none
none
Native vegetation community
Dist. Small Stream/
Narrow FP Forest
Dist. Small Stream/
Narrow FP Forest
Dist. Small Stream/
Narrow FP Forest
herbaceous
t:
Percent composition of exotic
invasive vegetation
80
<10
<10
<10
Regulatory Considerations
Regulation
Applicable?
Resolved?
Supporting Documentation
Waters of the United States - Section 404
Y
N
Waters of the United States - Section 401
Y
N
Endangered Species Act
Y
Y
CE
Approved 9/30/11
Historic Preservation Act
N
N/A
Coastal Zone Management Act (CZMA)/ Coastal Area
Management Act (CAMA)
N
N/A
FEMA Floodplain Compliance
Y
N
CLOMR in progress
Essential Fisheries Habitat
N
N/A
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
16
5.0 DETERMINATION OF CREDITS
Mitigation credits presented in these tables are projections based upon site design. Upon completion of
site construction the project components and credits data will be revised to be consistent with the as -built
condition.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
17
Table 4: Projected Mitigation Credits
Hogan Creek Stream Mitigation
Surry County, North Carolina
EEP Project No. 94708
Stream Mitigation Credits
Type
Restoration
Enhancement I
Enhancement II
Preservation
Total
2,493
1,200
166
1,136
Project Components
Project Component
-or- Reach ID
Proposed
Stationing /Location
Existing
(Thalweg) LF
'Approach
Restoration -or-
Restoration
Equivalent
Proposed LF
Mitigation
Ratio
Hogan Reach 1
STA 1000 -2200
1,331
P2
El
1,200
1:1
Hogan Reach 1
STA 2200 -2884
797
P2
R
684
1:1
Hogan Reach 2
STA 2935 -3897
876
P2
R
962
1:1
UT1, 1A, 1B
Upstream of STA 1000
1,485
Preservation
P
1,485
5:1
UT1
STA 1000 -1066
66
P3
Ell
66
2.5:1
UT2, 2A, 2B, 2C
Upstream of STA 650
3,225
Preservation
P
3,225
5:1
UT2
STA 650 -1000
370
P3
Ell
350
2.5:1
UT2
STA 1000 -1555
633
P2
R
555
1:1
UT3
Upstream of STA 940
963
Preservation
P
963
5:1
UT3
STA 940 -1232
260
P2
R
292
1:1
Component Summary
Restoration Level
Proposed Stream
Length (LF)
Restoration
2,493
Enhancement 1
1,200
Enhancement 11
416
Preservation
5,673
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
17
6.0 CREDIT RELEASE SCHEDULE
All credit releases will be based on the total credit generated as reported by the as -built survey of the
mitigation site. Under no circumstances shall any mitigation project be debited until the necessary US
Department of the Army (DA) authorization has been received for its construction or the District Engineer
(DE) has otherwise provided written approval for the project in the case where no DA authorization is
required for construction of the mitigation project. The DE, in consultation with the Interagency Review
Team (IRT), will determine if performance standards have been satisfied sufficiently to meet the
requirements of the release schedules below. In cases where some performance standards have not
been met, credits may still be released depending on the specifics of the case. Monitoring may be
required to restart or be extended, depending on the extent to which the site fails to meet the specified
performance standard. The release of project credits will be subject to the criteria described as follows:
Table 5: Stream Credits Release Schedule
Monitoring
Credit Release Activity
Interim
Total
Year
Release
Released
0
Initial Allocation - see requirements above
30%
—
30%
1
First year monitoring report demonstrates performance standards are being met
10%
40%
2
Second year monitoring report demonstrates performance standards are being
10%
50% (65 %`)
met
3
Third year monitoring report demonstrates performance standards are being met
10%
60% (75 %`)
4
Fourth year monitoring report demonstrates performance standards are being
10%
70% (85 %`)
met
5
Fifth year monitoring report demonstrates performance standards are being met
15%
100%
and project has received closeout approval
6.1 Initial Allocation of Released Credits
The initial allocation of released credits, as specified in the mitigation plan can be released by the EEP
without prior written approval of the DE upon satisfactory completion of the following activities:
a. Approval of the final Mitigation Plan
b. Recordation of the preservation mechanism, as well as a title opinion acceptable to the USACE
covering the property
c. Completion of project construction (the initial physical and biological improvements to the
mitigation site) pursuant to the mitigation plan; per the EEP Instrument, construction means that a
mitigation site has been constructed in its entirety, to include planting, and an as -built report has
been produced. As -built reports must be sealed by an engineer prior to project closeout, if
appropriate but not prior to the initial allocation of released credits.
d. Receipt of necessary DA permit authorization or written DA approval for projects where DA permit
issuance is not required.
6.2 Subsequent Credit Releases
All subsequent credit releases must be approved by the DE, in consultation with the IRT, based on a
determination that required performance standards have been achieved. For stream projects a reserve of
15% of a site's total stream credits shall be released after two bankfull events have occurred, in separate
years, provided the channel is stable and all other performance standards are met. In the event that less
than two bankfull events occur during the monitoring period, release of these reserve credits shall be at
the discretion of the IRT. As projects approach milestones associated with credit release, the EEP will
submit a request for credit release to the DE along with documentation substantiating achievement of
criteria required for release to occur. This documentation will be included with the annual monitoring
reports.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
18
7.0 MITIGATION WORK PLAN
7.1 Target Streams
The Hogan Creek site affords the opportunity to address the major stressors described in the RBRP
(EEP, 2009) and the Local Watershed Plan Technical Memorandum (EcoEngineering, 2008) for the
Hogan Creek watershed. The project's conceptual design phase focused on developing objectives that
would enhance the ecological services threatened by these stressors. (The proposed conservation
easement boundaries will encompass the four wetlands at the site, but no work is proposed and no
wetland mitigation credit is being sought.) Table 6 below summarizes the links between each design
objective proposed for this project and the ecological service improvements that can be achieved on a
reach -by -reach basis. Specific site constraints and design measures for each reach, along with the target
Rosgen stream types, are presented in Table 7.
Table 6: Design Objectives and Ecological Services
Reach
Target Stream
Type (Slope)
Project Reach
Design Objective
Enhanced Ecological Services
Hogan
Hogan
Levee removal; in- stream structures; bank grading;
Hogan R1
C4 (0.007)
bedrock in profile; culverts at
bankfull benches; new off -line channel segments;
Reach 1
Reach 2
UT1
UT2
UT3
Remove levees; restore stream to
a. Flood attenuation
✓
✓
✓
floodplain interaction.
b. Fine sediment storage
a. Maintenance of stable channel
bed and banks.
Create new channel dimension,
b. Equilibrium sediment transport
✓
✓
✓
✓
pattern and profile
C. Maintenance of in- stream riffle
and pool habitats
Use in- stream structures and
a. Maintenance of stable channel
bank grading to promote stability,
bed and banks.
riffle and pool formation and
b. Equilibrium sediment transport
✓
✓
✓
✓
✓
sediment transport continuity for
C. Maintenance of in- stream riffle
on -line reaches.
and pool habitats
Establish 50 -foot wide riparian
a. Filtration of runoff
buffers with diverse group of
b. Thermal regulation
✓
✓
✓
✓
native species.
C. Input of organic matter
Eradicate invasive exotic
vegetation and seed source;
a. Riparian buffer habitat
✓
✓
✓
✓
replant buffer areas with native
b. Robust species diversity
vegetation.
Install additional livestock fencing
a. Protection of water quality from
and ford crossings to restrict
nutrient and pathogen inputs.
✓
✓
livestock access to streams;
b. Protection of banks from
provide alternative water source.
livestock trampling
Table 7. Target Streams, Constraints and Reach - Specific Measures
Reach
Target Stream
Type (Slope)
Constraints
Reach - Specific Measures
Farming operations on left bank;
Levee removal; in- stream structures; bank grading;
Hogan R1
C4 (0.007)
bedrock in profile; culverts at
bankfull benches; new off -line channel segments;
downstream end
riparian buffers; invasive species removal; livestock
fencing; ford crossing
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
19
Table 7. Target Streams, Constraints and Reach - Specific Measures
Farming operations on left bank;
Levee removal; new off -line channel; in- stream
Hogan R2
C4 (0.006)
culverts at upstream end
structures; bank grading; bankfull benches; riparian
buffers; invasive species removal
UT1
B4 (0.031)
Mature forest; confluence with
Bank sloping and minor re- alignment at downstream
Hogan Creek
end
Farm road and new bridge crossing;
New off -line channel; in- stream structures; bank
UT2
B4 (0.022)
right -of -way; mature forest
grading; bankfull benches; riparian buffers; invasive
species removal; livestock fencing
Mature forest upstream; confluence
New off -line channel; in- stream structures; bank
UT3
B4 (0.025)
with Hogan Creek
grading; bankfull benches; riparian buffers; invasive
species removal
7.2 Target Plant Communities
The target plant community is a more robust and diverse version of the existing Felsic Mesic Forest plant
community identified in the upland and relatively undisturbed reaches of the three UTs. In upland areas
where stream and floodplain grading are not proposed but where invasive exotic plants have encroached,
buffer restoration design will include the following:
• Eradication of invasive exotic species;
• Preservation of desirable existing species; and
• Supplemental planting with selected native trees and shrubs to encourage a more diverse
version of the target community.
Most of the areas proposed for stream and floodplain grading are currently pasture or hay field. The
target plant community for these areas will be the same as the upland areas, but species within this
community will be selected for their adaptation to streambank and floodplain conditions. Appendix C
includes a table with several candidate species for buffer planting.
7.3 Design Methodology and Data Analyses
The design methodology incorporated form -based and analytical approaches, using a combination of
statistical relationships and analyses to arrive at a design discharge for each reach. Other primary design
criteria, such as cross section dimensions, pattern and profile, are all linked to the design discharge and
to each other. The following sections summarize each phase of the methodology; supporting calculations
and data are included in Appendix C.
7.3.1 Design Discharge
In order to estimate a range of design discharge for each reach, we evaluated regional regression
equations, analyzed field bankfull indicators using hydraulic models, and considered sediment transport
competence using critical discharge for initiation of bed material mobility.
In addition to evaluating discharge at various surveyed riffle cross sections on the project reaches, we
also evaluated the predicted discharge for the Mill Creek reference reach as a check of the analysis
methodology. As indicated in the table, there is considerable spread in the predicted design discharge
values. The USGS 2 -year estimate typically provides an upper bound on the bankfull discharge while the
critical discharge estimates typically provide a lower bound. (The nearest USGS stream gauging station
is not particularly helpful for our analyses; it is located on the Mitchell River with a drainage area nearly 40
times larger than the project reach.) The critical discharge estimates based on competence for the bar
sample Dloo appear to over - predict bankfull discharge for Hogan Creek and under - predict bankfull
discharge for the two tributaries and the reference reach. The field indicators and the critical discharge
based on pavement D84 appear to be reasonable predictions, judging by their close agreement to each
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
20
other and the regional curve. Selected design discharge values are indicated Table 8 below. We did not
perform hydraulic or sediment transport analyses for UT1 since the bank sloping work proposed is minor
and will not significantly affect channel dimension, pattern or profile.
Table 8: Design Discharge Estimates (cfs)
Design Reach
NC Rural
Piedmont
Regional Curve
USGS
2 -year
Hydraulic Model
using Field
Indicators
Critical
Discharge
(Pavement Da4)
Critical
Discharge
(Bar D,00)
Selected
Design Value
Hogan Reach
163
211
201 -308
111 -163
215 -290
170
Hogan Reach 2
166
215
220
142
356
180
UT2
20
22
25
8
3
20
UT3
7
7
28
3
1
7
Mill Creek R.R.
284
385
191 -196
173 -270
77 -87
N/A
7.3.2 Sediment Transport
Table 8 above summarizes sediment transport competence analyses; supporting data are included in
Appendix C. Our analyses indicate the design streams (in terms of cross section and profile) will
transport the size of the large bed materials sampled at the site. We also evaluated sediment transport
capacity and continuity between the supply and design reaches, using unit stream power as the indicator
parameter. We compared stream power over a range of stages up to and above the bankfull stage to
check if continuity was achieved. Hydraulic models (HEC -RAS and RIVERMorph) of the existing and
design conditions were used to support the sediment transport analyses by providing hydraulic
parameters such as hydraulic radius, slope, shear stress, and power. Graphical output of these analyses
is included in Appendix C.
Given the presence of mid - channel sediment deposition and abundant bedrock in the bed, aggradation is
more of a concern that degradation for Hogan Creek. Bars were observed to contain a mixture of coarse
gravel (bed material) and fine to medium sand. The sand fraction is likely the product of bank erosion in
upstream reaches rather than watershed supply and overland flow given the presence of the levee
adjacent to agricultural fields, which tends to trap sediment and confine stream flows. A primary design
objective is to create somewhat greater stream power than currently exists in order to minimize the
potential for future aggradation from the upstream supply reach. Analyses indicate that the Hogan Creek
design reaches have slightly greater unit stream power than the supply reach for stages up to 1.2 to 1.3
times the bankfull stage (about 2.5 times the bankfull discharge). At UT2, unit stream power comparisons
show similar values in the supply and design reaches up 2.3 times the bankfull stage (about 5 times the
bankfull discharge). At UT3, the supply reach has consistently greater unit stream power than the design
reach, but aggradation is not of great concern for UT3 (or UT1 or UT2) because sediment supply is
relatively low with the forested headwaters, which will remain forested in conservation easement.
7.3.3 Cross Section
Design discharge and sediment transport analyses inform the design of cross section dimensions and
shapes; cross section dimensions and shapes along with slope govern hydraulic parameters that are
relevant to design. Past experience also informs the cross section design. For example, project
monitoring over the past several years has indicated that a newly constructed E or C -type channel with a
width -depth ratio less than about 10 can lead to stability problems. We evaluated reference cross
sections as indications of bankfull area and general shape, but the design bank slopes are also governed
by geotechnical stability needs during the monitoring period in areas where little or no deep- rooted
vegetation will be present for the first few growing seasons. Ratios of pool -to -riffle depth and top width
are based in part on reference reach data and in part on past experience.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
21
The design cross sections also account for sediment storage within the channel on point bars and /or in
lateral bars upstream of vane structures. This stored sediment is available for transport during large flow
events, which promotes long -term stability and sediment transport equilibrium; if sediment is not available
for transport within the channel, hungry water conditions can lead to bed and bank scour.
7.3.4 Plan and Profile
Plan geometry design is based on multiple factors, chiefly the selected design slope and lateral
constraints such as easement boundaries and topography. At a particular plan feature such as a
meander bend, geometry is based on a range of dimensionless ratios that have proven to be effective in
meeting design objectives while promoting stability. The prime example for plan geometry is radius of
curvature ratio; well- vegetated and /or bedrock - influenced reference reaches (Mill Creek and upstream
reaches of the UTs) suggest a radius of curvature ratio of 1.0 or less would be desirable, but experience
indicates that a ratio less than about 1.8 places undue stresses on newly constructed banks that lack
deep rooted vegetation. We note that the geomorphic characteristics of the Mill Creek reference reach
are affected by bedrock on the banks and in the bed.
We considered reference reaches when developing plan geometry. Our search for a Hogan Creek
reference reach included upstream reaches of Hogan itself and several other streams in relatively
undisturbed watersheds, primarily in Surry County. We identified a reach of Mill Creek with a stable
meander bend in a valley and with bed materials similar to Hogan Creek. For the UTs, we were able to
locate stable reference cross sections and /or reaches in upland areas at the project site. Reference
cross section /reach data for each project stream are summarized in Appendix C.
As with reference cross sections, reference plan form is useful as a general guide for parameters such as
belt width, radius of curvature and pool -pool spacing. However, as with low width -depth ratios in
reference cross sections, tight radii and pool spacing in reference reaches often cannot be assigned to a
design reach without risk of stability problems in the time while vegetation is becoming established. The
selected pattern and profile take into account aquatic habitat needs, stability throughout the monitoring
period and space constraints. With pattern being directly linked to profile, we considered profile
constraints such as existing bedrock outcrops and the culverts on Miller Gap Road, as well as sediment
transport equilibrium, when assigning profile grades. We also referenced data from three hand auger
borings on the right floodplain of Hogan Creek Reach 2; as mentioned previously, these borings
encountered coarse grained sediments indicative of a former creek bed at depths close to the Reach 2
design thalweg.
The target stream type for Hogan Creek is a moderately sinuous, moderate width -depth ratio C4, which is
appropriate for the relatively flat and wide alluvial valley through which it will flow. Reach 1 will be
constructed largely within the existing channel, with modest pattern shifts at station 22 +00 where existing
pattern is unstable and near station 27 +00 where the new channel will connect to an abandoned oxbow
(wetland 1). The levee on the left bank will be removed, as will a portion of the perpendicular levee near
21 +20. In- stream structures will be incorporated in Reach 1 to promote sediment transport equilibrium,
riffle and pool formation, and enhanced bank stability. Bedrock is not anticipated to affect construction
significantly because the profile will generally follow the existing thalweg.
Reach 2 will be constructed mainly off -line to position the channel in the low point of the valley and
provide much improved floodplain access on both banks. The short reach immediately downstream of
Miller Gap Road will be left relatively straight, with a pool constructed in order to dissipate energy. We
considered enhancing Reach 2 in its existing channel but determined that the result would be sub - optimal
in terms of natural riffle and pool formation and floodplain access. In -line enhancement would also
require as much if not more earthwork /hauling, significant structure /bioengineering, and considerably
more streamflow control during construction than an off -line approach. In the proposed off -line scenario,
excess cut material not used to backfill the abandoned channel can be spoiled on -site in upland areas.
The target stream type for each of the UTs is a B4, with a moderate width -depth ratio and moderate
sinuosity which is suited to the somewhat steeper and more confined tributary valleys. Bankfull benches,
cut on 10:1 slopes, will be provided on both banks. The off -line channel segments promote formation of
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
22
riffle and pool sequences while also affording the ability during construction to maintain clean flow
separate in the original channel.
7.3.5 In- Stream Structures
In- stream structure types and locations were selected based on design stability, habitat enhancement and
sediment transport objectives within each reach. Table 9 below provides a summary of specific
objectives for the proposed structures. Data and analyses supporting the sizing of stone for in- stream
structures are provided in Appendix C.
8.0 MAINTENANCE PLAN
EEP shall monitor the site on a regular basis and shall conduct a physical inspection of the site a
minimum of once per year throughout the post- construction monitoring period until performance
standards are met. These site inspections may identify site components and features that require routine
maintenance. Routine maintenance should be expected most often in the first two years following site
construction and may include the following:
Table 10. Maintenance Provisions
Component /Feature
Table 9. In- Stream Structures
Structure
Objectives
Stream
a.
Bank stability at channel plugs
Geolifts
b.
Quickly establish deep rooted bank vegetation
Rock Vane or Log Vane
a.
Direct flow toward center of channel
vegetation maintenance and repair activities may include supplemental planting, pruning, mulching, and
b.
Promote sediment storage upstream and pool formation downstream
a.
Center flow
Cross Vane / Parabolic Vane
b.
Mitigate over -wide conditions and lessen potential for mid - channel bar formation
Site Boundary
C.
Promote sediment storage upstream and pool formation downstream
means as allowed by site conditions and /or conservation easement. Boundary markers disturbed,
a.
Set grade in profile
Constructed Riffle or Step
b.
Provide roughness in bed
Structure
C.
Initiate riffle habitat and sediment transport equilibrium
a.
Enhance bank stability
Root Wad Cluster
b.
Provide bank roughness
C.
Establish near -bank cover and pool habitat
8.0 MAINTENANCE PLAN
EEP shall monitor the site on a regular basis and shall conduct a physical inspection of the site a
minimum of once per year throughout the post- construction monitoring period until performance
standards are met. These site inspections may identify site components and features that require routine
maintenance. Routine maintenance should be expected most often in the first two years following site
construction and may include the following:
Table 10. Maintenance Provisions
Component /Feature
Maintenance through project close -out
Routine channel maintenance and repair activities may include securing of loose coir matting and
Stream
supplemental installations of live stakes and other target vegetation along the channel. Areas where
stormwater and floodplain flows intercept the channel may also require maintenance to prevent bank
failures and head - cutting.
Vegetation shall be maintained to ensure the health and vigor of the targeted plant community. Routine
vegetation maintenance and repair activities may include supplemental planting, pruning, mulching, and
Vegetation
fertilizing. Exotic invasive plant species shall be controlled by mechanical and /or chemical methods. Any
vegetation control requiring herbicide application will be performed in accordance with NC Department of
Agriculture (NCDA) rules and regulations.
Site boundaries shall be identified in the field to ensure clear distinction between the mitigation site and
Site Boundary
adjacent properties. Boundaries may be identified by fence, marker, bollard, post, tree - blazing, or other
means as allowed by site conditions and /or conservation easement. Boundary markers disturbed,
damaged, or destroyed will be repaired and /or replaced on an as needed basis.
Ford Crossing
By landowner, as allowed by Conservation Easement.
Road Crossing
By landowner, as allowed by Conservation Easement.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
23
9.0 PERFORMANCE STANDARDS
In accordance with the provisions in CFR Title 33, "performance standards that will be used to assess
whether the project is achieving its objectives... and should relate to the objectives ... so that the project
can be objectively evaluated to determine if it is developing into the desired resource type, providing the
expected functions, and attaining any other applicable metrics ".
Table 11 below lists proposed success criteria for each proposed ecological service enhancement. While
some success criteria are quantitative (e.g. bank height ratio) and others are qualitative (e.g. observations
of fine sediment deposition on the floodplain), each is measurable. Year to year comparisons for the
various parameters will allow adaptive management to be implemented early on in the monitoring period
if necessary in order to reduce the risk of widespread problems.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
24
Table 11. Performance Standards
Proposed Ecological Service
Metrics /Success Criteria
Enhancements
a.
Evidence of at least two out -of -bank flows (wrack lines, crest gage data) by year 5
Flood attenuation
b.
BHR < 1.2 each year
Fine sediment storage
a.
Evidence of fine sediment on floodplain at least twice by year 5
a.
Annual changes in riffle cross sectional area generally modest (e.g. <20 %) and
Maintenance of stable channel bed
exhibit a stabilizing trend.
and banks
b.
Annual width -depth ratio changes generally modest (e.g. <20 %) and exhibit a
stabilizing trend
a.
No trends in widespread development of robust (e.g. comprised of coarse material
and /or vegetated actively diverting flow) mid - channel bar features
Equilibrium sediment transport
b.
Majority of riffle pebble counts indicate maintenance or coarsening of substrate
distributions
a.
Overall number and distributions of riffle and pool features are generally maintained
Maintenance of in- stream riffle and
b.
Pool depths may vary from year to year, but the majority maintain depths sufficient to
pool habitats
be observed as distinct features in the profile
c.
Majority of riffle pebble counts indicate maintenance or coarsening of substrate
distributions
Filtration of runoff
a.
Evidence of floating debris or fine sediment on buffer vegetation at least twice by year
5
Thermal regulation
a.
Measured water temperature reduction at locations of new buffer establishment and
at selected dates at years 3 and 5;
a.
Density of 320 stems /ac at year 3; 260 stems /acre at year 5
Riparian buffer habitat density and
b.
Four dominant species at year 5 shall be native
diversity
c.
<20% non - native species at year 5, based on measurements of aerial extent
Protection of water quality from
a.
Observations of intact livestock fencing and absence of evidence of livestock access
nutrient and pathogen inputs
to streams, each year
Protection of banks from livestock
a.
Observations of intact livestock fencing and absence of evidence of livestock impacts,
trampling
each year
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
24
10.0 MONITORING REQUIREMENTS
Annual monitoring data will be reported using the EEP monitoring template. The monitoring report shall
provide a project data chronology that will facilitate an understanding of project status and trends,
population of EEP databases for analysis, research purposes, and assist in decision making regarding
project close -out.
Table 12. Monitoring Requirements
Required Parameter
Quantity
Frequency
Notes
As per April 2003 USACE
Pattern /profile survey will extend for at least 20
Pattern
Wilmington District Stream
annual
bankfull widths per reach.
Mitigation Guidelines
As per April 2003 USACE
A minimum of one representative riffle and pool
Dimension
Wilmington District Stream
annual
cross section will be surveyed per reach.
Mitigation Guidelines
As per April 2003 USACE
Pattern /profile survey will extend for at least 20
Profile
Wilmington District Stream
annual
bankfull widths per reach.
Mitigation Guidelines
As per April 2003 USACE
Sampling will include reach -wide pebble counts
Substrate
Wilmington District Stream
annual
and zigzag pebble counts
Mitigation Guidelines
As per April 2003 USACE
A crest gauge and /or pressure transducer will be
Surface Water
Wilmington District Stream
annual
installed on site; the device will be inspected on
Hydrology
Mitigation Guidelines
a quarterly /semi - annual basis to document the
occurrence of bankfull events on the project
Quantity and location of
Vegetation
vegetation plots will be
annual
Vegetation will be monitored using the Carolina
determined in consultation with
Vegetation Survey (CVS) protocols
EEP
Exotic and nuisance
annual
Locations of exotic and nuisance vegetation will
vegetation
be mapped
Project boundary
semi - annual
Locations of fence damage, vegetation damage,
boundary encroachments, etc. will be mapped
Photographs
annual
Reference photographs will be made at selected
overviews and near - stream locations.
11.0 LONG -TERM MANAGEMENT PLAN
Upon approval for close -out by the Interagency Review Team (IRT) the site will be transferred to the
NCDENR Division of Natural Resource Planning and Conservation's Stewardship Program or other IRT-
approved stewardship entity. This party shall be responsible for periodic inspection of the site to ensure
that restrictions required in the conservation easement or the deed restriction document(s) are upheld.
Endowment funds required to uphold easement and deed restrictions shall be negotiated prior to site
transfer to the responsible party.
The NCDENR Division of Natural Resource Planning and Conservation's Stewardship Program currently
houses EEP stewardship endowments within the non - reverting, interest - bearing Conservation Lands
Stewardship Endowment Account. The use of funds from the Endowment Account is governed by North
Carolina General Statute GS 113A- 232(d) (3). Interest gained by the endowment fund may be used only
for the purpose of stewardship, monitoring, stewardship administration, and land transaction costs, if
applicable. The NCDENR Stewardship Program intends to manage the account as a non - wasting
endowment. Only interest generated from the endowment funds will be used to steward the
compensatory mitigation sites. Interest funds not used for those purposes will be re- invested in the
Endowment Account to offset losses due to inflation.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
25
12.0 ADAPTIVE MANAGEMENT PLAN
Upon completion of site construction EEP will implement the post- construction monitoring protocols
previously defined in this document. Project maintenance will be performed as described previously in
this document. If, during the course of annual monitoring it is determined the site's ability to achieve site
performance standards are jeopardized, EEP will notify the USACE of the need to develop a Plan of
Corrective Action. The Plan of Corrective Action may be prepared using in -house technical staff or may
require engineering and consulting services. Once the Corrective Action Plan is prepared and finalized
EEP will:
1. Notify the USACE as required by the Nationwide 27 permit general conditions.
2. Revise performance standards, maintenance requirements, and monitoring requirements as
necessary and /or required by the USACE.
3. Obtain other permits as necessary.
4. Implement the Corrective Action Plan.
5. Provide the USACE a Record Drawing of Corrective Actions. This document shall depict the
extent and nature of the work performed.
13.0 FINANCIAL ASSURANCES
Pursuant to Section IV H and Appendix III of the Ecosystem Enhancement Program's In -Lieu Fee
Instrument dated July 28, 2010, the North Carolina Department of Environment and Natural Resources
has provided the U.S. Army Corps of Engineers Wilmington District with a formal commitment to fund
projects to satisfy mitigation requirements assumed by EEP. This commitment provides financial
assurance for all mitigation projects implemented by the program.
14.0 DEFINITIONS
Belt width — amplitude of a stream meander bend, measured from outside top of bank to top of bank
DX— with respect to sediment grain size distribution, the grain mean diameter which is larger than x% of
the sample distribution
Morphological description — the stream type; stream type is determined by quantifying channel
entrenchment, dimension, pattern, profile, and boundary materials; as described in Rosgen, D. (1996),
Applied River Morphology, 2nd edition
Native vegetation community — a distinct and reoccurring assemblage of populations of plants, animals,
bacteria and fungi naturally associated with each other and their population; as described in Schafale,
M.P. and Weakley, A. S. (1990), Classification of the Natural Communities of North Carolina, Third
Approximation
Project Area - includes all protected lands associated with the mitigation project
Priority Levels of Restoration — 1: convert incised stream to new stream at original floodplain elevation; 2:
establish new stream and floodplain at existing stream elevation; 3: convert incised stream to new stream
type without establishing an active floodplain but providing flood -prone area; 4: stabilize incised stream in
place.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
26
15.0 REFERENCES
Andrews, E.D. (1984), Bed - material Entrainment and Hydraulic Geometry of Gravel -Bed Rivers in
Colorado. Geol. Soc. of Am. Bull., 95, 371 -378.
Andrews, E.D. and James M. Nankervis. (1995). Effective Discharge and the Design of Channel
Maintenance Flows for Gravel -Bed Rivers. Geophysical Monograph Series, Vol. 89,151 -164.
Bathurst, James C., (2007). Effect of Coarse Surface Layer on Bed -Load Transport. Journal of Hydraulic
Engineering, 33(11), 1192 -1205.
EcoEngineering (2008). Technical Memorandum Task 2, Upper Yadkin Basin Local Watershed Plan.
Harman, et al. (1999). Bankfull Hydraulic Geometry Relationships for North Carolina Streams, AWRA
Wildland Hydrology Symposium Proceedings, Journal of Hydraulic Engineering, AWRA Summer
Symposium, Bozeman, MT, 401 -408.
Leigh, D.S. and Webb, P.A. (2006) Holocene erosion, sedimentation and stratigraphy at Raven Fork,
Southern Blue Ridge Mountains, USA, Geomorphology 78 (2006) 161 -177, Elsevier
Leab, Roger J. (2007), Soil Survey of Surry County, North Carolina, NRCS
Leopold, L.B., Wolman, M.G. and Miller, J.P. (1964). Fluvial Processes in Geomorphology, Dover
Publications, Inc., New York, NY.
North Carolina Ecosystem Enhancement Program (2009), Upper Yadkin Pee -Dee River Basin Priorities.
Rosgen, D. L. (1994). A classification of natural rivers. Catena 22:169 -199.
_. (1996). Applied River Morphology. Pagosa Springs, CO: Wildland Hydrology Books.
_. (1997). A geomorphological approach to restoration of incised rivers. Proceedings of the
Conference on Management of Landscapes Disturbed by Channel Incision. Wang, S.S.Y, E.J.
Langendoen, and F.D. Shields, Jr., eds. 12 -22.
_. (1998). The reference reach - A blueprint for natural channel design (draft). ASCE Conference on
River Restoration. Denver CO. March, 1998. ASCE. Reston, VA.
(2001a). A stream channel stability assessment methodology. Proceedings of the Federal
Interagency Sediment Conference. Reno, NV. March, 2001.
_. (2001 b). The cross -vane, w -weir and j -hook vane structures... their description, design and
application for stream stabilization and river restoration. ASCE conference. Reno, NV. August,
2001.
Schafale, M.P. and Weakley, A. S. (1990). Classification of the Natural Communities of North Carolina,
Third Approximation, NC Natural Heritage Program, Raleigh, NC.
Surry County Planning and Development Department (2006). Land Use Plan 2015; A Ten -Year Vision
for Surry County, North Carolina.
US Army Corps of Engineers Wilmington District (2003). Stream Mitigation Guidelines.
Weaver, J.C., Toby D. Feaster and Anthony J. Gotvald, (2009). "Magnitude and Frequency of Rural
Floods in the Southeastern United States, through 2006: Volume 2, North Carolina" Scientific
Investigations Report 2009 -5158, USGS, Nashville, TN.
Young, T.F. and Sanzone, S. (editors). (2002), A framework for assessing and reporting on ecological
condition. Ecological Reporting Panel, Ecological Processes and Effects Committee. EPA Science
Advisory Board. Washington, DC.
Hogan Creek Mitigation Project - Draft Final Mitigation Plan December 2011
27
APPENDIX A
SITE PROTECTION INSTRUMENTS
APPENDIX B
BASELINE INFORMATION
WETLAND DETERMINATION DATA FORM - Eastern Mountains and Piedmont
Project/Site: (,y-- 1t� cvl: City/County: _ Sampling Date:
21 • t�
Lj
Applicant/Owner: State: NC. Sampling Point: \A)C. #� 1
Investigator(s): 'R- NCVI;tjn t C - R\d(j 1P Section, Township, Range:
Landform (hilislope, terrace, etc.): Q# SICk?f—. Local relief (concave, convex, none): anmye Slope my f%'Z
Subregion (LRR or MLRA): ML\ZPe 13(a Lat: 3(o• ?22.020 Long: 00 •tnC7`�1,7`�l Datum: NA-P E�3
Soil Map Unit Name: _Q56- CQiVCAyC( `6 'aLnh�-S NWI classification: n0,11e
Are climatic ! hydrologic conditions on the site typical for this time of year? Yes — X No (If no, explain in Remarks.)
Are Vegetation , Soil , or Hydrology significantly disturbed? Are "Normal Circumstances" present? Yes X_ No
Are Vegetation , Soil , or Hydrology naturally problematic? (If needed, explain any answers in Remarks.)
SUMMARY OF FINDINGS — Attach site map showing sampling point locations, transects, important features, etc.
Hydrophytic Vegetation Present? Yes % No
Is the Sampled Area
Hydric Soil Present? Yes X No within a Wetland? Yes No
Wetland Hydrology Present? Yes 7C No
Remarks:
HYDROLOGY
Wetland Hydrology Indicators:
Secondary Indicators (minimum of two required)
Primary Indicators (minimum of one is required; check all that apply)
_ Surface Soil Cracks (86)
X Surface Water (Al)
_ True Aquatic Plants (1314)
— Sparsely Vegetated Concave Surface (138)
_ High Water Table (A2)
rC Hydrogen Sulfide Odor (C1)
Drainage Patterns (1310)
X Saturation (A3)
X Oxidized Rhizospheres on Living Roots (C3)
Moss Trim Lines (1316)
Water Marks (81)
_ Presence of Reduced Iron (C4)
_ Dry- Season Water Table (C2)
_ Sediment Deposits (132)
_ Recent Iron Reduction in Tilled Soils (C6)
_ Crayfish Burrows (C8)
— Drift Deposits (133)
_ Thin Muck Surface (C7)
_ Saturation Visible on Aerial Imagery (C9)
_ Algal Mat or Crust (134)
_ Other (Explain in Remarks)
— Stunted or Stressed Plants (D1)
_ Iron Deposits (135)
_ Geomorphic Position (D2)
_ Inundation Visible on Aerial Imagery (67)
_ Shallow Aquitard (D3)
Water - Stained Leaves (139)
_ Microtopographic Relief (D4)
Aquatic Fauna (1313)
_ FAC- Neutral Test (D5)
Field Observations:
Surface Water Present? Yes ) No
Depth (inches): O--Ps
Water Table Present? Yes X No
Depth (inches): 0`2
Saturation Present? Yes No
Depth (inches): 0
Wetland Hydrology Present? Yes No
includes capillary fringe)
Describe Recorded Data (stream gauge, monitoring well, aerial photos, previous inspections), if available:
Remarks:
t
US Army Corps of Engineers Eastern Mountains and Piedmont— Interim Version
VEGETATION (Four Strata) - Use scientific names of plants.
Tree Stratum (Plot size: )
1. S01ly_ t(1kC1rD._,
% Cover Species? Status
to Det-
2. L1V`I er�_jY-C)n 1U 1ts?t
lid
_�
3.
FAC species
x 3 =
4.
x4=
UPL species
5, '
Column Totals:
(A) (B)
6.
B/A =
7.
8.
Sapling /Shrub Stratum (Plot size: )
�D
= Total Cover
2. P2iUiCL VIIGya7�.
3.
1 C�
-
4.
5.
6.
7.
8.
9.
10.
Herb Stratum (Plot size: )
1. i m t2Gt-i -j eri
50
= Total Cover
2. JQJ C,05
to
3. (/ F'� c�
1d
,V
4.
5.
6.
7.
8.
9.
10.
11.
12.
Sampling Point:
Dominance Test worksheet:
Number of Dominant Species ci
That Are OBL, FACW, or FAC: -1 (A)
Total Number of Dominant
Species Across All Strata: 5 (B)
Percent of Dominant Species
That Are OBL, FACW, or FAC: (A/B)
Total % Cover of:
Multiply by:
OBL species
x 1 =
FACW species
x2=
FAC species
x 3 =
FACU species
x4=
UPL species
x5=
Column Totals:
(A) (B)
Prevalence Index =
B/A =
_ 1 - Rapid Test for Hydrophytic Vegetation
_ 2 - Dominance Test is X50%
_ 3 - Prevalence Index is 53.0'
_ 4 - Morphological Adaptations' (Provide supporting
data in Remarks or on a separate sheet)
_ Problematic Hydrophytic Vegetation' (Explain)
'Indicators of hydric soil and wetland hydrology must
be present, unless disturbed or problematic.
Definitions of Four Vegetation Strata:
Tree - Woody plants, excluding vines, 3 in. (7.6 cm) or
more in diameter at breast height (DBH), regardless of
height.
Sapling /Shrub - Woody plants, excluding vines, less
than 3 In. DBH and greater than 3.28 ft (1 m) tall.
Herb -All herbaceous (non- woody) plants, regardless
of size, and woody plants less than 3.28 ft tall.
5� = Total Cover Woody vine -All woody vines greater than 3.28 ft in
Woody Vine Stratum (Plot size: ) height.
2. -Po ey/QV -10- -, 1Q
3.
4.
5 Hydrophytic
Vegetation
6• Present? Yes X No
15 =Total Cover
Remarks: (Include photo numbers here or on a separate sheet.)
No �1o�S we�� u"�e� to evci�vct to v ege rton .
enttv�c we��anok_ ate, \rjo-s ccr+eivc
US Army Corps of Engineers
Eastern Mountains and Piedmont - Interim Version
SOIL
Profile Description: (Describe to
Sampling Point:
or confirm the absence of indicators.)
Depth Matrix Redox Features
(inches) . Color (moist) % Color (moist) % Type' Loc
U--Co rCN` P_ -6r i l ciG( io'i(z 51 ?' 1 t4A PL
RM= Reduced
Hydric Soil Indicators:
Histosol (Al)
_ Histic Epipedon (A2)
_ Black Histic (A3)
_ Hydrogen Sulfide (A4)
Stratified Layers (A5)
_ 2 cm Muck (A10) (LRR N)
_ Depleted Below Dark Surface (A11)
Thick Dark Surface (Al2)
Sandy Mucky Mineral (S1) (LRR N,
MLRA 147, 148)
_ Sandy Gleyed Matrix (S4)
_, Sandy Redox (S5)
_ Stripped Matrix (S6)
Type:
Depth (inches):
marks:
Texture Remarks
2Location: PL =Pore Lining, M= Matrix.
Indicators for Problematic Hydric Sc
_ Dark Surface (S7)
_ Polyvalue Below Surface (SB) (MLRA 147,14B)
_ Thin Dark Surface (39) (MLRA 147, 146)
Loamy Gleyed Matrix (F2)
Depleted Matrix (F3)
_ Redox Dark Surface (F6)
_ Depleted Dark Surface (F7)
_ Redox Depressions (FB)
_ Iron - Manganese Masses (F12) (LRR N,
MLRA 136)
_ Umbric Surface (F13) (MLRA 136, 122)
_ Piedmont Floodplain Soils (F19) (MLRA 146)
2 cm Muck (A10) (MLRA 147)
_ Coast Prairie Redox (A16)
(MLRA 147, 148)
_ Piedmont Floodplain Soils (F19)
(MLRA 136, 147)
— Red Parent Material (TF2)
_ Very Shallow Dark Surface (TF12)
Other (Explain in Remarks)
'Indicators of hydrophytic vegetation and
wetland hydrology must be present,
unless disturbed or problematic.
Hydric Soil Present? Yes %c No
US Army Corps of Engineers Eastern Mountains and Piedmont– Interim Version
WETLAND DETERMINATION DATA FORM — Eastern Mountains and Piedmont
Project/Site: t2!(n ck wet r^lcj City /County: 50T C.-:j Sampling Date: z� • �,
Applicant/Owner: ESP State: NC-1 Sampling Point: �A1� -$Z
Investigator(s): Mf-W %Dn r G l�Cf l� Section, Township, Range:
Landform (hills lope, terrace, etc.): Local relief (concave, convex, none): CLl✓BG.CA1JZ Slope ( %): (3y -2-
Subregion (LRR or MLRA): ML9-A 1�Ca7 Lat: �(p a� Z Long: - CC�(3 ' J'1 Datum: � � icy
Soil Map Unit Name: Cf,5A " Ca; .-CAS -b Scr -neS NWI classification: Y'1C7-l2
Are climatic / hydrologic conditions on the site typical for this time of year? Yes K_ No (If no, explain in Remarks.)
Are Vegetation , Soil or Hydrology significantly disturbed? Are "Normal Circumstances" present? Yes Y% No
Are Vegetation , Soil or Hydrology naturally problematic? (if needed, explain any answers in Remarks.)
SUMMARY OF FINDINGS - Attach site map showing sampling point locations, transects, important features, etc.
Hydrophytic Vegetation Present? Yes 7C No
Is the Sampled Area
Hydric Soil Present? Yes )C No within a Wetland? Yes No
Wetland Hydrology Present? Yes 7C No
Remarks:
HYDROLOGY
Wetland Hydrology Indicators:
Secondary Indicators (minimum of two required)
Primary Indicators (minimum of one is required: check all that apply)
_ Surface Soil Cracks (136)
Surface Water (Al)
_ True Aquatic Plants (1314)
Sparsely Vegetated Concave Surface (138)
_ High Water Table (A2)
Hydrogen Sulfide Odor (C1)
— Drainage Patterns (1310)
Saturation (A3)
Oxidized Rhizospheres on Living Roots (C3)
_ Moss Trim Lines (B16)
_ Water Marks (B1)
_ Presence of Reduced Iron (C4)
_ Dry- Season Water Table (C2)
_ Sediment Deposits (132)
_ Recent Iron Reduction in Tilled Soils (C6)
_ Crayfish Burrows (C8)
Drift Deposits (B3)
`_
_ Thin Muck Surface (C7)
_ Saturation Visible on Aerial Imagery (C9)
Algal Mat or Crust (B4)
_ Other (Explain in Remarks)
_ Stunted or Stressed Plants (D1)
_ Iron Deposits (B5)
_ Geomorphic Position (D2)
Inundation Visible on Aerial Imagery (B7)
_ Shallow Aquitard (D3)
Water - Stained Leaves (B9)
_ Microtopographic Relief (D4)
Aquatic Fauna (1313)
_ FAC- Neutral Test (135)
Field Observations:
Surface Water Present? Yes No
Depth (inches): Q-
WaterTable Present? Yes No _ Depth (inches): , 0—
Saturation Present? Yes _ No
Depth (inches):
Wetland Hydrology Present? Yes No
includes capillary fringe)
_
Describe Recorded Data (stream gauge, monitoring well, aerial photos, previous inspections), if available:
Remarks:
US Army Corps of Engineers Eastern Mountains and Piedmont - Interim Version
VEGETATION (Four Strata) - Use scientific names of plants.
Tree Stratum (Plot size:
1, t�Esr �oC�,CfF 1Ci�' t1� 61'�tO
} % Cover . Species? Status
2.
3,
(A)
4.
5,
(B)
6.
7.
(A/B)
8.
Sapling /Shrub Stratum (Plot size:
1. jt0j n,7elr� 1Q i Y' IOrr
30 = Total Cover
}
2.
3.
4.
5.
6.
7.
(B)
8.
9.
10.
Herb Stratum (Plot size:
1. Impatiens
r3� = Total Cover
)
2.
3.
4.
5.
6.
7.
8.
9.
10.
11.
12.
Woody Vine Stratum (Plot size:
1.
2.
3.
4.
5.
6.
Sampling Point: 1Z
Dominance Test worksheet:
Number of Dominant Species
That Are OBL, FACW, or FAC:
(A)
Total Number of Dominant
Species
Across All Strata:
(B)
Percent of Dominant Species
�„°�
That Are OBL, FACW, or FAC: 0
(A/B)
Prevalence Index worksheet:
Total % Cover of: Multiply by:
OBL species x 1 =
FACW species x2=
FAC species x 3 =
FACU species x4=
UPL species x 5 =
Column Totals: (A)
(B)
Prevalence Index = B/A =
Hydrophytic Vegetation Indicators:
- 1 - Rapid Test for Hydrophytic Vegetation
_ 2. Dominance Test is >50%
_ 3 - Prevalence Index is 53.0'
_ 4 - Morphological Adaptations' (Provide supporting
data in Remarks or on a separate sheet)
_ Problematic Hydrophytic Vegetation' (Explain)
'Indicators of hydric soil and wetland hydrology must
be present, unless disturbed or problematic.
Definitions of Four Vegetation Strata:
Tree - Woody plants, excluding vines, 3 in. (7.6 cm) or
more in diameter at breast height (DBH), regardless of
height.
Sapling /Shrub - Woody plants, excluding vines, less
than 3 in. DBH and greater than 3.28 ft (1 m) tall.
Herb -All herbaceous (non- woody) plants, regardless
of size, and woody plants less than 3.28 ft tall.
Woody vine - All woody vines greater than 3.28 ft in
=Total Cover height.
Hydrophytic
Vegetation
Present? Yes iC No
= Total Cover
larks: (Include photo numbers here or on a separate sheet.)
-
4
Pt Yy)- onck -enng -,,..re`f , one. ten- w< \JQ�JOnCk- Cre:?A-
WCLS cDncC octt&
US Army Corps of Engineers Eastern Mountains and Piedmont - Interim Version
SOIL
Sampling Point: 1fe9(—
Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.)
Depth Matrix
Redox Features
(inches) Color (moist) %
Color (moist) % Tvge Loc
Texture Remarks
O - l�`I�Zl1 ��f
iD`49 -e+1(o
'Type: C= Concentration, D =De lefion, RM= Reduced Matrix, MS= Masked Sand Grains.
2Location: PL =Pore Lining, M= Matrix.
Hydric Soil Indicators:
Indicators for Problematic Hydric Soils':
_ Histosol (A1)
_ Dark Surface (S7)
_ 2 cm Muck (A10) (MLRA 147)
_ Histic Epipedon (A2)
_ Polyvalue Below Surface (S8) (MLRA 147,148)
_ Coast Prairie Redox (A16)
_ Black Histic (A3)
_ Thin Dark Surface (S9) (MLRA 147,148)
(MLRA 147, 148)
Hydrogen Sulfide (A4)
_ Loamy Gleyed Matrix (F2)
_ Piedmont Floodplain Soils (1719)
_ Stratified Layers (A5)
Depleted Matrix (F3)
(MLRA 136, 147)
_ 2 cm Muck (A10) (LRR N)
_ Redox Dark Surface (F6)
_ Red Parent Material (TF2)
_ Depleted Below Dark Surface (A11)
_ Depleted Dark Surface (F7)
_ Very Shallow Dark Surface (TF12)
_ Thick Dark Surface (Al2)
_ Redox Depressions (1713)
— Other (Explain in Remarks)
_ Sandy Mucky Mineral (S1) (LRR N,
_ Iron - Manganese Masses (F12) (LRR N,
MLRA 147, 148)
MLRA 136)
_ Sandy Gleyed Matrix (S4)
— Umbric Surface (F13) (MLRA 136,122)
31ndicators of hydrophytic vegetation and
_ Sandy Redox (S5)
— Piedmont Floodplain Soils (F19) (MLRA 148) wetland hydrology must be present,
_ Stripped Matrix (S6)
unless disturbed or problematic.
Restrictive Layer (if observed):
Type:
Depth (inches):
Hydric Soil Present? Yes _ No
Remarks:
US Army Corps of Engineers Eastern Mountains and Piedmont – Interim Version
WETLAND DETERMINATION DATA FORM — Eastern Mountains and Piedmont
Project(Site: b4ol CX• — W6-lCVy-k_t?'6 City /County: a0r`T`:t Sampling Date: �J Z\ • `1 \
Applicant/Owner: G E \---> State: V3C— Sampling Point:
Investigator(s): iZ• WC%- 0'CDn C'.- Section, Township, Range:
Landform (hillslope, terrace, etc.): SUr 'ff( cal relief (concave, convex, none): Cio,1 Cca tJ-e_ Slope ( %): 02-
Subregion (LRR or MLRA): Lat: 'No-32-3123 Long: "SD• 009 1 Z Datum: W -
Soil Map Unit Name: F,5L 1F0k 1/ttN,) - SGg*-'t V-ne i Cpfri47icYG NWI classification: InC n-C
Are climatic / hydrologic conditions on the site typical for this time of year? Yes _ No (If no, explain in Remarks.)
Are Vegetation , Soil or Hydrology significantly disturbed? Are "Normal Circumstances" present? Yes---,X No
Are Vegetation , Soil or Hydrology naturally problematic? (If needed, explain any answers in Remarks.)
SUMMARY OF FINDINGS - Attach site map showing sampling point locations, transacts, important features, etc.
Hydrophytic Vegetation Present? Yes _ X No Is the Sampled Area
Hydric Soil Present? Yes . )k No within a Wetland? Yes No
Wetland Hydrology Present? Yes 7� No
Remarks:
HYDROLOGY
Wetland Hydrology Indicators:
Secondary Indicators (minimum of two required)
Primary indicators (minimum of one is required: check all that apply)
_ Surface Soil Cracks (66)
X Surface Water (Al)
_ True Aquatic Plants (B14)
_ Sparsely Vegetated Concave Surface (138)
High Water Table (A2)
— Hydrogen Sulfide Odor (C1)
_ Drainage Patterns (1310)
X Saturation (A3)
Oxidized Rhizospheres on Living Roots (C3)
_ Moss Trim Lines (B16)
Water Marks (B1)
_ Presence of Reduced Iron (C4)
_ Dry- Season Water Table (C2)
_ Sediment Deposits (B2)
_ Recent Iron Reduction in Tilled Soils (C6)
` Crayfish Burrows (C8)
_ Drift Deposits (B3)
_ Thin Muck Surface (C7)
_ Saturation Visible on Aerial Imagery (C9)
Algal Mat or Crust (B4)
_ Other (Explain in Remarks)
_ Stunted or Stressed Plants (D1)
_ Iron Deposits (135)
— Geomorphic Position (D2)
_ Inundation Visible on Aerial Imagery (137)
— Shallow Aquitard (D3)
Water - Stained Leaves (139)
_ Microtopographic Relief (D4)
_ Aquatic Fauna (1313)
_ FAC- Neutral Test (D5)
Field Observations:
Surface Water Present? Yes _ No
Depth (inches): C�
Water Table Present? Yes No
Depth (inches): Q ° Z
Saturation Present? Yes_ No
Depth (inches): U
Wetland Hydrology Present? Yes No
includes capillary fringe)
Describe Recorded Data (stream gauge, monitoring well, aerial photos, previous inspections), if available:
Remarks:
US Army Corps of Engineers Eastern Mountains and Piedmont- Interim Version
VEGETATION (Four Strata) - Use scientific names of plants,
Tree Stratum (Plot size: )
1. LirVC3G1��IC��iY1 tV`I�i�C'�G._
% Cover Species? Status
`F�tG
2. YkCer Vb�Ur'fl
! 3 FAC
3.
FACW species
4.
FAC species
x3=
FACU species
6.
UPL species
7.
Column Totals:
8.
Sapling /Shrub Stratum (Plot size:
1, Ito M ca me It 3 'V i V-Q F rl k C(A 6k-
1E5 =Total Cover
}
2. L1Q05-TVQrn 5I11 °en -)e.
2- 14 FAG
3. r, M k1L3��S �'!'1✓i�.k 1{yS�1�SiS
Z �I FflG�-
4.
height.
5.
8.
6.
7.
than 3 in. DBH and greater than 3.28 ft (1 m) tall.
Sampling Point:
Dominance Test worksheet:
Number of Dominant Species
That Are OBL, FACW, or FAC: (A)
Total Number of Dominant
Species Across All Strata: co (B)
Percent of Dominant Species
That Are OBL, FACW, or FAC: 30/0 (A/B)
Prevalence Index worksheet:
Total % Cover of:
Multiply by:
OBL species
x 1 =
FACW species
x2=
FAC species
x3=
FACU species
x4=
UPL species
x5=
Column Totals:
(A) (B)
Prevalence Index = B/A =
8.
- 1 - Rapid Test for Hydrophytic Vegetation
- 2 - Dominance Test is >50%
3 - Prevalence Index is 53.01
9.
10.
_� 4 - Morphological Adaptations' (Provide supporting
5 °2-. = Total Cover
Herb Stratum (Plot size: )
data in Remarks or on a separate sheet)
Problematic Hydrophytic Vegetation' (Explain)
'Indicators of hydric soil and wetland hydrology must
be present, unless disturbed or problematic.
2. 00 J�, � 61 Urn a ,y (�St" IGr✓1U(C�CS
3'
4'
Definitions of Four Vegetation Strata:
5.
Tree - Woody plants, excluding vines, 3 in. (7.6 cm) or
more in diameter at breast height (DBH), regardless of
6'
7.
height.
8.
Sapling /Shrub - Woody plants, excluding vines, less
g.
than 3 in. DBH and greater than 3.28 ft (1 m) tall.
1 D.
Herb - All herbaceous (non- woody) plants, regardless
of size, and woody plants less than 3.28 ft tall.
11.
12.
1 D = Total Cover Woody vine - All woody vines greater than 3.28 ft in
Woody Vine Stratum (Plot size: )
height.
1, ioniceya.. japDvina,
2.
3.
4.
Hydrophytic
5. Vegetation
6. Present? Yes No
�5 = Total Cover
ks: (Include photo numbers here or on a separate sheet.)
Imo 016 is \NCr-e- Used '?-\f r ) CA tom Ce ;-- ;-�vr .
Pr m2C1nci2�1�� ax o �n2 �r�h�� w iCv7c�•
c�rec WCQ) Cmcicr-tcal,
US Army Corps of Engineers Eastern Mountains and Piedmont - Interim Version
SOIL
Sampling Point: \[4L-AA-3
Profile Description: (Describe to the depth needed to document the indicator or confirm the absence of indicators.)
Depth Matrix
Redox Features
(Inches) . Color (moist) %
Color (moist) % Twe Loc
Texture Remarks
y-to 104 1�-41 ( C10
i o`F t2 3i(2 2_ 21A
'Type: C= Concentration, D =De letion, RM= Reduced Matrix, MS= Masked Sand Grains.
ZLocation: PL =Pore Lining, M= Matrix.
Hydric Soil Indicators:
Indicators for Problematic Hydric Soils':
_ Histosol (Al)
_ Dark Surface (S7)
— 2 cm Muck (A10) (MLRA 147)
_ Histic Epipedon (A2)
_ Polyvalue Below Surface (S8) (MLRA 147,
148) — Coast Prairie Redox (A16)
Black Histic (A3)
_ Thin Dark Surface (S9) (MLRA 147, 148)
(MLRA 147, 148)
_ Hydrogen Sulfide (A4)
_ Loamy Gleyed Matrix (F2)
_ Piedmont Fioodplain Soils (F19)
_ Stratified Layers (A5)
ZC Depleted Matrix (F3)
(MLRA 136, 147)
_ 2 cm Muck (A10) (LRR N)
_ Redox Dark Surface (F6)
_ Red Parent Material (TF2)
_ Depleted Below Dark Surface (A11)
_ Depleted Dark Surface (F7)
_ Very Shallow Dark Surface (TF12)
_ Thick Dark Surface (Al2)
_ Redox Depressions (F8)
_ Other (Explain in Remarks)
_ Sandy Mucky Mineral (S1) (LRR N,
_ Iron - Manganese Masses (F12) (LRR N,
MLRA 147, 148)
MLRA 136)
Sandy Gleyed Matrix (S4)
_ Umbric Surface (F13) (MLRA 136, 122)
31ndicators of hydrophytic vegetation and
Sandy Redox (35)
_ Piedmont Floodplain Soils (F19) (MLRA 14B) wetland hydrology must be present,
_ Stripped Matrix (S6)
unless disturbed or problematic.
Restrictive Layer (if observed):
Type:
Depth (inches):
Hydric Soil Present? Yes �_ No
Remarks:
US Army Corps of Engineers
Eastern Mountains and Piedmont – Interim Version
NC DWQ Stream Identification Form Version 4.11
Date:
v3- Ilk • Z0!\
Project/Site: EEC .
as t- V- (f �
Latitude:
Evaluator: �.bc'�tti(A� 1 \`�f',1 tor-1
County:
Longitude:
Total Points: ?,
Stream Determination (circ a
Other 'S' kk0c_ ,rrl Q C%_
Stream is at least intermittent
if >_ 19 or perennial if >_ 30*
Ephemeral Intermittent (Perennial'i
e.g. Quad Name:
A. Geomorphology (Subtotal = 2A )
Absent
Weak
Moderate
Strong
1a. Continuity of channel bed and bank
0
1
2
3
2. Sinuosity of channel along thalweg
0
1
2
3
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
1
n,
V_J
3
4. Particle size of stream substrate
0
1
2
3 .
5. Active /relict floodplain
0
1
2
1.5
6. Depositional bars or benches
0
1
0.5
3
7. Recent alluvial deposits
0
1
2
3
8. Headcuts
0
1
2
3
9. Grade control
0
n
1
1.5
10. Natural valley
0
0.5
1
Co
11. Second or greater order channel
No = 0
Yes 3
artificial ditches are not rated; see discussions in manual
B. Hydroloqy (Subtotal= ( )
12. Presence of Baseflow
0
1
2
3®
13. Iron oxidizing bacteria
0
1
2
3
14. Leaf litter
1.5
1
<
0
15. Sediment on plants or debris
0
0.5
21. Aquatic Mollusks
1.5
16. Organic debris lines or piles
0
0.5
1
.5
17. Soil -based evidence of high water table?
No= 0
Yes = 3
C. Biology (Subtotal= 'w __1)
18. Fibrous roots in streambed
3
2
1
0
19. Rooted upland plants in streambed
2
1
0
20. Macrobenthos (note diversity and abundance)
0
3
21. Aquatic Mollusks
0
1
2
3
22. Fish
0.5
1
1.5
23, Crayfish
CO)
0.5
1
1.5
24. Amphibians
0
0.5
1
1.5
25. Algae
CO)
0.5
1
1 1.5
26. Wetland plants in streambed
I
FACW = 0.75; OBI = 1.5 Other 0
*perennial streams may also be identified using other methods. See p.
35 of manual.
Notes: r7CA "
L ve <, , rY'3 �:,� =r v-t(- c� -�- `✓'�Cx .�
° �Fa a+� �� c�°i -+��a� en c t r � .
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date:
0'6.2\. Zcr
Project/Site: EE
, i C -<,ff K
Latitude:
Evaluator:_
v
County: �.
Longitude:
Total Points:
Stream Determination (circl
Other 5t \DCtrn
Stream is at least intermittent
if? 19 or perennial if? 30*
Ephemeral Intermittent erennial
e.g. Quad Name:
A. Geomorphology (Subtotal = 2.2• )
Absent
Weak
Moderate
Strong
1a' Continuity of channel bed and bank
0
1
2
(3
2. Sinuosity of channel along thalweg
0
1
2
3
3. In- channel structure: ex. riffle-pool, step -pool,
ripple-pool sequence
0
1
0
3
4. Particle size of stream substrate
0
1
2
Ci
5. Active /relict floodplain
0
1
23
1.5
6. Depositional bars or benches
0
1
2
3
7. Recent alluvial deposits
0
1
2
3
8. Headcuts
G
1
2
3
9. Grade control
0
0.5
1
1.5
10. Natural valley
0
0.5
1
11. Second or greater order channel
No = 0
Yes 3
° artificial ditches are not rated; see discussions in manual
B. Hydrology (Subtotal = Co )
12. Presence of Baseflow
0
1
2
0
13. Iron oxidizing bacteria
0
1
2
3
14. Leaf litter
1.5
1
0.5
0
15. Sediment on plants or debris
0
1
1
1.5
16. Organic debris lines or piles
0 1
0.5
1
.5
17. Soil -based evidence of high water table?
No = 0
Yes = 3
C. Biologv (Subtotal = )
18. Fibrous roots in streambed
2
1
0
19. Rooted upland plants in streambed
2
1
0
20. Macrobenthos (note diversity and abundance)
0
1
2
3
21. Aquatic Mollusks
0
1
2
3
22. Fish
0
.5
1
1.5
23. Crayfish
0
0.5
1
1.5
24. Amphibians
0
0
1
1.5
25. Algae
0
0.5
1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other 0
*perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: . ,�
n t-. r v {�'rY c
r► zt c..
Sketch:
NC DWO Stream Identification Form Version 4.11
Date:
Project/Site: F-EP5L-kr-
Latitude:
Evaluator:
County: s
Longitude:
Total Points: 1
Stream Determination (circllesing
Other 51 00j- A QUC'ck
Stream is at least intermittent
Ephemeral Intermittent erennial)
e.g. Quad Name:
if ? 19 or perennial if ?
NC DWQ Stream Identification Form Version 4.11
Date:
Project/Site: ��
Latitude:
Evaluator: pl� oc1?1
County: SUf%r.�4
Longitude:
Total Points: 2.cl 5
Stream Determination (circle one)
Other S \ \0CtiJq Q\XAd(.
Stream is at least intermittent
Ephemeral Intermittent P-erenniat
e.g. Quad Name:
if? 19 or perennial if ? 30`
2
3D
A. Geomorphology (Subtotal = t )
Absent
Weak
Moderate
Strong
1a"Continuity of channel bed and bank
0
1
2
3
2. Sinuosity of channel along thalweg
0
1
2
3D
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
1
2
3
4. Particle size of stream substrate
0
1
2
3
5. Active/relict floodplain
0
1
2
3
6. Depositional bars or benches
0
1
3
7. Recent alluvial deposits
0
CD
2
3
8. Headcuts
(0
1
2
3
9. Grade control
0
Q
1
1.5
10. Natural valley
0
0.5
1
11. Second or greater order channel
No 0
Yes = 3
- artificial ditches are not rated; see discussions in manual
B. Hvdrolociv (Subtotal= 5.5 )
12. Presence of Baseflow
0
1
3
13. Iron oxidizing bacteria
0
1
2
3
14. Leaf litter
1.5
C1
0.5
0
15. Sediment on plants or debris
0
(D
1
1.5
16. Organic debris lines or piles
0
0.5
3
1.5
17. Soil -based evidence of high water table?
No =Q)
Yes = 3
C. Bioloqv (Subtotal = �► )
18. Fibrous roots in streambed
3
Q
1
0
19. Rooted upland plants in streambed
CD
2
1
0
20. Macrobenthos (note diversity and abundance)
0
1
Q
3
21. Aquatic Mollusks
Q
1
2
3
22. Fish
0.5
1
1.5
23. Crayfish
0.5
1
1.5
24. Amphibians
0.5
1
1.5
25. Algae
0.5
1
1
1.5
26. Wetland plants in streambed
FACW =
0.75; OBL = 1.5 Other
'perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: Ctc(a'
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date:
Project/Site: ��J�t
Latitude:
Evaluator:
County: SUS
Longitude:
Total Points:
Stream Determi "on (circle one)
Other11�Ctty
Stream is at least intermittent
if ? 19 or perennial if ? 30*
Ephemeral termittent Perennial
P
e. Quad Name:
9'
A. Geomorphology (Subtotal = 1 ° )
Absent
Weak
Moderate
Strong
1"Continuity of channel bed and bank
0
1
2
3
2. Sinuosity of channel along thalweg
t
1
2
3
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
0.5
2
3
4. Particle size of stream substrate
0
1
2
3
5. Active /relict floodplain
0
1
2
3
6. Depositional bars or benches
M
1
2
3
7. Recent alluvial deposits
0
1 ,
2
3
8. Headcuts
0
1
2
3
9. Grade control
0
0.5
V
1.5
10. Natural valley
0
0.5
1
11. Second or greater order channel
No 0
Yes = 3
artificial ditches are not rated; see discussions in manual
B. Hydrology (Subtotal= 2.5 )
12. Presence of Baseflow
0
Q
2
3
13. Iron oxidizing bacteria
0 )
2
2
3
14. Leaf litter
1.5
1
0.5
0
15. Sediment on plants or debris
0
0.5
1
1.5
16. Organic debris lines or piles
0
0.5
1
1.5
17. Soil -based evidence of high water table?
No
Yes = 3
C. Biologv (Subtotal = 6 )
18. Fibrous roots in streambed
3
Q
1
0
19. Rooted upland plants in streambed
2
1
0
20. Macrobenthos (note diversity and abundance)
0
1
2
3
21. Aquatic Mollusks
1
2
3
22. Fish
0
0.5
1
1.5
23. Crayfish
0.5
1
1.5
24. Amphibians
0.5
1
1.5
25. Algae
0.5
1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other =to-)
*perennial streams may also be identified using other methods. See p. 35 of manual.
Notes:
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date:
U'' .2 1d
Project/Site: GG�' Std _
n tire'
Latitude:
Evaluator:
County:
Longitude:
Total Points: 51
Stream Determination (circle
511C3C.ttV1 QLkOC
Other ,
Stream is at least intermittent
if ?
NC DWQ Stream Identification Form Version 4.11
Date:
Project/Site: OE'�p Sim` `
Latitude:
Evaluator:
County:
Longitude:
Total Points: �.
Stream Determination circl
(}
Other
Stream is at least intermittent
if ? 19 or perennial if ? 30"
Ephemeral Intermittent erennial
P
e. 5' Quad Name:
A. Geomorphology (Subtotal= )
Absent
Weak
Moderate
Strong
1' Continuity of channel bed and bank
0
1
2
3
2. Sinuosity of channel along thalweg
0
1
2
3
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
�*�
=='
2
3
4. Particle size of stream substrate
0
1
1
3
5. Active /relict floodplain
0
1
2
1.5
6. Depositional bars or benches
0
1
2
3
7. Recent alluvial deposits
0
1
2
3
8. Headcuts
a
1
2
3
9. Grade control
0
0.
1
1.5
10. Natural valley
0
0.5
1
.5
11. Second or greater order channel
No = 0
Yes 3
artificial ditches are not rated; see discussions in manual
B. Hydrology (Subtotal= V' 6 )
12. Presence of Baseflow
0
1
2
1
13. Iron oxidizing bacteria
t0
1
2
3
14. Leaf litter
1.5
1
0.5
0
15. Sediment on plants or debris
6
0.5
1
1.5
16. Organic debris lines or piles
0
0.5
1
.5
17. Soil -based evidence of high water table?
No 0
Yes = 3
C. Biology (Subtotal = )
18. Fibrous roots in streambed
3
2
1
0
19. Rooted upland plants in streambed
2
1
0
20. Macrobenthos (note diversity and abundance)
0
1
2
3
21. Aquatic Mollusks
1
2
3
22. Fish
0.5
1
1.5
23. Crayfish
a
0.5
1
1.5
24. Amphibians
0
0.5
1
1.5
25. Algae
0
0.5
1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other 0
'perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: i
min _.
�1 r) :N IBS r�o �✓ tic .�
pr C
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date:
a95, '21, ZO°t\
Project/Site, `_'� St-< -
l - cv ff V.
Latitude:
Evaluator: `- � �
County: son .
Longitude:
Total Points: y ,
Stream Determination (cir el
Other C
`fit �Ct�
Stream is at least intermittent
if? 19 or erennial if> 30*
Ephemeral Intermittent erennial
e.g. Quad Name:
A. Geomorphology (Subtotal = � CA, )
Absent
Weak
Moderate
Strong
1 a. Continuity of channel bed and bank
0
1
2
3
2. Sinuosity of channel along thalweg
0
1
2
0
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
1
Q
3
4. Particle size of stream substrate
0
1
2
1.
5. Active /relict floodplain
0
1
2
3
6. Depositional bars or benches
0
1
6)
3
7. Recent alluvial deposits
0
0.5
2
3
8. Headcuts
0
1
3
9. Grade control
0
0.5
1.5
10. Natural valley
0
0.5
1
.5
11. Second or greater order channel
No 00
Yes = 3
a artificial ditches are not rated; see discussions in manual
B. Hydrology (Subtotal = (Q }
12. Presence of Baseflow
0
1
�,.
3
13. Iron oxidizing bacteria
0
1°
2
3
14. Leaf litter
1.5
)
0.5
0
15. Sediment on plants or debris
0
1
1
1.5
16. Organic debris lines or piles
0
0.5
1
1.
17. Soil -based evidence of high water table?
No .0
Yes = 3
C. Biology (Subtotal= UST-)
18. Fibrous roots in streambed
3
Q
1
0
19. Rooted upland plants in streambed
03
2
1
0
20. Macrobenthos (note diversity and abundance)
0
1
2
3
21. Aquatic Mollusks
0
1
2
3
22. Fish
0
0.5
1
1.5
23. Crayfish
0
0.5
1
1.5
24. Amphibians
0
0.5
1.5
25. Algae
0
0.5
1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other
*perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: - ae)
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date:
0�- -Lt 20 \!
Project/Site: EEA' Std
v`{ -cK.
Latitude:
Evaluator: 9_"noe Y>
County: S?rv--4
Longitude:
Total Points: 31
Stream Determination (cir an4)
Other 5 0cri,"l
if 2: 19 or if ? 30' is at least intermittent
if >_ 19
Ephemeral Intermittent erennia
e.g. Quad Name:
A. Geomorphology (Subtotal
Absent
Weak
Moderate
Strong
1a. Continuity of channel bed and bank
0
1
2
3 -
2. Sinuosity of channel along thalweg
0
1
2
37
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
p
1
0
3
4. Particle size of stream substrate
0
1
2
3
5. Active /relict floodplain
0
1
2
3
6. Depositional bars or benches
d
1
2
3
7. Recent alluvial deposits
0
1
2
3
8. Headcuts
0
1
2
3
9. Grade control
0
0.5
1.5
10. Natural valley
0 1
0.5
1
0
11. Second or greater order channel
No
Yes = 3
artificial ditches are not rated; see discussions in manual
B. Hydrology (Subtotal = )
12. Presence of Baseflow
0
1
0
3
13. Iron oxidizing bacteria
M7-
1
2
3
14. Leaf litter
1.5
1
0.5
0
15. Sediment on plants or debris
0
0.5
0
1.5
16. Organic debris lines or piles
0
1 0.5
1
1.5
17. Soil -based evidence of high water table?
No 0
Yes = 3
C. Biology (Subtotal = )
18. Fibrous roots in streambed
3
2
1
0
19. Rooted upland plants in streambed
3
2
1
0
20. Macrobenthos (note diversity and abundance)
0
1
3
21. Aquatic Mollusks
0
2
3
22. Fish
0"
0.5
1
1.5
23. Crayfish
0.5
1
1.5
24. Amphibians
d
0.5
1
1.5
25. Algae
0
0.5 1
1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other
*perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: c
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date:
Project/Site: ESQ '�
Latitude:
Evaluator:
County-�
Longitude:
Total Points: �e�j.�
Stream Determination (circle one)
Other 0UQ(A_
Stream is at least intermittent
Ephemeral- (Yf mitte Perennial
e.g. Quad Name:
if? 19 or perennial if? 30�
2
3
A. Geomorphology (Subtotal ='I )
Absent
Weak
Moderate
Strong
1a. Continuity of channel bed and bank
0
1
2
W
2. Sinuosity of channel along thalweg
0
1
2
3
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
1
2�
3
4. Particle size of stream substrate
0
1
2
_
5. Active /relict floodplain
0i
Yes = 3
2
3
6. Depositional bars or benches
0
1
2
3
7. Recent alluvial deposits
0
1
2
3
8. Headcuts
0
1
2
3
9. Grade control
0
.5
1
1.5
10. Natural valley
0
0.5
1
1.
11. Second or greater order channel
No =IQ
Yes = 3
a artificial ditches are not rated; see discussions in manual
B. Hydrology (Subtotal = (0-5 )
12. Presence of Baseflow
0
1
1
3
13. Iron oxidizing bacteria
0
1
(
3
14. Leaf litter
1.5
1
2
0
15. Sediment on plants or debris
0
1
1
1.5
16. Organic debris lines or piles
0
1 0.5
1
1.
17. Soil -based evidence of high water table?
No 0
Yes = 3
C. Biology (Subtotal=___ Pi ) '
18. Fibrous roots in streambed
3
1
0
19. Rooted upland plants in streambed
0
2
1
0
20. Macrobenthos (note diversity and abundance)
Q
1
2
3
21. Aquatic Mollusks
0
1
2
3
22. Fish
0.5
1
1.5
23. Crayfish
o
0.5
1
1.5
24. Amphibians
0.5
1
1.5
25. Algae
0
0.5
1
1 1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other - 0
'perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: \_,kT Z10
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date: •,
Project/Site: C . �6 _
Latitude:
Evaluator: .� I
County:
Longitude:
Total Points: ? 2 �j
Stream Determi circle one)
Other i r-n °.�t;� C-d
Stream is at leastintermiftenT
if? 19 or perennial if >_ 30*
Ephemeral termittent Perennial
e.g. Quad Name:
A. Geomorphology (Subtotal = $ ° )
Absent
Weak
Moderate
Strong
1a. Continuity of channel bed and bank
0
1
2
6)
2. Sinuosity of channel along thalweg
0
1
9)
3
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
0.5
2
3
4. Particle size of stream substrate
0
1
1
3
5. Active /relict floodplain
E2
1
2
3
6. Depositional bars or benches
0
1
1
3
7. Recent alluvial deposits
0
1
2
3
8. Headcuts
0
1
2
3
9. Grade control
0
0.5
1.5
10. Natural valley
0
0.5
1
11. Second or greater order channel
No _0
Yes = 3
artmcial ditches are not rated; see discussions in manual
B. Hvdroloav (Subtotal= 2, 57) 1
12. Presence of Baseflow
0
0
2
3
13. Iron oxidizing bacteria
1 1
1
2
3
14. Leaf litter
1.5
1
2
0
15. Sediment on plants or debris
0
0.5
1
1.5
16. Organic debris lines or piles
0
0.5
1
1.5
17. Soil -based evidence of high water table?
No 0)
Yes = 3
G. 13loloQV (Subtotal = c5 .c )
18. Fibrous roots in streambed
3
(0
1
0
19. Rooted upland plants in streambed
3
V
1
0
20. Macrobenthos (note diversity and abundance)
0
1
2
3
21. Aquatic Mollusks
1
2
3
22. Fish
Q
0.5
1
1.5
23. Crayfish
0.5
1
1.5
24. Amphibians
0
0.5
1
1.5
25. Algae
0
1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other x'01
*perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: C -
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date: ®. � `
Project/Site: e�p S If
Latitude:
Evaluator:e_lf�a
County: re
Longitude:
Total Points: j � .5
Stream Determination circle onel
Other 1 r C(,,. f1; .a
�7Gr��
Stream is at least intermittent
if ? 19 or perennial if ? 30
Ephemeral Intermittent ennia
P
,
e. Quad Name:
9
A. Geomorphology (Subtotal = _)_0 )
Absent
Weak
Moderate
Strong
1a. Continuity of channel bed and bank
0
1
2
0.
2. Sinuosity of channel along thalweg
0
1
2
ID
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
1)
V
3
4. Particle size of stream substrate
0
1
2
1.5
5. Active /relict floodplain
0
1
2
3
6. Depositional bars or benches
0
1
2
3
7. Recent alluvial deposits
0
1
2
3
8. Headcuts
0
1
2
3
9. Grade control
0
0.5
1
10. Natural valley
0
0.5
1
11. Second or greater order channel
No 0
Yes = 3
_ artiticial ditches are not rated; see discussions in manual
B. Hvdroloav (Subtotal= Z* 1
12. Presence of Baseflow
0
1?
1
3
13. Iron oxidizing bacteria
3
1
2
3
14. Leaf litter
1.5
1
0.
0
15. Sediment on plants or debris
0
0D
1
1.5
16. Organic debris lines or piles
0
0.5
1
1.5
17. Soil -based evidence of high water table?
No tlZ'
Yes = 3
U. ti101OCIV (Subtotal = -1 .1-) )
18. Fibrous roots in streambed
3
2
1
0
19. Rooted upland plants in streambed
3
2
1
0
20. Macrobenthos (note diversity and abundance)
0
1
(D
3
21. Aquatic Mollusks
(D
1
2
3
22. Fish
0
0.5
1
1.5
23. Crayfish
0
0.5
1
1.5
24. Amphibians
0.
1
1.5
25. Algae
0.5
1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other .. 0
"perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: S
aion n_) gf'<'CXC" 0
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date: „ �',o 2\ ��
- IQ
Project/Site: GE ?
Latitude:
Evaluator: n
County: �rY
Longitude:
Total Points: 2�vv
:1t
Stream is least intermittent
Stream Determination (circl o e
Other `;E' , a
at
if? 19 or perennial if? 30'
Ephemeral Intermitten erennial
P
e. Quad Name:
g•
A. Geomorphology (Subtotal=
Absent
Weak
Moderate
Strong
18 Continuity of channel bed and bank
0
1
2
3,
2. Sinuosity of channel along thalweg
0
1
2
0
3. In- channel structure: ex. riffle -pool, step -pool,
ripple-pool sequence
0
1
1
3
4. Particle size of stream substrate
0
1
1
3
5. Active/relict floodplain
0
1
1
3
6. Depositional bars or benches
0
1
1
3
7. Recent alluvial deposits
0
1 ,
2
3
8. Headcuts
0
1
2
3
9. Grade control
0
0.5
1
1.5
10. Natural valley
0
_ 0.5
1
.5
11. Second or greater order channel
No
Yes = 3
artlticial ditches are not rated; see discussions in manual
B. Hvdroloav (Subtotal = 4 )
12. Presence of Baseflow
0
1
01.
3
13. Iron oxidizing bacteria
3 )
1
2
3
14. Leaf litter
1.5
1
0.5
0
15. Sediment on plants or debris
0
(Q
1
1.5
16. Organic debris lines or piles
0
0.5
1
1.5
17. Soil -based evidence of high water table?
No 0 )
Yes = 3
L. bloloQV (subtotal = ilo )
18. Fibrous roots in streambed
3
1
0
19. Rooted upland plants in streambed
3 )
2
1
0
20. Macrobenthos (note diversity and abundance)
'0
2
3
21. Aquatic Mollusks
0
1
2
3
22. Fish
U
0.5
1
1.5
23. Crayfish
0.5
1
1.5
24. Amphibians
0.5
1
1.5
25. Algae
0
0.5 1
1 1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other 0
"perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: P,
ops-nrleCA" TM 01 0
Sketch:
NC DWQ Stream Identification Form Version 4.11
Date:
Project/Site: G � Sit-' '
n cir e4f ..
Latitude:
Evaluator:
v
County: e.,
Longitude:
0
1
2
Total Points: 2�6
Stream Determina 'on circle one)
other 51 lr_.i€aM
Stream is at least intermittent
if? 19 or perennial if? 30`
Ephemeral Inermittent erennial
P
e. Quad Name:
g'
A. Geomorphology (Subtotal = i )
Absent
Weak
Moderate
Strong
1a' Continuity of channel bed and bank
0
1
2
3
2. Sinuosity of channel along thalweg
0
1
Q
3
3. In- channel structure: ex. riffle -pool, step -pool,
ripple -pool sequence
0
1
2
3
4. Particle size of stream substrate
0
1
2
3
5. Active /relict floodplain
0
1
2
3
6. Depositional bars or benches
0
1
2
3
7. Recent alluvial deposits
0
0.5
2
3
8. Headcuts
1
2
3
9. Grade control
0
0`
1
1.5
10. Natural valley
0
1
1.5
11. Second or greater order channel
No qQ
Yes = 3
a artificial ditches are not rated; see discussions in manual
B. Hvdroloav (Subtotal = -1 )
12. Presence of Baseflow
0
1
Q2
3
13. Iron oxidizing bacteria
0
1
2
3
14. Leaf litter
1.5
1
0.5
0
15. Sediment on plants or debris
0
1
1
1.5
16. Organic debris lines or piles
0
0.5
1
1.5
17. Soil -based evidence of high water table?
No "
Yes 3
C. Biology (Subtotal= C:� )
18. Fibrous roots in streambed
3
1
0
19. Rooted upland plants in streambed
0
2
1
0
20. Macrobenthos (note diversity and abundance)
(D
1
2
3
21. Aquatic Mollusks
0
1
2
3
22. Fish
0.5
1
1.5
23. Crayfish
0.5
1
1.5
24. Amphibians
0.5
1
1.5
25. Algae
0.5
1
1.5
26. Wetland plants in streambed
FACW = 0.75; OBL = 1.5 Other =�
"perennial streams may also be identified using other methods. See p. 35 of manual.
Notes: LtT
art _ SE, REQ�.2�,
.
Sketch:
Appendix A
Categorical Exclusion Form for Ecosystem Enhancement
Program Projects
Version 1.4
Note', Only Appendix A should to be submitted (along with any supporting documentation) as the
enwil °onmontai document.
t'ro eC[ Name:
Count Name:
EEP Number:
Project Sponsor:
Hogan Creek Mitigation Project
Surry
94708
Ecosystem Enhancement Program
Project Contact Name:
Julie Cahill
Project Contact Address:
5 Ravenscroft Drive, Asheville, NC 28801
Project Contact E -mail:
julie.cahill @ncdenr.gov
EEP Proiect Manager:
Julie Cahill
Reviewed By:
6 Version 1.4, 8118105
APPENDIX C
MITIGATION WORK PLAN DATA AND ANALYSIS
Existing Conditions Data
Existing, Design and Reference Morphology Parameters
Parameter
Existing Stream
Design Stream
Reference Stream
Min
I Median
I Max
Min
I Median
I Max
Min
I Median
I Max
Stream name
Hogan Creek
Hogan Creek
Mill Branch
Stream type
C4
C4
C4
Drainage area, DA (sq mi)
2.37
2.37
5
Mean riffle depth, dbkf (ft)
2.1
1.9
2.0
1.8
1.9
2.0
1.9
2.0
2.2
Riffle width, Wbkf (ft)
21.5
25.7
29.7
22.5
23.3
24.0
27.2
30.4
33.6
Width -to -depth ratio, [Wbkfldbkf]
10.3
13.6
14.9
12.5
12.3
12.1
14.5
15.0
15.6
Riffle cross - section area, Abkf (sq ft)
45.1
48.6
59.3
40.6
44.1
47.6
50.8
61.6
72.4
Max riffle depth, dmbkf (ft)
2.5
2.7
3.2
2.5
2.6
2.8
2.4
2.5
2.7
Max riffle depth ratio, [dmbkfldbkf]
1.2
1.4
1.6
1.4
1.4
1.4
1.3
1.4
1.4
Mean pool depth, db.kfp (ft)
2.2
2.5
2.9
2.6
2.6
2.6
2.3
2.4
2.6
Mean pool depth ratio, [db.kfp /dbkf]
1.0
1.3
3.0
1.4
1.4
3.0
1.2
1.3
1.4
Pool width, Wb.kfp (ft)
28.1
31.4
34.8
34.0
35.0
36.0
20.1
22.3
24.4
Pool width ratio, [Wb.kfpNUbkf]
1.3
1.2
1.2
1.5
1.5
1.5
0.7
0.8
0.9
Pool cross - section area, &kfp (sq ft)
61.4
80.6
99.8
92.0
92.0
92.0
51.5
53.4
55.4
Pool area ratio, [Ab.kfp /Ab.kf]
1.4
1.7
1.7
2.3
2.1
1.9
1.0
1.1
1.1
Max pool depth, dmbkfp (ft)
4.0
4.3
4.7
4.0
4.0
4.0
3.4
3.5
3.5
1
Max pool depth ratio, [dmbkfp /dbkf)
1.9
2.3
2.3
2.2
2.1
2.0
1.8
1.8
1.9
Low bank height, LBH (ft)
3.14
3.4
4.6
2.5
2.7
2.8
2.4
2.5
2.56
Low bank height ratio, [LBH /d,,b.kf]
1.3
1.3
1.4
1.0
1.0
1.0
1.0
1.0
1.1
Width flood -prone area, Wfpa (ft)
178
220
246
100
150
200
72.1
72.3
72.5
Entrenchment ratio, ER [Wfpa/Wbkf]
8.3
8.6
8.3
4.4
6.5
8.3
2.7
2.7
2.7
Meander length, L,, (ft)
133
297
479
133
311
325
81
81
81
Meander length ratio [L,,/Wb.kf]
6.2
11.6
16.1
5.9
13.4
13.5
3.0
3.0
3.0
Radius of curvature, Rc (ft)
20
29
52
67
73
101
19.6
22.7
25.8
Radius of curvature ratio [Rc/Wb.kf]
0.9
1.1
1.8
3.0
3.1
4.2
0.7
0.8
0.9
Belt width, Wbit (ft)
44
65
117
48
88
126
86
86
86
Meander width ratio [WNt/Wb.kf]
2.0
2.5
3.9
2.1
3.8
5.3
3.2
3.2
3.2
Valley length, VL (ft)
2525
2525
4730
Stream centerline length, SL (ft)
2762
2897
327
Valley Elevation Change, VE (ft)
18
18
60
Stream Elevation Change, SE (ft)
17.56
17.96
3.29
Valley slope, VS (ft/ft)
0.0071
0.0071
0.0127
Average water surface slope, S (ft/ft)
0.0064
0.0062
0.0101
Sinuosity, k = VS /S
1.12
1.15
1.26
Riffle slope, Srif (ft/ft)
0.0100
0.0240
0.0550
0.0067
0.0100
0.0132
0.0194
0.0201
0.0207
Riffle slope ratio, [Srif /S]
1.6
3.8
8.7
1.1
1.6
2.1
1.9
2.0
2.1
Pool slope, Sp (ft/ft)
0.0000
0.0010
0.0070
0.0010
0.0012
0.0013
0.0003
0.0013
0.0022
Pool slope ratio, [Sp /S]
0.0
0.2
1.1
0.2
0.2
0.2
0.0
0.2
0.3
D5o riffle (mm)
30
30
40
D5o bar (mm)
28
28
20
Dfoo bar (mm)
116
116
94
w
O
L
a
aA
a�
3
L
•V
W
Y
4l
4l
i
V
ca
dA
W
J
cW
C
Q
N �
U Q
W W
7 �
N � Q
v 3 N ti
z
?i � XTL XTL X XTL XTL XTL X �
v1 O in O In O in O
00 00 Obi a) a) a) a) a)
ti ti
(11) uolIeA@13
O
O
O
O
Ln
m
O
O
O
m
0
Ln
N
E
O 0
O C
N ++
f6
V)
00
ti
O
O
O
ti
O
O
Ln
O
y
T- 7-
(11) uoi }enaI-q
0
0
i§
M
9
W
N
U
0
N
. 0
2
N
O
fn
4-a
(-
�
Q
C
CU
m
Ln
N
N
O
N
T- 7-
(11) uoi }enaI-q
0
0
i§
M
9
W
N
U
0
N
. 0
2
N
O
fn
4-a
(-
�
Q
C
CU
m
Ln
N
O
N
T- 7-
(11) uoi }enaI-q
0
0
i§
M
9
W
N
U
0
N
. 0
2
O
�
�
O
O
T- 7-
(11) uoi }enaI-q
0
0
i§
M
9
W
N
U
0
N
. 0
2
I
(D II
ca
0000"%%
O
� O
0� oc)
Q.
N
`.0000 II
(11) uoi }enaI-q
i
9
s
U
cu
Q
cu
0
N
.0
2
cn
4-a
L
O
Q
CU
C
.
o
C
O
C�
0
(11) uoi }enaI-q
i
9
s
U
cu
Q
cu
0
N
.0
2
N
N
rn
Cn
N
di
C
�
II
� U
Q
X
W
�_
>� O
■
o
L
*%M.0000
�
N
N
N
c
�_ II
Cn
o
C
O
� U
Q
X
C:
_0
(a ,
O
T-
(11) uoi }enaI-q
J
N
v
U
cn
i5
c�
�--0
O
N
.L
O
2
N
c
�_ II
O 4-a
C
O
O
T-
(11) uoi }enaI-q
J
N
v
U
cn
i5
c�
�--0
O
N
.L
O
2
C:
di
N
cn
�_ II
O y-�
C
V
O
II
ca
`r
4--
U)
0000"%%
ma
(D -I-'
C:
0���
O
*%ft.0000
N
Mw
II
Cn
L
�e
C
c�
C:
N
cn
�_ II
O y-�
C
O
O
I
I
LO
O
O
T-
(11) uoi }enaI-q
i
9
W
U
cu
Q
c�
0
N
.0
2
O
T- 7-
(11) uoi }enaI-q
0
cfi
N
LO
(6
U
cu
Q
O
N
.L
O
2
c�
c N
�_ II
rn
N
Ln
II
�
W
C/)
C:
O
>�
*%M.0000
N
'^
V
II
4-4
♦
C/)
4--
(a
Q
C
(u
O
T- 7-
(11) uoi }enaI-q
0
cfi
N
LO
(6
U
cu
Q
O
N
.L
O
2
� l9
c N
�_ II
O 4-4
C
O
O
T- 7-
(11) uoi }enaI-q
0
cfi
N
LO
(6
U
cu
Q
O
N
.L
O
2
co
II
Ln
i
O
(D
di
�
II
`
4-�
U)
m
0000"%% '
W
�_
�C:
L�
>� O
>
Tt1
VJ
C/)
o
L
`.0000
►
N
co
II
i
O
4-a
-1.4
X
U
Q
C:
(u
m
Ln
Tt1
VJ
C/)
N
Oo
�
II
O
O
m 00 00 00
m m m m
(11) uoi }enaI-q
0
—LO
N
-LO
O
—O
-LO
U
cu
i5
cu
O
N
L-
0
2
r
r
cn
O
4-�
x
U
di
U
C
II
ca
rn
N
`--
4-�
00
on'�
W
U
c
HO
N
._
n
I
L
O
I
00
00
CD
r
r
cn
O
4-�
x
U
Q
clul�
m C:
C
Cl)
rn
N
C:
I I
00
7
O
I
O
I
00
00
CD
00 00 00
m m m
(11) uoi }enaI-q
i
i
LO
O
O
00
U
cu
Q
cu
O
N
.O
N
di
Ln
N
U
II
ca
N cn
O
i n
�
U
Q
C:
CU
N
I
cn
°�
X
�
U
Q
C:
CU
-0
C
m
�
OC)
cn
N
0
�
II
O
O
m 00 00 00 ti
m m m m m
(11) uoi }enaI-q
i
0
LO
O
LO
ti
U
cu
Q
ca
O
N
.L
O
2
0 o rn rn rn rn
(11) uoi }enaI-q
i
i
A
In
9
U
O
N
.L
O
2
N
nV♦
W
E
m
cn
C:
�O
n
oc)
cn
U
Q
CU
(a
C
m
C
ry
cn
�
C:
�°
4-�
CU
0
CD
T
o
0 o rn rn rn rn
(11) uoi }enaI-q
i
i
A
In
9
U
O
N
.L
O
2
RIVERMORPH PARTICLE SUMMARY
River Name:
Hogan Creek
Reach Name:
Reach 1
Sample Name:
Hogan Reach 1 Bar
Survey Date:
03/08/2011
SIEVE (mm) NET WT
31.5
4485.2
16
2587.3
8
1532.2
4
967.3
2
785.1
PAN
1229
D16 (mm)
4.39
D35 (mm)
16.59
D50 (mm)
28.44
D84 (mm)
86.68
D95 (mm)
106.84
D100 (mm)
116
Silt/Clay ( %)
0
Sand ( %)
9.33
Gravel ( %)
69.63
Cobble ( %)
21.04
Boulder ( %)
0
Bedrock ( %)
0
Total Weight = 13178.8000.
Largest Surface Particles:
Size(mm) Weight
Particle 1: 116 950.9
Particle 2: 111 641.8
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary% 20Data /hogan %20reach %201 %20bar.tat[10 /4/2011 2:53:20 PM]
RIVERMORPH PARTICLE SUMMARY
River Name:
Hogan Creek
Reach Name:
Reach 1
Sample Name:
Hogan Reach 1 pebble, 200' d/s of UT 1
Survey Date:
03/08/2011
Size (mm) TOT # ITEM % CUM %
0-0.062
0 0.00
0.00
0.062 - 0.125
0 0.00
0.00
0.125-0.25
0 0.00
0.00
0.25-0.50
2 1.92
1.92
0.50 - 1.0
0 0.00
1.92
1.0-2.0
1 0.96
2.88
2.0-4.0
1 0.96
3.85
4.0 - 5.7
1 0.96
4.81
5.7- 8.0
3 2.88
7.69
8.0 - 11.3
4 3.85
11.54
11.3 -16.0
12 11.54
23.08
16.0-22.6
13 12.50
35.58
22.6-32.0
19 18.27
53.85
32-45
18 17.31
71.15
45-64
11 10.58
81.73
64-90
4 3.85
85.58
90- 128
11 10.58
96.15
128- 180
3 2.88
99.04
180-256
1 0.96
100.00
256-362
0 0.00
100.00
362- 512
0 0.00
100.00
512- 1024
0 0.00
100.00
1024- 2048
0 0.00
100.00
Bedrock
0 0.00
100.00
D16 (mm)
13.12
D35 (mm)
22.29
D50 (mm)
30.02
D84 (mm)
79.33
D95 (mm)
123.87
D100 (mm)
255.99
Silt/Clay ( %)
0
Sand ( %)
2.88
Gravel ( %)
78.85
Cobble ( %)
18.27
Boulder ( %)
0
Bedrock ( %)
0
Total Particles = 104.
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary% 20Data /hogan %20reach %201 %20zigzag.txt[10 /4/2011 2:53:20 PM]
RIVERMORPH PARTICLE SUMMARY
River Name:
Hogan Creek
Reach Name:
Reach 2
Sample Name:
Bar sample by zigzag 2
Survey Date:
04/08/2011
SIEVE (mm) NET WT
31.5
2592.3
16
2350.6
8
1500.3
4
1031
2
968.1
PAN
1303.3
D16 (mm)
2.94
D35 (mm)
10.93
D50 (mm)
20.61
D84 (mm)
89.3
D95 (mm)
122.78
D100 (mm)
138
Silt/Clay ( %)
0
Sand ( %)
11.85
Gravel ( %)
69.96
Cobble ( %)
18.2
Boulder ( %)
0
Bedrock ( %)
0
Total Weight = 11002.9000.
Largest Surface Particles:
Size(mm) Weight
Particle 1: 138 676.5
Particle 2: 122 580.8
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary% 20Data /hogan %20reach %202 %20bar.tat[10 /4/2011 2:53:20 PM]
RIVERMORPH PARTICLE SUMMARY
River Name:
Hogan Creek
Reach Name:
Reach 2
Sample Name:
Zigzag at Riffle
Survey Date:
04/08/2011
Size (mm) TOT # ITEM % CUM %
0-0.062
0 0.00
0.00
0.062 - 0.125
0 0.00
0.00
0.125-0.25
0.00
0.00
0.25-0.50
0 0.00
0.00
0.50 - 1.0
0 0.00
0.00
1.0-2.0
1 0.99
0.99
2.0-4.0
0 0.00
0.99
4.0 - 5.7
2 1.98
2.97
5.7- 8.0
1 0.99
3.96
8.0 - 11.3
7 6.93
10.89
11.3 -16.0
11 10.89
21.78
16.0-22.6
15 14.85
36.63
22.6-32.0
17 16.83
53.47
32-45
13 12.87
66.34
45-64
13 12.87
79.21
64-90
10 9.90
89.11
90- 128
9 8.91
98.02
128- 180
2 1.98
100.00
180-256
0 0.00
100.00
256-362
0 0.00
100.00
362- 512
0 0.00
100.00
512- 1024
0 0.00
100.00
1024- 2048
0 0.00
100.00
Bedrock
0 0.00
100.00
D16 (mm)
13.51
D35 (mm)
21.88
D50 (mm)
30.06
D84 (mm)
76.58
D95 (mm)
115.12
D100 (mm)
180
Silt/Clay ( %)
0
Sand ( %)
0.99
Gravel ( %)
78.22
Cobble ( %)
20.79
Boulder ( %)
0
Bedrock ( %)
0
Total Particles = 101.
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary% 20Data /hogan %20reach %202 %20zigzag.txt[10 /4/2011 2:53:20 PM]
RIVERMORPH PARTICLE SUMMARY
River Name: Hogan Creek
Reach Name: Supply Reach
Sample Name: Bar sample by zigzag supply riff
Survey Date: 04/08/2011
SIEVE (mm) NET WT
31.5
1302.6
16
2581.1
8
1698.8
4
1064.9
2
869
PAN
1491
D16 (mm)
2.39
D35 (mm)
8.96
D50 (mm)
16.37
D84 (mm)
68.67
D95 (mm)
110.83
D100 (mm)
130
Silt/Clay ( %)
0
Sand ( %)
14.38
Gravel ( %)
72.77
Cobble ( %)
12.85
Boulder ( %)
0
Bedrock ( %)
0
Total Weight = 10369.4000.
Largest Surface Particles:
Size(mm) Weight
Particle 1: 130 1012
Particle 2: 90 350
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary% 20Data /hogan %20supply %20bar.txt[10 /4/2011 2:53:21 PM]
RIVERMORPH PARTICLE SUMMARY
River Name: Hogan Creek
Reach Name: Supply Reach
Sample Name: Zigzag at supply riffle
Survey Date: 04/08/2011
Size (mm) TOT # ITEM % CUM %
0-0.062
0 0.00
0.00
0.062 - 0.125
0 0.00
0.00
0.125-0.25
1 0.97
0.97
0.25-0.50
0 0.00
0.97
0.50 - 1.0
0 0.00
0.97
1.0-2.0
0 0.00
0.97
2.0-4.0
0 0.00
0.97
4.0 - 5.7
3 2.91
3.88
5.7- 8.0
3 2.91
6.80
8.0 - 11.3
4 3.88
10.68
11.3 -16.0
12 11.65
22.33
16.0-22.6
14 13.59
35.92
22.6-32.0
16 15.53
51.46
32-45
14 13.59
65.05
45-64
19 18.45
83.50
64-90
9 8.74
92.23
90- 128
6 5.83
98.06
128- 180
2 1.94
100.00
180-256
0 0.00
100.00
256-362
0 0.00
100.00
362- 512
0 0.00
100.00
512- 1024
0 0.00
100.00
1024- 2048
0 0.00
100.00
Bedrock
0 0.00
100.00
D16 (mm)
13.45
D35 (mm)
22.15
D50 (mm)
31.12
D84 (mm)
65.49
D95 (mm)
108.05
D100 (mm)
180
Silt/Clay ( %)
0
Sand ( %)
0.97
Gravel ( %)
82.53
Cobble ( %)
16.5
Boulder ( %)
0
Bedrock ( %)
0
Total Particles = 103.
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary% 20Data /hogan %20supply %20zigzag.txt[10 /4/2011 2:53:21 PM]
(11) uoi }enaI-q
El I
s�
U
cu
Q
cu
O
N
L-
0
2
C)
O
II
U
cu
4-a
I
U
�
O
�L
4-�
C/)
O
4--
ca
C
X
m
C:
r
�
cn
II
0
o
4a
O
C�
0
(11) uoi }enaI-q
El I
s�
U
cu
Q
cu
O
N
L-
0
2
Existing, Design and Reference Morphology Parameters
Parameter
Existing Stream
Design Stream
Reference Stream
Min
Median
Max
Min
Median
Max
Min
I Median
Max
Stream name
UT2
UT2
UT2 Upstream
Stream type
E4b
B4
E4b
Drainage area, DA (sq mi)
0.13
0.13
0.12
Mean riffle depth, dbkf (ft)
1.5
0.7
0.9
Riffle width, Wbkf (ft)
8.2
9.0
7.1
Width -to -depth ratio, [Wbkfldbkf]
5.6
12.5
7.6
Riffle cross - section area, Abkf (sq ft)
12.1
6.5
6.6
Max riffle depth, dmbkf (ft)
2.1
1.0
1.2
Max riffle depth ratio, [dmbkfldbkf]
1.4
1.4
1.3
Mean pool depth, db.kfp (ft)
1.5
1.1
1.1
Mean pool depth ratio, [db.kfp /dbkf]
1.0
1.5
1.2
Pool width, Wb.kfp (ft)
9.3
12.0
6.8
Pool width ratio, [Wb.kfpNUbkf]
1.1
1.3
1.0
Pool cross - section area, &kfp (sq ft)
14.4
12.8
7.3
Pool area ratio, [Ab.kfp /Ab.kf]
1.2
2.0
1.1
Max pool depth, dmbkfp (ft)
2.7
1.6
1.5
1
Max pool depth ratio, [dmbkfp /dbkf)
1.8
2.2
1.6
Low bank height, LBH (ft)
3.2
1.0
1.2
Low bank height ratio, [LBH /d,,b.kf]
1.6
1.0
1.0
Width flood -prone area, Wfpa (ft)
66.0
30.0
15.0
Entrenchment ratio, ER [Wfpa/Wbkf]
8.0
3.3
2.1
Meander length, L,, (ft)
128
159
190
73
103
130
53
58.5
64
Meander length ratio [L,,/Wb.kf]
15.6
19.4
23.2
8.1
11.4
14.4
7.5
8.2
9.0
Radius of curvature, Rc (ft)
16
18.5
21
22
27
30
7
16
25
Radius of curvature ratio [Rc/Wb.kf]
2.0
2.3
2.6
2.4
3.0
3.3
1.0
2.3
3.5
Belt width, Wbit (ft)
28
42
56
17
26
49
62
67.5
73
Meander width ratio [WHt/Wb.kf]
3.4
5.1
6.8
1.9
2.9
5.5
8.7
9.5
10.3
Valley length, VL (ft)
641
641
1350
Stream length, SL (ft)
568
555
1980
Valley Elevation Change, VE (ft)
20
20
48
Stream Elevation Change, SE (ft)
13.33
12.35
52
Valley slope, VS (ft/ft)
0.0312
0.0312
0.0356
Average water surface slope, S (ft/ft)
0.0235
0.0223
0.0263
Sinuosity, k = VS /S
1.33
1.40
1.47
Riffle slope, Srif (ft/ft)
0.0303
0.0326
0.0561
0.0267
0.0323
0.0378
0.0227
0.0334
0.0363
Riffle slope ratio, [Srif /S]
1.3
1.4
2.4
1.2
1.5
1.7
0.9
1.3
1.4
Pool slope, Sp (ft/ft)
- 0.0036
0.0028
0.0069
0.0030
0.0045
0.0060
0.0008
0.0027
0.0118
Pool slope ratio, [Sp /S]
-0.2
0.1
0.3
0.1
0.2
0.3
0.0
0.1
0.5
D5o riffle (mm)
21
21
40
D5o bar (mm)
8
8
20
Dfoo bar (mm)
84
84
94
(:y) uOi;ena13
v
V
f0
7 ao
N
v 3
x X
I I
ON
O
O
O
00
0
,
a
�
oo
(L)
3
s
H
S
0 °
W
�
N
MA
�X
W
N
H
°O
Zt
°O
N
O
O O 01 01 00 00
O O a> a> a> a>
(:y) uOi;ena13
CD
4-4
N
U
N
cu
XCU
U
i C/)
C:
O
n
OC)
cn
CD
4-4
�o�
�
U
-Q
Q
70
XCU
m
N
N
cn
o
C
O
c�
0
(11) uoi }enaI-q
H
W
U
cu
Q
0
N
L-
0
0
0
(11) uoi }enaI-q
loo
i
U
cu
Q
0
0
N
L-
0
di
di
0
ca
II
`r
4--
(i c
�
0000"%%
O
di
Ln
0 ►
�,
0
11
0
0
(11) uoi }enaI-q
loo
i
U
cu
Q
0
0
N
L-
0
CU
Q
CU
70
m
�
N
N
'
�cn
�
II
0
C
0
c�
0
0
0
(11) uoi }enaI-q
loo
i
U
cu
Q
0
0
N
L-
0
W
H
. L
a)
C.)
C:
a)
L
4-
a)
L
N
D
1
U II
ca �
U
" C/)
O
rn
o Q
CU C:
cn II
C
O
c�
0
(11) uoi }enaI-q
U
cu
Q
O
N
.L
O
Q9
N
V
nC:
W
L
W
L
C/) 4-�
CU Q
CU70
CU m OC)
N`n
� II
C
0
c�
0
(11) uoi }enaI-q
U
cu
-1--+
Q
0
N
L-
0
0
II
LE
4-�
V
nC:
W
L
W
L
C/) 4-�
CU Q
CU70
CU m OC)
N`n
� II
C
0
c�
0
(11) uoi }enaI-q
U
cu
-1--+
Q
0
N
L-
0
RIVERMORPH PARTICLE SUMMARY
River Name:
Hogan Creek
Reach Name:
UT2
Sample Name:
zigzag near ref riffle
Survey Date:
09/12/2011
Size (mm) TOT # ITEM % CUM %
0-0.062
0 0.00
0.00
0.062 - 0.125
0 0.00
0.00
0.125-0.25
0 0.00
0.00
0.25-0.50
3 2.86
2.86
0.50 - 1.0
4 3.81
6.67
1.0 -2.0
2 1.90
8.57
2.0-4.0
6 5.71
14.29
4.0 - 5.7
4 3.81
18.10
5.7- 8.0
6 5.71
23.81
8.0 - 11.3
8 7.62
31.43
11.3 -16.0
14 13.33
44.76
16.0-22.6
7 6.67
51.43
22.6-32.0
6 5.71
57.14
32-45
8 7.62
64.76
45-64
11 10.48
75.24
64-90
8 7.62
82.86
90- 128
7 6.67
89.52
128- 180
5 4.76
94.29
180-256
2 1.90
96.19
256-362
1 0.95
97.14
362- 512
0 0.00
97.14
512- 1024
1 0.95
98.10
1024- 2048
0 0.00
98.10
Bedrock
2 1.90
100.00
D16 (mm)
4.76
D35 (mm)
12.56
D50 (mm)
21.19
D84 (mm)
96.5
D95 (mm)
208.4
D100 (mm)
Bedrock
Silt/Clay ( %)
0
Sand ( %)
8.57
Gravel ( %)
66.67
Cobble ( %)
20.95
Boulder ( %)
1.91
Bedrock ( %)
1.9
Total Particles = 105.
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary %20Data /ut2 %20zigzag.tat[10 /4/2011 2:53:22 PM]
RIVERMORPH PARTICLE SUMMARY
River Name:
Hogan Creek
Reach Name:
UT2
Sample Name:
Bar sample us reach
Survey Date:
09/15/2011
SIEVE (mm) NET WT
16
508.6
8
509.1
4
420.8
2
467.2
PAN
477.1
D 16 (mm)
0
D35 (mm)
4.23
D50 (mm)
8.29
D84 (mm)
50.29
D95 (mm)
73.46
D100 (mm)
84
Silt/Clay ( %)
0
Sand ( %)
17.24
Gravel ( %)
77.47
Cobble ( %)
5.29
Boulder ( %)
0
Bedrock ( %)
0
Total Weight = 2767.2000.
Largest Surface Particles:
Size(mm) Weight
Particle 1: 84 146.1
Particle 2: 80 238.3
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary %20Data /ut2 %20bar.txt[10 /4/2011 2:53:22 PM]
Existing, Design and Reference Morphology Parameters
Parameter
Existing Stream
Design Stream
Reference Stream
Min
Median
Max
Min
Median
Max
Min
I Median
I Max
Stream name
UT3
UT3
Upstream UT3
Stream type
G4
B4
E4b
Drainage area, DA (sq mi)
0.03
0.03
0.02
Mean riffle depth, dbkf (ft)
0.9
0.4
1.0
Riffle width, Wbkf (ft)
5.9
5.0
5.8
Width -to -depth ratio, [Wbkfldbkf]
6.3
12.5
6.1
Riffle cross - section area, Abkf (sq ft)
5.5
2.0
5.6
Max riffle depth, dmbkf (ft)
1.4
0.5
1.3
Max riffle depth ratio, [dmbkfldbkf]
1.5
1.3
1.4
Mean pool depth, db.kfp (ft)
1.0
0.7
1.0
Mean pool depth ratio, [db.kfp /dbkf]
1.0
1.7
1.0
Pool width, Wb.kfp (ft)
7.0
8.0
7.0
Pool width ratio, [Wb.kfpNUbkf]
1.2
1.6
1.2
Pool cross - section area, &kfp (sq ft)
6.8
5.5
6.8
Pool area ratio, [Ab.kfp /Ab.kf]
1.2
2.8
1.2
Max pool depth, dmbkfp (ft)
1.6
1.0
1.6
1
Max pool depth ratio, [dmbkfp /dbkf)
1.7
2.5
1.6
Low bank height, LBH (ft)
4.4
0.5
1.9
Low bank height ratio, [LBH /d,,b.kf]
3.2
1.0
1.5
Width flood -prone area, Wfpa (ft)
12.0
20.0
31.0
Entrenchment ratio, ER [Wfpa/Wbkf]
2.1
4.0
5.3
Meander length, L,, (ft)
75.0
64
70
76
78.0
128.5
179.0
Meander length ratio [L,,/Wb.kf]
12.8
12.8
14.0
15.2
15.6
25.7
35.8
Radius of curvature, Rc (ft)
11.0
16
17
29
14.0
21.0
28.0
Radius of curvature ratio [Rc/Wb.kf]
1.9
3.2
3.4
5.7
2.8
4.2
5.6
Belt width, Wbit (ft)
26.0
22
25
27
47.0
55.5
64.0
Meander width ratio [WHt/Wb.kf]
4.4
4.4
5.0
5.4
9.4
11.1
12.8
Valley length, VL (ft)
290
290
697
Stream length, SL (ft)
298
292
925
Valley Elevation Change, VE (ft)
9
9
40
Stream Elevation Change, SE (ft)
9
7.76
41
Valley slope, VS (ft/ft)
0.0310
0.0310
0.0574
Average water surface slope, S (ft/ft)
0.0302
0.0266
0.0443
Sinuosity, k = VS /S
1.03
1.17
1.29
Riffle slope, Srif (ft/ft)
0.0247
0.1447
0.3831
0.0254
0.0317
0.0381
0.0247
0.1181
0.2115
Riffle slope ratio, [Srif /S]
0.8
4.8
12.7
1.0
1.2
1.4
0.6
2.7
4.8
Pool slope, Sp (ft/ft)
0.0038
0.0098
0.0126
0.0013
0.0013
0.0013
0.0038
0.0060
0.0082
Pool slope ratio, [Sp /S]
0.1
0.3
0.4
0.0
0.0
0.0
0.1
0.2
0.3
D5o riffle (mm)
14
14
14
D5o bar (mm)
2
2
2
Dfoo bar (mm)
65
65
65
O
L
aAA
^ 0
W
3
s`
F-
b.0
X
W
M
H
a)
U
f6
i
to
a) O
(6 a I
s
4- X
I
N O 00 to ZT N O
Ol Ol 00 00 00 00 00
Ol Ol Ol Ol Ol Ol M
(11) UOIIEAD13
O
Ln
m
O
O
m
O
Ln
N
O
O
N
r_
O
ca
N
O
Ln
-i
O
O
O
Ln
O
0
Q0
4-�
di
O
N
`n
CU
�
II
V,
U
�
,000=.%s
n '
N C
_
W
O
L�
>
o0
M
II
`.0000
0
i
W
H
. L
U
L
W
L
M
Ln
Ln
U II
LE 4-�
U)
O
rn
O Q
-�e 0
� -0
CU
m C: N
Ln
cn
1--j II
C
O
c�
0
(11) uoi }enaI-q
El I
0
9
9
U
cu
Q
0
N
L-
0
L)
L
L
O Q
� ca
70
CU
CU
o,
M`n
� II
C
O
c�
0
(11) uoi }enaI-q
W-
In
5
9
A
U
cu
Q
O
N
L-
0
U
II
LE
4-�
O
U)
^
� O
rn
L)
L
L
O Q
� ca
70
CU
CU
o,
M`n
� II
C
O
c�
0
(11) uoi }enaI-q
W-
In
5
9
A
U
cu
Q
O
N
L-
0
RIVERMORPH PARTICLE SUMMARY
River Name:
Hogan Creek
Reach Name:
UT3
Sample Name:
zigzag thru ref riffle
Survey Date:
09/12/2011
Size (mm) TOT # ITEM % CUM %
0-0.062
0 0.00
0.00
0.062 - 0.125
0 0.00
0.00
0.125-0.25
4 3.92
3.92
0.25-0.50
6 5.88
9.80
0.50 - 1.0
5 4.90
14.71
1.0-2.0
1 0.98
15.69
2.0-4.0
2 1.96
17.65
4.0 - 5.7
8 7.84
25.49
5.7- 8.0
9 8.82
34.31
8.0 - 11.3
10 9.80
44.12
11.3 -16.0
11 10.78
54.90
16.0-22.6
15 14.71
69.61
22.6-32.0
8 7.84
77.45
32-45
3 2.94
80.39
45-64
10 9.80
90.20
64-90
6 5.88
96.08
90- 128
2 1.96
98.04
128- 180
1 0.98
99.02
180-256
1 0.98
100.00
256-362
0 0.00
100.00
362- 512
0 0.00
100.00
512- 1024
0 0.00
100.00
1024- 2048
0 0.00
100.00
Bedrock
0 0.00
100.00
D16 (mm)
2.32
D35 (mm)
8.23
D50 (mm)
13.86
D84 (mm)
51.99
D95 (mm)
85.22
D100 (mm)
255.99
Silt/Clay ( %)
0
Sand ( %)
15.69
Gravel ( %)
74.51
Cobble ( %)
9.8
Boulder ( %)
0
Bedrock ( %)
0
Total Particles = 102.
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary %20Data /ut3 %20zigzag.tat[10 /4/2011 2:53:22 PM]
RIVERMORPH PARTICLE SUMMARY
River Name:
Hogan Creek
Reach Name:
UT3
Sample Name:
Bar sample us reach
Survey Date:
09/12/2011
SIEVE (mm) NET WT
16
150.1
8
258.3
4
280
2
346.1
PAN
1346.1
D 16 (mm)
0
D35 (mm)
0
D50 (mm)
0
D84 (mm)
13.94
D95 (mm)
46.74
D100 (mm)
65
Silt/Clay ( %)
0
Sand ( %)
52.25
Gravel ( %)
47.6
Cobble ( %)
0.15
Boulder ( %)
0
Bedrock ( %)
0
Total Weight = 2576.2000.
Largest Surface Particles:
Size(mm) Weight
Particle 1: 65 116.7
Particle 2: 64 78.9
file :IHWI /Projects/Hogan %20Creek/ Assessment / Geomorphic% 20Summary %20Data /ut3 %20bar.txt[10 /4/2011 2:53:23 PM]
Hydraulic Analyses — Flood Attenuation
/\\
/ \/
;i \ ��
8
G
8
/
17
CD
c
/
g
5
x
0
$
0
% {
//
R
\
�
°
co
CL
�0
$
%
o
$
�
2
\
�
2
�
0
e
O
o
7
\
\
ƒ
\
\
\ \ \
\
U um mg
/\\
/ \/
;i \ ��
/
\\
\\
\;/
/
\/
\ ®\
:2
�
;i
\ :6
;�
:�
S
G
\
6
CD
e
e
\
§
\
_
$
2
% E
/
\
@ §
°
k �
E7
F
0
f
_ .
}
\
)
} \
\
0
2
\
17
2
O
g
%
9
E
I
;
co
\
\
\ \ \
\
U uq mg
/
\\
\\
\;/
/
\/
\ ®\
:2
�
;i
\ :6
;�
:�
\.;\
\\
/
/ \,/
�
m
:�
@
2 LU
i
\
8
G
\
%
G
k
g
E
LO
\
o
m
/
ƒ 0
C
\
R
e
9
:
co
�22
/
CL
{ >
U)
$
e
LO
\
�
7
�
\
2
$
e
O
§
%
9
E
I
$
\
\
\
\ \
\ (
U u@ mg
�
:�
d � C1 C> 1 -6
� d Cy
x Cy
J
w W
V
r
O LN n
O
N
C) r
O
C) r
O
C
>
N N
o y
°O
O
4-- O
O o-
0
N
0)
v
cL
o
co
N
O
LO
Q
N
UO
)
7
U)
co
0
N
O
'
CC
O
LLv O
J
Y
N
N L
U co
�
o
co
0)
O
2
O LO
0)
O O
0)
rn 00 00 00 0� 00
0) 0) 0) 0) 0) 0)
(; ;) uol;en913
m
>
r
r
O
N
LO
O
r
O)
C
N
X
N
O
O
N
0)
c
co
L
co
,o7
VJ
co
y-+
0
y-+
J
Y
N
N
L
U
c
co
0)
co
2
.N
r
r
O
N
LO
O
r
O)
C
N
X
N
O
O
N
0)
c
co
L
co
,o7
VJ
co
y-+
0
y-+
J
Y
N
N
L
U
c
co
0)
co
2
r
r
O
N
LO
O
r
C
O)
N
N
O
O
N
O)
C
co
L
co
,o7
VJ
co
y-+
0
y-+
J
Y
N
N
L
U
c
co
0)
co
2
.N
r
r
O
N
LO
O
r
C
O)
N
N
O
O
N
O)
C
co
L
co
,o7
VJ
co
y-+
0
y-+
J
Y
N
N
L
U
c
co
0)
co
2
Section Design and Sediment Transport Analyses
Hogan Creek Reach 1 Typical Section Design
RIFFLE SECTION Regional Curve Estimate Hogan Creek to Miller Gap bridge
Right Bank Slope, x:1
2.5
DA (sq. mi.)
2.31
Left Bank Slope, x:1
2.5
NC Mountains (area)
38.18659
Max Depth (ft)
2.5
NC Mountains (discharge)
190.1585
Bottom Width (ft)
10
Area
40.625
NC rural Piedmont (area)
37.86852
Bankfull Width (ft)
22.5
NC rural Piedmont (discharge)
162.6993
Bankfull Depth (ft)
1.81
W/D ratio
12.46
USGS 2 year discharge
Ave Width (ft) =
NC Hydro Area 1
211
SW Appalachian (area)
58.4128
Discharge Calculation overall reach
SW Appalachian (discharge)
281.117
Q = 1.49/n R" s" A
WP (ft)
23.46
FROM CAD, design tw slope =
0.006959
R (ft)
1.73
design slope
0.0073
existing eg slope from RAS =
0.007881
Channel n
0.035
design eg slope from RAS =
0.007348
Q (cfs) 214
Q (power) 4.36
7Rs = 0.7939221 psf bar sample 1
grain diam, Shields = 120 mm (CO data) d84 =
dloo =
.��eenletzz.��
Right Bank Slope, x:1
Left Bank Slope, x:1
Max Depth (ft)
Bottom Width (ft)
Area
Bankfull Width (ft)
pt bar tob o/s
outside bank tob o/s
OFF -LINE POOL
Right Bank Slope, x:1
Left Bank Slope, x:1
Max Depth (ft)
Bottom Width (ft)
Area
Bankfull Width (ft)
pt bar tob o/s
outside bank tob o/s
3.5
2.5
4
10
88
34
19
15
4
2.5
4
10
92
36
21
15
width ratio =
depth ratio =
width ratio =
depth ratio =
79 mm
256 mm
1.51
2.22
1.60
2.22
< - - -- questionable, more like 130 mm
Andrews (1984) and Andrews and Nankervis (1995)
ti,i* = 0.0834(di/d'50) -0.872
ti,i* = 0.0384(di/d'50) -0.887
di = d50 of riffle pavement (from zigzag), mm
d'5o = d5o of sub - pavement (bar sample), mm
d = 1ciTPsand- Ph20) /Ph2O)*Dj) /s
applies if di /d'50 ranges from 3 to 7
if di /d'50 is 1.3 to 3.0
d = mean bankfull depth of water (ft) needed to move largest particle
Psand = 2.65 g /cc specific gravity of sand
Ph20 = 1.00 g /cc specific gravity of water
Di = largest particle found in bar or subpavement sample (ft)
S = average (bankfull) water surface slope
For Reach 1 sample location
di
30 mm
d'50
28 mm
di /d'50
1.071429 out of range
tici* =
0.036121
Di
116 mm = 0.380577 ft
s
0.0071 ft/ft
d =
3.19 ft
For Hogan supply reach samples
di 31 mm
d'50 16 mm
di /d'50 1.9375
tici* = 0.021357
Di 130 mm = 0.426509 ft
s 0.0071 ft/ft
d = 2.12 ft
from stage report in RM w/ dbkf = d, %
from RAS model of Qbkf for reach 1
215 cfs XS2
290 cfs XS5
237 cfs XS8
Bathurst et al (1987)
gcD50 = (0.15g0.5D501.5)/(S1.12)
gci — gcD50( D i /D 50) b
b = 1.5(D84/D16) -1
Hogan Reach 1 Pebble Count
D50 =
0.03 m
D84 =
0.079 m
D16 =
0.013 m
S =
0.007881
gcD50 =
5.961453 cfs
b =
0.246835
qci =
7.570906 cfs /ft
Active
Channel
Section
Width (ft) q�i (cfs) _
Supply
17.2
130
XS2
21.5
163
XS5
14.6
111
XS8
15.7
119
Dinft
0.0984 ft
0.25912 ft
0.04264 ft
Check discharge for initiation of Phase 2 transport using Bathurst (2007) equations
qc2 = 0.0513 g0 5 D501.5 S -1.2
units of cros; D (m) of the surface material from pebble count
qo2 = 0.0133 g0.5 D841.5 S -1.23
g = 9.81
m /s`
From Hogan Supply Reach:
D50 = 0.031 m
D84 = 0.065 m
S = 0.0079
Bottom Width (active channel) =
17.2 ft
qc2, D50 = 0.292 m " /s /m
0.089 cros /ft =
3.145 cfs /ft
54 cfs
qc2, D84 = 0.266 m' /s /m
0.081 cros /ft =
2.862 cfs /ft
49 cfs
From Hogan XS 2
D50 = 0.03 m
D84 = 0.079 m
S = 0.0079
Bottom Width (active channel) =
21.5 ft
qc2, D50 = 0.278279517 m' /s /m
0.0848413 cros /ft =
2.993842 cfs /ft
64 cfs
qc2, D84 = 0.356488447 m " /s /m
0.1086855 cros /ft =
3.835245 cfs /ft
82 cfs
From Hogan XS 5
D50 = 0.03 m
D84 = 0.079 m
S = 0.0079
Bottom Width (active channel) =
14.6 ft
qc2, D50 = 0.278279517 m " /s /m
0.0848413 cros /ft =
2.993842 cfs /ft
44 cfs
qc2, D84 = 0.356488447 m' /s /m
0.1086855 cros /ft =
3.835245 cfs /ft
56 cfs
From Hogan XS 8
D50 = 0.03 m
D84 = 0.079 m
S = 0.0079
Bottom Width (active channel) =
15.7 ft
qc2, D50 = 0.278279517 m' /s /m
0.0848413 cros /ft =
2.993842 cfs /ft
47 cfs
qc2, D84 = 0.356488447 m " /s /m
0.1086855 cros /ft =
3.835245 cfs /ft
60 cfs
RIFFLE SECTION
Right Bank Slope, x:1
Left Bank Slope, x:1
Max Depth (ft)
Bottom Width (ft)
Area
Bank-full Width (ft)
Bank-full Depth (ft)
W/D ratio
Ave Width (ft) _
Hogan Creek Reach 2 Typical Section Design
Regional Curve Estimate Hogan Creek to downstream end
2.5 DA (sq. mi.) -
2.5 NC Mountains (area) 38.85829
2.8 NC Mountains (discharge) 193.9007
10
47.6
24
1.98
12.10
Discharge Calculation overall reach
Q = 1.49/n R 21 s "2 A
WP (ft)
25.08
R (ft)
1.90
design slopey
Channel n
0.035
Q (cfs)
244
C2 (power)
4
yRs = 0.7283777 psf
grain diam, Shields = 110 mm (CO data)
POOL SECTION
Right Bank Slope, x:1
4
Left Bank Slope, x:1
&25
Max Depth (ft)
Bottom Width (ft)
Area
92
Bank-full Width (ft)
36
pt bar tob o/s
21
outside bank tob o/s
15
NC rural Piedmont (area) 38.53462
NC rural Piedmont (discharge) 165.7311
USGS 2 year discharge
NC Hydro Area 1 215
SW Appalachian (area) 59.47228
SW Appalachian (discharge) 286.5757
Qbkf slope from design model = 0.00615
bar sample 2
d.4 = 89 mm
dloo = 138 mm
width ratio = 1.50
depth ratio = 2.02
Andrews (1984) and Andrews and Nankervis (1995)
ti,i* = 0.0834(di/d'50) -0.872
ti,i* = 0.0384(di/d'50) -0.887
di = d50 of riffle pavement (from zigzag), mm
d'5o = d5o of sub - pavement (bar sample), mm
d = 1ciTPsand- Ph20) /Ph2O)*Dj) /s
applies if di /d'50 ranges from 3 to 7
if di /d'50 is 1.3 to 3.0
d = mean bankfull depth of water (ft) needed to move largest particle
Psand = 2.65 g /cc specific gravity of sand
Ph20 = 1.00 g /cc specific gravity of water
Di = largest particle found in bar or subpavement sample (ft)
S = average (bankfull) water surface slope
For Hogan Reach 2 sample location
di 31 mm
d'50 21 mm
di /d'50 1.47619
tiCi* = 0.027183
Di 138 mm = 0.452756 ft
s 0.0063 ft/ft from RAS model of Qbkf for reach 2
d = 3.22 ft mean bankfull depth
from stage report in RM w/ dbkf = d, % — 356 cfs XS11
Bathurst et al (1987)
gcD50 = (0.15g0.5D501.5)/(S1.12)
gci — gcD50( D i /D 50) b
b = 1.5(D84/D16) -1
Hogan Reach 2 Pebble Count
D50 =
0.03 m
D84 =
0.077 m
D16 =
0.014 m
S =
0.0061
gcD50 =
7.942229 cfs
b =
0.272727
qci =
10.27043 cfs /ft
Active
Channel
Section Width (ft) q�i (cfs) _
XS11 13.8 142
Dinft
0.0984 ft
0.25256 ft
0.04592 ft
Check discharge for initiation of Phase 2 transport using Bathurst (2007) equations:
qc2 = 0.0513 g0 5 D501.5 S -1.2 units of cros; D (m) of the surface material from pebble count
qo2 = 0.0133 g0.5 D841.5 S -1.23 g = 9.81 m /s`
From Hogan Reach 2 (XS11):
D50 = 0.03 m
D84 = 0.077 m
S = 0.0079
Bottom Width (active channel) = 13.8 ft
qc2, D50 = 0.278 m " /s /m 0.085 cros /ft = 2.994 cfs /ft 41 cfs
qc2, D84 = 0.343 m' /s /m 0.105 cros /ft = 3.691 cfs /ft 51 cfs
1.2
1
N 0.s
L
f6
w
N 0.6
M
0.4
0
m
U
N
w
3
0
0
a
E
M
w
L
Hogan Creek - Stage vs. Shear
0 '
0 1 2 3 4 5
Stage (feet)
s
6
5
4
3
2
1
0
0
Hogan Supply
Hogan Reach 1 Design
Hogan Reach 2 Design
Hogan Creek - Stage vs. Unit Stream Power
1 2 3 4 5
Stage (feet)
Hogan Supply
Hogan Reach 1 Design
Hogan Reach 2 Design
UT2 TYPICAL SECTION DESIGN
RIFFLE SECTION Regional Curve Estimates
Right Bank Slope, x:1
2.5
DA (sq. mi.)
Left Bank Slope, x:1
2.5
NC Mountains (area)
Max Depth (ft)
1
NC Mountains (discharge)
Bottom Width (ft)
4
Area
6.5
NC rural Piedmont (area)
Bankfull Width (ft)
9
NC rural Piedmont (discharge)
Bankfull Depth (ft)
0.72
W/D ratio
12.46
USGS 2 year discharge
NC Hydro Area 1
Discharge Calculation overall reach
SW Appalachian (area)
SW Appalachian (discharge)
Q = 1.49/n R2i3 s1i2 A
WP (ft)
9.39
R (ft)
0.69
FROM CAD, design slope =
design slope
0.0223
Channel n
0.04
Q (cfs)
28
bar sample 1
yRs =
0.961682 psf
d84 =
grain diam, Shields =
140 mm (CO data) dloo =
POOL SECTION
Right Bank Slope, x:1
3
Left Bank Slope, x:1
2
Max Depth (ft)
1.6
width ratio = 1.33
Bottom Width (ft)
4
depth ratio = 2.22
Area
12.8
Bankfull Width (ft)
12
pt bar tob o/s
6.8
outside bank tob o/s
5.2
0.126199
5.288994
20.87245
5.244939
20.06068
22
7.611258
31.76657
0.022252
30 mm
84 mm
Andrews (1984) and Andrews and Nankervis (1995)
ti,i* = 0.0834(di/d'50) -0.872
ti,i* = 0.0384(di/d'50) -0.887
di = d50 of riffle pavement (from zigzag), mm
d'5o = d5o of sub - pavement (bar sample), mm
d = 1ciTPsand- Ph20) /Ph2O)*Dj) /s
applies if di /d'50 ranges from 3 to 7
if di /d'50 is 1.3 to 3.0
d = mean bankfull depth of water (ft) needed to move largest particle
Psand = 2.65 g /cc specific gravity of sand
Ph20 = 1.00 g /cc specific gravity of water
Di = largest particle found in bar or subpavement sample (ft)
S = average (bankfull) water surface slope
Using UT2 sediment data from reference reach:
di 21 mm
d'50 8 mm
di /d'50 2.625
tici* = 0.016314
Di 84 mm = 0.275591 ft
s 0.022252 ft/ft
d = 0.33 ft
from stage report in RM w/ dbkf = d, qci — 2.6 cfs xs6
3.0 cfs ref riffle
Bathurst et al (1987)
gcD50 = (0.15905 D501.5)/(S1.12) Din ft
qci — gcD50( D i /D 50) b
b = 1.5(D84/D16) -1
UT2 Reference Riffle
D50 =
0.021 m 0.06888 ft
D84 =
0.097 m 0.31816 ft
D16 =
0.005 m 0.0164 ft
S =
0.022252
gcD50 =
1.091688 cfs
b =
0.07732
qci =
1.2288 cfs /ft
channel width (assumed bottom width) = 6.4 ft
qci =
7.9 cfs
Check discharge for initiation of Phase 2 transport using Bathurst (2007) equations:
qc2 = 0.0513 g0 5 D501.5 S -1.2 units of cros; D (m) of the surface material from pebble count
qo2 = 0.0133 g0.5 D841.5 S -1.23 g = 9.81 m /s`
From UT2 reference reach:
D50 = 0.021 m
D84 = 0.097 m
S = 0.0223
Bottom Width (active channel) = 6.4 ft
qc2, D50 = 0.047 m " /s /m 0.014 cros /ft = 0.506 cfs /ft 3.2 cfs
qc2, D84 = 0.136 m' /s /m 0.041 cros /ft = 1.460 cfs /ft 9.3 cfs
2.5
2
1.5
L
t
M 1
C
0
m
0.5
0
0
UT2 - Stage vs. Shear
25
20
U
N
15
L
N
3 10
0
0
CL
E
M
L 5
41
E
0
0
0.5 1 1.5 2
Stage (feet)
2.5 3 3.5
UT2 - Stage vs. Unit Stream Power
0.5 1 1.5 2 2.5 3 3.5
Stage (feet)
UT2 Supply
UT2 Design
UT2 Supply
UT2 Design
UT3 TYPICAL SECTION DESIGN
RIFFLE SECTION
Regional Curve Estimate UT3
Right Bank Slope, x:1
2
DA (sq. mi.)
0.027515
Left Bank Slope, x:1
2
NC Mountains (area)
1.877441
Max Depth (ft)
0.5
NC Mountains (discharge)
6.559159
Bottom Width (ft)
3
Area
2.0
NC rural Piedmont (area)
1.861803
Bankfull Width (ft)
5
NC rural Piedmont (discharge)
6.700075
Bankfull Depth (ft)
0.40
W/D ratio
12.50
USGS 2 year discharge
Ave Width (ft) =
NC Hydro Area 1
7
SW Appalachian (area)
2.616728
Discharge Calculation overall
reach
SW Appalachian (discharge)
10.13584
Q = 1.49/n R2i3 s1i2 A
WP (ft)
5.24
R (ft)
0.38
design slope
0.0254
FROM CAD, design slope =
0.02538
Channel n
0.045
Q (cfs)
6
Q (power)
9
yRs =
grain diam, Shields =
POOL SECTION
Right Bank Slope, x:1
Left Bank Slope, x:1
Max Depth (ft)
Bottom Width (ft)
Area
Bankfull Width (ft)
pt bar tob o/s
outside bank tob o/s
0.605 psf
100 mm (CO data)
2 width ratio =
1 depth ratio =
3
5.5
8
4.5
3.5
UT3 bar sample 1
d84 = 14 mm
dloo = 65 mm
1.60
2.50
Andrews (1984) and Andrews and Nankervis (1995)
ti,i* = 0.0834(di/d'50) -0.872
ti,i* = 0.0384(di/d'50) -0.887
di = d50 of riffle pavement (from zigzag), mm
d'5o = d5o of sub - pavement (bar sample), mm
d = 1ciTPsand- Ph20) /Ph2O)*Dj) /s
applies if di /d'50 ranges from 3 to 7
if di /d'50 is 1.3 to 3.0
d = mean bankfull depth of water (ft) needed to move largest particle
Psand = 2.65 g /cc specific gravity of sand
Ph20 = 1.00 g /cc specific gravity of water
Di = largest particle found in bar or subpavement sample (ft)
S = average (bankfull) water surface slope
For UT3 sample location
di 14 mm
d'50 6 mm
di /d'50 2.333333
tici* = 0.018111
Di 52 mm = 0.170604 ft
s 0.023292 ft/ft
d = 0.22 ft
from stage report in RM w/ dbkf = d, qci
Bathurst et al (1987)
gcD50 = (0•15905D501 .5)/(S1.12) Din ft
qci — gcD50( D i /D 50) b
b = 1.5(D84/D16) -1
UT3 Reference Riffle
D50 =
0.014 m 0.04592 ft
D84 =
0.052 m 0.17056 ft
D16 =
0.002 m 0.00656 ft
S =
0.023292
gcD50 =
0.564614 cfs
b =
0.057692
qci =
0.609017 cfs /ft
channel width (assumed bottom width) _
qci = 2.7 cfs
1.11 cfs
Existing REW above culvert
4.4 ft
0.023292
Check discharge for initiation of Phase 2 transport using Bathurst (2007) equations:
qc2 = 0.0513 g0 5 D501.5 S -1.2 units of cros; D (m) of the surface material from pebble count
qo2 = 0.0133 g0.5 D841.5 S -1.23 g = 9.81 m /s`
From UT3 reference reach:
D50 = 0.014 m
D84 = 0.052 m
S = 0.0233
Bottom Width (active channel) = 4.4 ft
qc2, D50 = 0.024 m " /s /m 0.007 cros /ft = 0.261 cfs /ft 1.1 cfs
qc2, D84 = 0.050 m' /s /m 0.015 cros /ft = 0.542 cfs /ft 2.4 cfs
1.8
1.6
1.4
N 1.2
a
m 1
w
t
0.8
M
C 0.6
0
m
0.4
0.2
0
0
UT3 - Stage vs. Shear
14
12
10
U
v
8
w 6
3
0
M.
E 4
M
w
L
Y
_ 2
C
0
0
0.5 1 1.5 2 2.5
Stage (feet)
3
3.5
UT3 - Stage vs. Unit Stream Power
0.5 1 1.5 2 2.5 3 3.5
Stage (feet)
UT3 Supply
UT3 Design
UT3 Supply
UT3 Design
Hand Auger Boring Summary
Hogan Creek Restoration
4/20/2011
HA -1 right floodplain Hogan Reach 2
0 -0.3' Topsoil
0.3' - 4.0' Tan silty sand, moist to wet
4.0' - 4.7' Gray silty sand, gw at 4.05'
4.7' Refusal on gravel
N: 940065.91
E: 1528232.14
Z: 984.68
HA -2 right floodplain Hogan Reach 2
0 -0.4' Topsoil
0.4'- 2.0' Tan and gray clayey sand, moist
2.0' - 3.9' Mottled gray and tan sandy clay, wood debris and gw at 2.5'
3.9' Refusal on gravel
N:
940071.48
E:
1528334.01
Z:
983.68
HA -3 right floodplain Hogan Reach 2
0 -0.3' Topsoil
0.4'- 2.2' Red -brown silty sand, moist
2.2'- 3.0' Red -brown and gray silt sandy, moist
3.0'- 3.7' Red -brown and gray coarse sand and gravel, wet
3.7' Refusal on gravel
N:
940050.98
E:
1528450.15
Z:
983.87
SNOiSin3�J
s� °o�may """
;.•,q9N�
�2'.
W Oa bua aauan �u��
OE55'SSZ'SZB:auoy�
}�
(�
_ O
'ddV
31V0
NOLdIaDS30
,' :y
? �� =� '��
Z c =
1099Z PUIIOJPD 3JON'allinasy
laanS PpOi8 91
"9NIN33NIDN3
�N 'AINf-IOJ AuunS
o
d
w
p
Z F-
H X
O
s�� °..•
Dd
3DN3m-1N0�
NO I1VIHN XX NVOH
w
Z �
w p Z
w
U)
2
i
i
1
�
a
4
K
m
O
w w g\ w
Y CL
Z F ll
\
C7
m � Q
H � W
Z Z
Q Q Z
O LL N =
W Z CL V
a
,
APPENDIX D
PRELIMINARY PLANS
�]
z°
a
w
z
Q
iti w
d
z
Qi d W .2
/ w
(SI y LL Z o .
L Z v
�j z- O z F
Z U w c
ci
a
U � w
�o
000 00
D
�w
z
J V W N
U o
O ° 0
80L i,6 'OAT JJ9TOWJ d99
SNOISIAI�l
s � o�nva
,'
I �" �2',
wOa 6uaaauanyuOa
OE55'SSZ'8Z8 :auoy�
1088Z PuIIOJPD LIVON "alllnaysy
[�
Z
O
'dCjv
]iV(l
NOI1 1213SIG
Z
=
j
lawns PPO'B 9I
Dd "9NI?J33NI9N3
JN'AINf1OJ Auurls
NOIIVDIJ IN >I-4ND NVDOH
0
iii
w
� O
w
m
3
3DN3ni:INOD
o
0
I �
o
i
►
�
In
O
0
�
w
w
O
J
w >
EL
z
>
w
w O
cn �
w Ch
z
cn w
Ch
z z o z w
z w
U
>
Q
M
> >
Q m
> >
o EL
>
�n
o
°
�
(n O (n
Q
X
w d S O
w
O w w
O z
Q
cn - w cL o U o
O
- c
O z
W
W
I
no
o
z
N
In
X
w w
w
w w
O O w
X
X w
z z w
O ~
U � C�
w U w
Ch w w w O w
O O U U w
Cif Q Q w > � >
d X m
Ea
E
?
- 3 E
3 -
E
°E -
_03
_ _
m - E - E y
-
49
_
m E
22
E' E.°
E �E c_ n E
m E
- - -
-
E c o
a r A R o 3 _°
-_
- N_ 3 a
- =� E° m E
-
a°
E_- E 3
m
3 _
u _ ° 3
E E
-- -
t�E r E m 3 v- y ffi A p
- -
m
E n n
OO +�Z 01 00 +0� 'd1S x
sNOlslnI� s� ��o�wa4 u
woa 6uaaauanyuoa o
'dCjv ]iV(l NOI1 1213SIG
N II 1=1 O
? � _ —j `.� : 1088Z PulIaPD LIVON "all!naysy _ p
Z a = lawns PPo,B 9I ~ J
`-6 JN 'A INf IOJ Auuns z
j Jd "9NR133NI9N3 o
NOIIVDIIIIN X -4-4ND NFL DOH w
3DN3ni:INOD
w w U' Z ui
V OZIV� N,: o N G
o
oo� S � +
f N
1 Ld
� o
� o
O cV
O
N 1 �
� co
1
,.
w o
> 1 o
+
0 '
LLI
LL }
I �t
+
o
1 °
f +
LU
LU
a
zL °
� w o
U Uz
c� z U 1 1 (D U
LL
Z
J
Q 1 Z
S Z (D u°�
O W v
1 W ❑
1} o
� 1
CD
p +
' I 1
1 � 'm
o
1 Iw
1 1 uwi °
w 1 1 LLJ < o
w 1
w
w
LL
0
Q =w 1 Y
° w
+
U
� Z
i
0 o rn rn rn rn s =
sNOisinI�l
70T N0
;
�Z}
l "VI
wOD bUDaDuanyuOD
OESS'SSZ'sZs :auoycj
I 099 PuIIOJPD 41JON'DIIIAa14sy
]aaA$ PPOIs 9 f
Dd IDNIN33NIDN3
3DN3ni -IN0-)
V
O
oo +z� of oo +�z dls
r�
rz w
N
JN 'A INf IOJ Auuns
o
i
O
NOIIVDIIIIN X - -uD NFL DOH
W
W
w
w
OZ¢
oN
x�
p
CD
I
m
LO
M
N
/
/
p
O
L
M
l
\
\
M
O
M
CD+
O
O
M
O
N
O
N
O
O
O
N
O
W
LL—
I
/
N
O
I
/
�
(D
�
N
\
W
J
O
\
=
+
\
\
IO
N
/
W
UJ
o0
J
O
a
O
I
I
ry
a
N
p
+'
I
LU
Q Z
N
Z K
+
N
7 W `
Oz \
CC W `
p
`n
(D U
Z /
Z Ur <
z
N
U1
W
w )
w
c
7
po
+
N
O
�
V
N
_
/
\
O
O
+
V
N
O
T
+
N
O
N
1
m
O
�
�
1
m
N
N
V
r
LU
J_
OO LL
+ p
N
d
O Y
W
W
N
U
o Z
o �
N
i
\
l
\
I
LU
J_
OO LL
+ p
N
d
O Y
W
W
N
U
o Z
o �
N
SNOISIOI�l
70T N0
s o� nva 4
'
, *�'",,�� �;
cNyS�L
wOa bUDaDuanyuOD
OE55'SSZ'8Z8 :auoy�
1099Z PulIaPD 41JON "alllnaysy
433nS PPOIB 9 f
O n
Dd "9NIN33NI'DN3
3DN3ni -IN0-)
av�
JN 'A INf1OJ Auuns
L6 +K 01 OO +Z�: d1S
M
O n
L�
rz w
N
co o
JN 'A INf1OJ Auuns
o
+
m
m
O
W
NOIIVDIIIIN X - -uD NFL DOH
W
w
w
oN
Oa
x�
O
o
0 o o
M
O n
0 0 m
a,
co o
+
m
m
> O
m
i
O
O+
_ oc)
� m
O
O
O
m
w
Q
O
F
+
CJ
W
ao0
p
�
+
a
I
rCDi
0
ii
m
LLJ
o
°+
a z
�
ZLLJ
m
Q H
o
W
(7 z
Cl)
Z (
Lu
W+
p
m
O
m
m
O
O
M
CD
N
m
O
O
�
N
m
O
V
W
J_
LL
O
w
d
Y
W
W
w
U
z
Q
O
O
2
SNOISIOI�J s 1p\,Ava� 09+01 01 OO +O L d1S
n;,lY wOa 6uaaauanyuOD o
'dd'd ]iV(l NOI1d1213SIG
�= 'T `.� : 1088Z PUIIOJPD LIVON "alllnaysy = p
Z a = halls PPOJB 9 f ~ W
` ' JN'AINf1oJ �uuns
j Dd "9NIN33NIDN3 0 O
NOIIVDI,LIIN )I"-4 --4ND NVDOH W
3DN3ni:IN0�
m w a ui
o
o �
1 wz 1 w
az
Z) � w
W w LL
O U = d
1 1 z cD ~
1 N LI
LU
1 1 w a
1
1 a
K
a
1 1
1
1
1
1 1
1
1
1 1
1
1 1
1 �
1 1
D
1 �
1
1
a �
I /
/ co /
SNOISIAIO s 0 �wa4�� Z 55 +9 � 01 00 +0 � +1S
n;,lY WOa 6uaaauanUUOD o
dd'd 31'dQ NOIldl2lo53a r �-j2"I� "may OESS'SSZ'8Z8
`.� : 1088Z PUIIOJPD LIVON'alllnaysy =
Z a = lawns PPO'B 9 f ~ _j W O
j Dd "9NI?J33NI9N3
0 O
NolsVDl�ra x��uD NVDox
w
3 3DN3ni:IN0� Q w
ui
o 0
a
°
0 o rn rn co m o
0
0
+
°
w N
W
O
a o
O °
+
a
0
0
0
F W
a z _
] J +
Z W O
oe Z 1
(7 U o
C7 0
z z o
H �
�W
LU o
�' rn
� o
0
� I
0
TO
o
0
co
o
o
0
O
+
0 o rn rn ro m �°
0 o rn rn rn rn
O
V
W
J_
LL
0
rr
a
N
H
M
- � O
O
(D M
M
F W
a z _
] J +
Z W O
oe Z 1
(7 U o
C7 0
z z o
H �
�W
LU o
�' rn
� o
0
� I
0
TO
o
0
co
o
o
0
O
+
0 o rn rn ro m �°
0 o rn rn rn rn
O
V
W
J_
LL
0
rr
a
N
H
o
0
co
o
o
0
O
+
0 o rn rn ro m �°
0 o rn rn rn rn
O
V
W
J_
LL
0
rr
a
N
H
SNOISIOI�J
s 1p\,Ava��''�".,
Sg �S +Z� 01 0t+6 b1S
JN'AINf1oJ �uuns
NOIIVDII,IIN X - -ND NVDOH
n;,lY
�= 'T `.� :
Z a =
` '
j
N,
:
WOa 6uaaauanyuOD
OE55'SSZ'8Z8 :auoyd
1088Z PuIIOJPD LIVON "alllnaysV
halls PPOJB 9 f
Dd "9NIN33NIDN3
~
0
w
o
o
=
w
0
W
O
m
F�
a
w
z
'dd'd
]iV(l
NOI1d1213SIG
3DN3f11�N0D
a
--
%�
r
-
W
z
O
�
❑ Ij
x
Irk
33x00
r
U �
LL
in o in
o
Y O
z
rn rn
rn i°n
W
+
� U
z
0
d
�
❑ O
1
o
I +
W
p
m z
LL
IL
1
w
¢
I
°
_J
o
1❑
1Z
I
O
3
I
/
a O
LU
z
❑ o
W
w '
a
--
z
ce 0
Ow
o o
a
cD z
Z (7
0
rn
y
I
X 0
W
1
11
1
1
O u
O O W
O O O
O
O
O+
CO O
O
i
1
I
�
I
1
0
V
�
I
w
J_
LL
O
fr
a
SNOISIOI�l s 1 �o�nva Z
` -,1131,111", wOa 6uaaauanyuOa CD
'dCjv ]iV(l NOIld121353a ,�n l`�j�" �2', OE55'SSZ'8Z8 :au-yd o ii 'z w
�= 'T 1088Z PuIIOJPD LIVON "alllna4SV cv _ V4 O
P.
Z a = halls PPOJB 9 f ~ Q `'
JN'AINf1OJ Auuns 0 z
j Jd "9NI?J33NIDN3 NOILFTDIIIIN )I$--42ID NVDOH
W w
3DN3ni:IN0D w :
> z
a o
o �
Z U
K
m �
F Z
z U
W U
W K % W ui
QU <ZCC
Z w W U
Z ¢� awa
M 0
n
w O'n Hwy
I
I
l
I
Y
O
m
� � I
,09) YJ
O
Y
2
�j
i
i
� O �
I �
N
I
I
0 \
I
SNOisinI�l s. . o.wa ..... z
wOa 6uaaauanUUOa C 31 N
d'd 'dQ NOIldl2��53a �'�`� OESS'SSZ'8Z8
d :auoy� o H
n �2
'T,J�w `.� 1088Z PUiIOJPD LIVON'allinaysV w 11 O
Z j lawns PPOJ 9 f JN CLNfIOJ i22IS
0 Dd 9NR33NI9N3 m w NOI VDII IN >I"-4 --ND NVDOH co
3 3DN3ni:INOD w i
C
M,os)
5'
0
N
0
SNOISIOI�l s �,,'vnva Z
0, Woa 6uaaauanyuoa d N
'ddH ]iV(l NOI1 1213SIG ,��j
a
OESS'SSZ'8Z8 � 4J o �
1099Z PuiIaPD LIVON "allinaysy ° O
jawls PPo,B 9 f ~ a
Z 2, �d "9NR133NI9N3 JN 'AINfIOD ANNf1S o Z o
� � o 3�N3f11� Lu
9 N0� NOIIVDIIIIN x -4-4uD NVDOH W
Lu
Lj SS3 ,,: 6i a Q a
HN '' o N
I — —
\
zI LU v
0 U Lu
K
m a I
LU O _] —
aI z
Z —
isss�:�daneg0
p�
QbQN dve M,�I301M
LU
/ \\
/ Z
N
O \
•N \
U
z
cq
\ Z N O O \ j
ID
I I
E a a
S.2 @ @ \\
m F I N N
~ l @ O
— L ~ Q d
s= N O O — —
U 75
� a o
U ° o
m
o x a
o @
.o o O o L S 15
u�aa -o ama ° -o a-i -gym
>N amv co d t -c % ua
a UJ N N ' v
cn U o m E a n o @ o a @ c@
3 a LL LL
H c L c n 3 m m 3 n c c o >+ O @ -mac LL
y o @ o @ N aai m
n s o 3 p_ N a L in co a W
E v� o L Uo ID
�momo ENO= =d�aco °O& m @ o �Y o cfla
O .N U Q o N fl�. p m m LL O N L2 m N c`7 L W
U Q m s .N o L U L a y N O Z LL, Z
a ._ - ,p 6 3 a o- c O cO N @ N N Q W
W = o° t °' "n �i m E m m c o °J a`� � 4Ni m N c 0_ 0 W oz O Z D_ Q
a ' O'3'o'm6'i4o�i�`°` =o°.3ao° -'`-6 �= o �o > a 0� On 0J WJ
m m a s o a n N o m a m .o n N tl .� It Z U) Z d Z a % 0 cn i s i 'y o o ._ E o o m a a c (n a N � F F o W m w °-m =t omomaao > Y 3 w Z� ZO ZO QZ
m3 Q QO QO
C C. . . N O j Y_ N. t6Q @ a> O.32s_ o. @U @ F 0_ 0_ LL d LL Z U
SNOISIOI�l `o�nva r
wor6ua- Duanguoa U
ddd 31d0 NOI1d12IOS30 = ' =,2 OESS'SSZ'SZS'auoy� N Z w
_ I099Z eui�OIPD 44loN'a��inaysb "� O
jp(1ZZZ _ 7aai1S Pegg 91 U F N
J1j/y+ �N 'X LNROD 12121I1S 0 z H a
1 a; Dd''�NI?J33NI9N3 a
�j NOIZVJlIly x� D NVDOx
di
0/ W a Q w
lyJ
J
}a F 'n r a U F J _ Y
FQ a (a ❑ Z � ¢ Q � F � Z
H LL❑ F uU ,
J S O O O O N m c c
2 2 O O N `@
U � lU m N Qa Q 1 T Q ° @ 3 @ °�2 O O 2 O N m m �
+
.
2 O O N m @
O 2 2 O N m 6 G
o
m N 7 I4 L F 2 � O
W N
W Z o0 o0 o m p m p
W — — — — — — — —
Z Q W N N N N N
O N >- 00 O elf
V Z Q Ii QQO Q O O � Q Q w W Q O w
LL LL w LL W Ii w W m W
IL 0 O O O O
o 0 0 U) U)
co U U U U U U U U U U
'D 2 W Q @ n
LL
LL E EL
E
° 4 c O
co wco d W (n U O
0 E i
SNOISIOI�l
wor6ua-aauanguoa U
ddd 31d0 NOI1d12IOS30 = ' =,2 OESS'SSZ'SZS 'auoy� N Z W
_ I 099 euiIOIPD 44loN'ailinaysb "� O
jp(1ZZZ _ laails Pea9 91
�N 'X LNROD 12121I1S 0 z H a
Dd''�NI?J33NI9N3 a
-,���iss� 3�N3f11�N0� NOIZVJlIly� xa D NVDOx w a Q w
W J P-i IyJ
H />0�� Qp
W
❑
J �
J W
J
U) m `)
FO U-
_`
F
0 O w �>
O0 Q wm x
¢
z
v z a OQ J
�? Z �0-m LU
a
LL z
J w F z
Q y% Z
of LU
F Z z
wx J❑a FO LU
0 00, x w zJ
ixJ z�z U OU
F g m Q lo Q Z—
Z Q U) � 0� i m
Q❑a QUw U
UQQ U�wO 0- U`
zol
< Q O W J
F lo n LL
��� Y
F W U
z
LU of
of
Q
W r C7 Q
F tr ❑ a
cn w w �
a
i C7
Z z
z w ~
J z
z U Q Y a
Z J 0 U
0m W
a z
U) <
z Z
LU ❑ — -
< z z UO z
(D J� z W
�
\ V y� J W
U r d h-f ❑ N d
z_ W z a
Z
w n
0
z 1 Z U`
O
U W W
zQ ❑ C7 w m ❑
\ K Q ZQ z Q K
Q c�
W x w w U 0 z w
i� > U�w J= Lu
tY ❑
0 of
Z m O W w ❑
F =LU 0> _
C7 Z FQ ZO W m K U
Z O J x Q L z
a ❑
F
❑ z � H
LL
w w O Q
a m
F w
z❑
F w F J O =
00 z m = g Y L
z F QU ❑ J� w w
Q z
w U W F U = O LLWO LU
� 1 z� 0 Ox
F W
=-2 0 0 O W =z aF W
Q Q Z) O W — Q§❑ U O w w> W F
x
O z 2 LL w U J F O O ne ❑ w¢ 0 O
LLI w OQ Q O❑ U 0 Z O LU
00 Q O F w m m oe > U N W Q Q 0 Q w F W H Z z O i aQ 0 W W F LQ ❑= Q H O Q LLJ
O F F W J
o
w KQ ❑Q Q U i 1-cLI:0 — LL w F z
XU <LLJ W �i W O x rJQOFU W
W U W % W W Q > o o o<,< o m w o O z
z Qm LU
=~ OO wz Q ¢ U J 0 a z ¢
zLLY YF LL w w
Q UQ z U �ae -
o_
z
� w � 0 U cli ai v ui
SNOISIOI�l `o�nva o
wor6ua DuanguoD
cq
dd'd 31'd0 NOIid12IOS30 = ' = -2 OESS'SSZ'SZS'auoyd N u W
I099Z P- IIOIPD 411- N'ailin34ib O
IDDAS Peoae 91 U
�N 'AiNnoD �uuns
�. Dd'E)NI?J33NI9N3 O P- F" �
a= NOI VDIIIW >IIRND NVOOH � J
3DN3niJNOD w H w
M
b
Z
V LU Q z ° LU
W W > °
OUJ
m
U- w OJ U
U z
0 ¢
p
0 W
— J ❑
°
tY(7 Jaw
a ui
H p=zQ0
JJJI ° — J
w a
o a° Of 0 0
W Z r z a = uj 0-
° O 2 n- [--
z FA o U 0x =¢CDaz
FO J Y (D°Z) 2W
F V J �Y p W 7Lu0° 0-
n o O 0 W Ox Z W
w a a wGmao
O U z U m J
J 0 Q Z J J W W
oe Q Z p U Q J° Z U) W
O N�' d C7 xo<n >-=
WoaO
00 H 2 wLU=a0
U d = U of
Y U J < W
Q p W m
° N H ~ w O
IL
W O co
° J Z~ 7 p W
I� W W J LLLL,D_
Z z Z 0,= 0
0W0~�
QV 0Y00U
g
a Y co Y W
J W Z N Z W of
J Q = Q W
LL o m0�-
Y Z N U ri
U
m
O
Z
H
X
W
O D_
z< Z N p N
N U U o W Q
W W o (n Of LU
LU
° W Q v LJi W
-i Y N W W
EE
N c. ~ EE x z U i
i U � U Q
i a U Q w a a
EL O 0 a� H 0
O O n
o z
C— °
U 00 M Z z O
a_
I �
J w a
I
I
SNOISIOI�l `o�nva o
wor6ua DuanguoD
ddd 31d0 NOIid1213S3a = ' = -2 OESS'SSZ'SZS'au0yd N u LL
Pow 1099Z euiloIeD 411-N 'ailin34ib � � � � O
]aa$$ Peoae 91
DN 'AiNnoD �uuns
�. Dd'E)NI?J33NI9N3 ° P- F" �
a= NOI VDIIIW >IIRND NOOH J
3DN3niJNOD w -i H w
F�
o II
� I
i
I I
c� - Z
z
o H
N r wQ ZLU LU
o w 2 o w
o m > K U U
Z J
N O m L ¢ LL
Z Z LLwx� LLJ
0_ �OZZ
U U �0�=¢
W W 0g��Lw
�L UJ ❑J (n �� <Zo
(-4j - _ J Z / J KU` �Q W
O OZ c9 O ¢oxxU
of zy O ��UOLu
a a Q U a U x Z Q 0 IL
Q Q W D 1 Q w a 0 U)
a N LL °< a M xow °o
U, } H U O H a Q 0 LL
LL H w J
° � x
Z ¢ ° z LL, Z Z0w�U
x w j N O N Lu Q U` Q❑
wo M (n U Ln (n UOZ) gw
U U K Z LU
CCUwm¢a
O w
J
m 2 J w Lu Lu
b z w
0 ¢a =nw
ro 1 U =LL1 (/) Z:
co 0 w (D
wwaZ)
U � _ ¢ O
x U K
J ¢
oM O wo�¢o
F- K LL Lu H
U w °z
Z LL 0
W J w
LL OU LL
U' - (n z OLL =O
J OwOFU
O U LL } LL W
a } H ° <N OO� Q
L l Y w Q= Q o W
QL YK
Z U r
N I
I I
o I
Z o Z
o O O
I � �
U U
w w
U
W U - w
c� - � LL
LL. L<_
/� -- c ii cr
U ~_ U
} H N } H
cD
F N N -Z J
Xw N Ul OZ C9a i v
w¢ ~ o= �� Dr)
� o Lu
¢ Z o a
OD
o °x w z 0
LL LL a
Z Y (D In O
D
°U < OLL W W LL
Z
O
U
SNOISIOI�l
woDtua DuanguoD Fi
dp"; o H N
'ddd 31d0 NOI1dl2losl0 = ' =,2 OESS'SSZ'SZS'au0yd N Z �n w
I099Z euiIOIPD 411- N'ailina4sy O
7aai1S Pea9 91
Od'Nld33NI9N3 DN '11LN110D k?I?II15
O O o
,= NOI VDIIIW >IIRND NF�OOH �, w
�iss�„ 3DN3niJNOD w Q
W rr�' w
J
Q
LLJ � U
O Z
J L O
J ~
O a Ow
w F7
n 0
~ Q O Z w
Z) � LL
O
X
70
U)
z 2 O U
O 00 Z
z J U)a
a U
0 ¢ O
LL
> 0
J %
N OO 100 � 0/
W J
P p0 \NT gPR LL
LL H h
Z
Z
QJ �- M �o
4/ R � )
U
�0 �0 Q411
�O O �v
a
Q-
�O /lo.sl&
w
0 Lu
LL
J ¢
0 ¢
w� Z
7
Z
o O
Z w
LL a U
w
Ul
w
C7 U = J
Z 0 w n H m H m
F N w 0 U m0
�O 0 X Q O O U
�W pwp �¢ LL z
00 z O z ¢ W W< J
x �O C� z �> draw
oe
F xw w �a(�
U ° U)
LL xC9 OU Q
J
W J Z
OW Lu O O 00 J
�:w mx Q
LL ° O 2i W 0 J
HL L
OzLU LL J z LL
w U) O p
Ul
}
LLI LU
x a ¢ U` Z+,�
w U
FLOW
x o¢ U
¢ W Z J Y ~>C� Z
ZW K w m warn�� A�
F Z � LU O U O J Q m l J 1 J LL O
¢ a o U z z of TOE OF BANK (TYP) C) Z
o � w(D cn ?Ux
I- 0 0 Z m U Co
z a F O§ z N D
¢ X ~ m H
J
LU 0 �_ z w g TOP OF BANK (TYP)
J
F UJ 0
OUzO
Z ¢ N
SNOISIOI�l `o�nva"
wor6ua-aauanguoa U) w
'ddd 31d0 NOI1dl2losl0 = ' =,2 OESS'SSZ'SZS'auoyd N Z �n W
I099Z euiIOIPD 411- N'ailina4sy O
j�(1ZZZ _ laailS Pea9 91 U F ~ N
J1j/y� a �d''�?J33NI9N3 DN '11LN110D k?I?II15 p
NI ❑
,= NOI VDIIIW >IIRND NVOOH �, w
�iss�„ 3DN3niJNOD w Q
W w
W
❑ J
❑ W m
LU
LU
W F
H m
z �_ ~ zJa
Q
Z ZOp ❑ �f ❑ U x L¢ Z ZQ U
_ U m Z
Q
W O ❑� d!
�dm
fl' O�~ Q�� Z
F O O p o O O Z O LL O U
z
Y cn x�n ? mFZwmo?�OUw ❑ a O
n U z ¢ z ji (D Lu Q a
Z o w w z Q z=> Q U m z
o � �U ~ w ❑ H 00 p o O O >
0 ¢ a fr Z w
Y
¢Z Z m � N m J
U
w
— LU
LU O0 <U� W ❑ m M N x W
F W O O J
LL z Y w
z ❑ Q --- I_ -- z
J
m w o
`L -
o z
U) Y Z \Lu-..U)
U) m W Q � z
° w15
� L ❑ m ❑
U Y Q U) Q N
W
gm � < - w
J
Q LL 00 LL
K❑ z o p U
w a
U
J
w
CL U)
�
IL w ❑
g m Q a � O
° W d. Y EE m p 0 Z
❑ w Um
w U �� a m
m Q J U
W S U M) (D N ❑
LU J Z m O
U Z ❑
F Q 5; � LLJ Z
z w Of O 2
o ❑ W z< w ❑ O m
~O❑ uwi Y ¢ L¢LI
�UZ a z¢ Q x
�a w
d W z
wm Q an W
O
7J) <,J o Q H
< o N O > U pew O ° D_
L �LLI Of a
c� cn
� J Q U o 0 ¢ Z O z ❑ d Z
a- w Q O z z U�
❑ ii 1 J _ Z. H Z_ dO
Q 2
x
+
V J
W W _ W m
= O Q
LL w O Y K m DC-1 U) z m D- OU ❑ m
J LLJ
J
P J LL a
O z
O
"oppFg��� 0 �❑W, L�o
O N Z U W U) :�! _ M O
J
❑ U) Q Q N z N J
LU o z ❑OZF� ow
z 0!
IK u) �F_�_W ZZ��
/ U 0 ❑ U
Z F opm�Oz� Fx
d' =OLLH �zw m�
p� d Z Y Y� D O D_
U << 0-wpwH
W m m O 0 m m m U)
U) N
SNOISIOI� �", a"
woDtua Duanguoa
'ddd 31d0 NOI1dl2losl0 OESS'SSZ'SZS'auo yd o H Fi
N
N Z �n LL
I099Z PuiIOIPD 411- N'ailina4sy U
j�(1ZZZ _ laailS Pea9 91 U F ~
a �d'?J33NI9N3 DN 'XLNf100 12121115 O
ONI °
,= NOI VDIIIW >IIRND NF�OOH �, w
�iss�„ 3DN3niJNOD w Q
W W
J
Q
W
J
m
Q
H
W
d'
H
U
0'
H
Z_
H
Z_
O
TOP OF BANK (TYP) P W z
Z O
� Q
w
TOE OF BANK (TYP) U) J
O W
U m LU
_ Y W
LU N P �N xa Q o
X J J ZZ U m
N d' W Z d 0 (n ��
K
O LU 0 ow 00 Z H
LL - -D O O W O m
LL m Q �•._. LL m
N M O
F
w U U
° m
O LL z
m cc w w
of W H m
W
° J z 0
W LL O U
2
>� Z
J > J
LL LL W
Y >
W O Q D
° W m (D
-,w
Z) Q
Om
m2
H =
K
W
Z
K
W
°
J
W O
m
Z LU
SOP OF >
6 PNK P Y o
Y ¢ O
m
O 4 LL Q
O
_ 2 O O� Q
�O�OF BPN� N 9 W ° p U) LWJi
P V Z
J U
Q z a
O H
00 Z X
O Lu
LL
\ D W W U a M
x-17 (Q7 U5 m
of ae
WLU z 0 z m
H p 0 0 ? w
70 O Q � z o pJ
=O
J > m J
LL > J LL ;
U) Q
ow U QCD
Jm m
0 m
m 2
Y ~
O3:
O
2
SNOISIOI�l
wor6ua DuanguoD
.'`9NI dp o H N
ddd 31dQ NOI1d12loS3a =' = -2 OESS'SSZ'EZS'auoyd N Z Cp
1099Z P- IIOIeD y�oN 'apinaysy W
j ow aaans veoje s 1 DN 'AINROD .,NN IS o Z S
7d'9Nld33NI9N3 Fc
3 �o�ss 'a 3�N3f11�N0� NOILF�JILIL�I xa � N��Ox w Q
j �'�f' W J w
m
CD
Q U
0 Y 0- Z 0
HzQ 7 oa D o
�C0 D (D �a
Ow zLL 0
z0_
00 o n a
�U ¢�
W W J
co 0 Z U
J
00 X Z
O
LU
H U)
U �
D_ /\ a a w > LU
W Q >0
m Q Y Y >
Q Q Q m LL z
Y m m W Z
0 O O
W z � O O v
a � Z �
N
M
U
W N >- W X
O a H D_ J
j0CL w0 Z�
(D 0n
m w z a
0 QD H
w Z
�0
J w N
o} o 0
W W U Z in III Z
Y Z K O W
U 0 m w W
LL 0 0
w � U
z I= H
�0, J7 W J O
(D N W In = _ W
X V
W
U J
v~i L wo v
o L 0
L � IIIIII z
z Z 0 C)� LU
0 U
LLJ O L Z O UaJ_
w02 �O>> > 2 F
W
W Z
U Ymn' W
D J m O W
m U
Ja LL co
J_
Q _ � = O H
W 0 0 Z Cn Z
O H w w w 0
a
O Z J W W W J
Z LL J W o w D_ N Q
} W ~ O L L Z < Z a w W w 0 CO
Q O
Z
> 0 CL a o 0 0
K o go iD (- W H W n-
o
Lu LU L n-
H
Q o oo > 0 N
O
Z_
o �
N CV
I I
W
SNOISIOI�l
wor6ua- Duanguoa
ddd 31dQ NOI1d12loS3a =' = -2 OESS'SSZ'SZS'auoyd N Z Cp
I099Z euiIOIPD 441 -N 'a��ina4sy 0
a
LL
fl ZZ _ laails Pe9 91 U `n Ln
�N '�iNno� �uuns 0 H ❑
Dd'E)NI?J33NI9N3 F�
��iss� ��� 3�N3f11�N0� NoIZVJ1IIV� xaD NVoox w Q
j �'�f' W J w
J
J_ W
LL z
Y Z
Q _ J
M U LL
❑ Y
w U
z ¢
O
❑
Q
m
J z
} �w
¢z
> _ 0
Y O �z U
w z <a Q
U ❑ a > W
w w> Z
w r' Q W O
22 u ¢ z � � cn
z Q U L
}
O 2 Q
LLJ Zi�2 r� Y
LL
U U Z
❑ U W IZ
z z m m U (n
00 H M W H
� u5 z U z
U Z z L4
W W Q w
� �_ 2 �
} ❑ U � In
¢ > ❑
W_ ~ Z W
i W Q z }
) W F
Z a
Q O
J �
O
LL
a
a
a
rr
m
w U)
❑ U)
e (D g
LL
= a — ¢ a ❑ U
z�w a as w LL
"¢U) Of mx O
m Q U w W
o LL co U� LL z0
¢
[if ? g Q p �>
K � ❑ 7 �U
°� hwX
` 2 W
h z
LLJ
0� (o �Q Q ¢ o
LU
OL z w z0
o Ow Q A o
> u H
W a z w ❑ z
¢ w X III UJ
¢a m z N
00 a z ¢� DO
�� ❑ UZ m �_J YQ
w az z-
0QU ' w� a �b mw
z� °m �a
Ow Z wg
H
SNOISIOI�l
woDtua DuanguoD
ddd ]iVG NOI1d12]OS30 OESS'SSZ'SZS'auoyd N Z Z H
I099Z P- IIOIeD 411oN'alllnaysy W w0
J1j/y 7aai1S Peae 91 DN'AINCIOD Q
�uuns
�. Dd'E)Nld33NI9N3 O Z W O p
a= NOI VOI11W >IFIRND
e �L , NVDOH � w F
F- (� w w ss� 3DN3niJN0� ii J
¢ U v W ux
p
w
z
00 LU
Q Q)¢ v U p
p O w
0 d 10 � V J
C) c°x N m¢
1 in
W
Y N
Q
O
U) O
0 W o M
> X O
M —
J cL �
L< Z
W
III - co Q' Z N
LU
Z } o I O r CL o Q
¢ 0 J -III= O m o
W l W X W III W W J Q= p c
Z x- H U o 0
¢ z� a O LL d ce m
D_ wLL m I- z U) OY
z ccLU° II IF O O °� wo m
W O O H (V III —III ~ J J
¢ ¢ J w 111 =1111 W 0 10 0- o m
a
O z oW- p w�
w p 01 U Q
IL aO ¢ ¢
> v tY i z = H O O
m Z m III 2 uJ Q pa
¢ ¢
I - N 0¢oY� O ° @
w -III p���m z ¢
0 � X 0..z Y
O1 xOZCn0 Q
z III II ~ W 0 H
cli z 1 - Y O¢Xa00 W
= I1 ¢ F ¢ g to j > U)
H
0WC7 CY J Z
O Yzcc
> aZ
��v�OW
x W W 0 Cfl
0 C> O J N p
LU D— W
I-
0
Z N
CL
J
W
U �
L 0 p
0 W W W
U)<n �m U)
Y W Ox W
CL
m0 z z� ui O ¢
c�
L Z C) w U� H 0
U� z� �O m
x p a s Q O w Z x H
J� L u Uo a J Q
LL w H O Z � O
°� �� p: O �x H W Q LU
az ov
ILL Lo U
o Z o
(D 0 zp No // �¢ O W
Fw /// wz Z
�> /i\ j mo O cn m
J Z � H n
W 2U' 2x W Z W o
>O0z �� ¢
/V A p
Q �� j /�� \ /�� j�\ F W CD W ID
W ��� �� %A�� U W z_ ¢ W D_
Lu! 2 O K Z < O
¢ a z
U)
xcex
OwLL
Opw
2
U) J
Q
m
U M M
a�
a
a� �
E c �
.F �, C @ y O O Oc
C > N LS1 d
U � � � tA N (6 3
N n 'c >
a �
D_ w a U m> U
m
E
Z
a
�
�
c
O
K
N
�
O�
C
U
U
N
U
c
~
aci
in
Q
_�
L
C
x
~
cn
>
N
p
O
C�
rn
°
�
�