HomeMy WebLinkAbout20220204 Ver 1_4520018 EWP Duplin County Permitting REPORT_20220131_;� � . Ate• • v �.-. - ,
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Prepared by:
(� LDS1
Jonathan Hinkle, PE
LDSI, Inc. I Kinston, NC
1308 H WY 258 N
Kinston NC 28504
Phone: 910-663-4123
jhinkle@ldsi-inc.com
Prepared for:
DUPLIN COUNTY
dupllncauntync-cam
Angie B. Quinn, Soil Conservation
Director
❑uplin Soil & Water Conservation
165 Agriculture Drive, Suite B.
Kenansville, NC 28349
angie.quinn@duplincountync.com
BACKGROUND
LDSI was contracted by Duplin County to assist with 3 sites that were affected by Hurricane Florence. LDSI
has previously assisted the County with the initial Damage Survey Reports (DSRs) which portions of this
submittal utilizes information gleaned during that project. LDSI has conducted topographic surveys and field
reconnaissance work to collect data that will be necessary to complete these projects. The sites are located
throughout Duplin County, NC. Two project sites include Channel Bank Stabilization and Sediment
Removal, while the third project site is just a Bank Stabilization. The purpose of this project is to restore the
drainage infrastructure to a condition which existed prior to the hurricane.
EXISTING CONDITIONS
Figure 1: National Wetlands Inventory Wetlands map of project area
Duplin County lies within the coastal plain of North Carolina and its landscape is characterized by agriculture,
pineland, forested wetlands, and residential areas. Numerous streams and freshwater wetlands drain to the
Northeast Cape Fear River, which runs through the county in a corridor of forested wetlands. The soils
present within the project sites are primarily sandy, well -drained soils that are typical of North Carolina's
Coastal Region. The damage done to the three sites within the project was caused by approximately 29.5
inches of rainfall that occurred during Hurricane Florence. This resulted in debris and sediment build up,
stream bank erosion, and significant scour. The existing conditions of the specific project sites are listed
below.
(OLDS1 DUPLI
N COUNTY
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039 — Tandam Branch
Project site 039 is located on prior converted farmland and contains a section of Tandam Branch that
passes through a box culvert beneath NC Highway 111. This channel has experienced increased erosion
and related damages as a result of Hurricane Florence. Bank failures and excessive sediment deposition
along the channel bed have de -stabilized the stream and bank blowouts near the culvert pose risk to the
existing roadway. Consequently, Tandam Branch is in need of rehabilitation.
040 — Dark Branch
Project site 040 is located on prior converted farmland and includes an approximately 1,000 LF section of
Dark Branch, starting at the outlet of two culverts passing under Dark Branch Road. This channel has
experienced severe erosion and scour as a result of Hurricane Florence. The slope of the stream bed
varies significantly throughout the reach and has become unstable. The left bank was blown out at the
upstream end of the reach by Dark Branch Road and poses a threat to the roadway if left unaddressed.
043 — Sarecta Road
The roadside bank located within project site 043 has experienced severe erosion from Hurricane
Florence. Failures can be seen along the side of Sarecta Road and the eroding slope will impact the
existing roadway and utilities if not addressed. No waters of the State were seen in this project area.
Soils Data
Descriptions of the unique soils found within the project areas are listed below. These represent the soils
most likely to be encountered during these projects.
BbA—Bibb sandy loam, 0 to 1 percent slopes, frequently flooded
Setting
• Landform: Flood plains
• Landform position (two-
dimensional): Toeslope
• Down -slope shape: Concave
• Across -slope shape: Linear
• Parent material: Sandy and loamy alluvium
GtA—Grifton fine sandy loam, 0 to 2 percent slopes
Setting
• Landform: Depressions
• Down -slope shape: Concave
• Across -slope shape: Linear
• Parent material: Loamy fluviomarine deposits
over marly sandy and clayey alluvium
4
(OLDSI DUP� COUNTY
Typical profile
A - 0 to 6 inches: loamy sand
Cg1 - 6 to 60 inches: sandy loam
Cg2 - 60 to 80 inches: loamy sand
Typical profile
• A - 0 to 8 inches: fine sandy loam
• Eg - 8 to 11 inches: sandy loam
• Btg - 11 to 50 inches: sandy clay loam
• Cg - 50 to 60 inches: loamy sand
• 2Cg - 60 to 80 inches: loamy sand
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JoA—Johns fine sandy loam, 0 to 2 percent slopes
Setting
• Landform: Stream terraces
• Landform position (three-dimensional): Tread
• Down -slope shape: Convex
• Across -slope shape: Convex
• Parent material: Loamy alluvium over sandy alluvium
LsB—Lucy loamy sand, 0 to 6 percent slopes
Typical profile
• Ap - 0 to 7 inches: fine sandy loam
• E - 7 to 11 inches: fine sandy loam
• Bt - 11 to 37 inches: sandy clay
loam
• 2Cg - 37 to 80 inches: sand
Setting Typical profile
• Landform: Broad interstream divides on marine 0 Ap - 0 to 8 inches: loamy sand
terraces, ridges on marine terraces 0 E - 8 to 24 inches: loamy sand
• Landform position (two-dimensional): Summit, 0 Bt1 - 24 to 35 inches: sandy loam
shoulder 0 Bt2 - 35 to 80 inches: sandy clay
• Landform position (three-dimensional): Crest loam
• Down -slope shape: Convex
• Across -slope shape: Convex
• Parent material: Loamy marine deposits
McC—Marvyn and Gritney soils, 6 to 15 percent slopes
Setting
Typical profile
•
Landform: Ridges on marine terraces
0 Ap - 0 to 4 inches: loamy fine sand
•
Landform position (two-dimensional): Shoulder,
0 E - 4 to 12 inches: loamy fine sand
backslope
0 Bt - 12 to 45 inches: sandy clay
•
Down -slope shape: Convex
loam
•
Across -slope shape: Convex
0 Cg - 45 to 80 inches: sandy clay
•
Parent material: Loamy and clayey marine deposits
loam
NbB—Noboco
loamy fine sand, 2 to 6 percent slopes
Setting
Typical profile
•
Landform: Broad interstream divides on marine
• Ap - 0 to 10 inches: loamy sand
terraces, ridges on marine terraces
• E - 10 to 13 inches: loamy sand
•
Landform position (two-dimensional): Summit, shoulder • Bt - 13 to 80 inches: sandy clay
•
Landform position (three-dimensional): Crest
loam
•
Down -slope shape: Convex
•
Across -slope shape: Convex
•
Parent material: Loamy marine deposits
OLDSI DUPLIN COUNTY
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PROJECT GOALS
The purpose of this project is to provide technical and administrative services to restore the three project
sites to pre -hurricane conditions while complying with the requirements of the USDA-NRCS Emergency
Watershed Protection program. This will be achieved by the following project objectives:
• Removal of sediment deposits within stream reaches
• Channel bank stabilization via grading and planting
• Installation of in -stream structures to maintain grade over time
• Backfilling large scour holes throughout the project sites
(OLDS1 DUPLI
N COUNTY
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039 — Tandam Branch
039.A Hydrology
Watershed characteristics for Tandam Branch were determined primarily through the USGS StreamStats
tool along with field reconnaissance. It was found that the watershed draining into the stream is
approximately 1.77 sq miles (1133 Acres) in size and has a 50-year peak flow of approximately 435 CFS
(Figure 2). The project site is at minimal flood risk in Flood Zone X.
0 2500 5000
Feet
PEAK FLOW STATISTICS
STATISTIC
VALUE
UNIT
2-YEAR PEAK FLOOD
87.3
CFS
5-YEAR PEAK FLOOD
176
CFS
10-YEAR PEAK FLOOD
247
CFS
25-YEAR PEAK FLOOD
347
CFS
50-YEAR PEAK FLOOD
435
CFS
Figure 2: StreamStats Watershed and Peak Flow Statistics for Tandam Branch
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039.13 Hydraulics
The dimensional parameters for the proposed stream at Tandam Branch were calculated by referencing
the work of Barbara Doll. Her work statistically analyzed the dimensional characteristics of pristine streams
within the coastal regions of North Carolina to determine the parameters of stable, healthy streams.
PARAMETER
VALUE
UNIT
AREA OF BANKFULL (Abkf)
20.8
SQFT
FLOW AT BANKFULL (Qbkf)
24.5
CFS
WIDTH OF BANKFULL (Wbkf)
13.3
FT
DEPTH AT BANKFULL (Dbkf)
1.5
FT
Figure 3: Dimensional Parameters of the Proposed Stream at Tandam Branch
039.0 Proposed Design
The proposed stream section of Tandam Branch will utilize control structures to maintain grade, prevent
unwanted erosion, and promote pool scour to increase biodiversity within the stream. These structures will
include 6 Log Sills that will be installed at the start of each pool section. They will allow the stream to hold
grade during high -flow storm events. The banks of the channel will be graded back at a stable slope and
side slopes will be matted with fiber matting and staked with live stakes to restore bank integrity.
OLDS1 DUPLIN COUNTY
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040 — Dark Branch
040.A Hydrology
Watershed characteristics for Dark Branch were determined primarily through the USGS StreamStats tool
along with field reconnaissance. It was found that the watershed draining into the stream is approximately
2.34 sq miles (1498 Acres) in size and has a 50-year peak flow of approximately 515 CFS (Figure 4). A
detailed Drainage Area and Soils Map for the Dark Branch watershed is included in Appendix A. The
project site is located in Flood Zone AE with a base flood elevation of 67.4 ft.
.: 3
PEAK FLOW STATISTICS
STATISTIC
VALUE
UNIT
2-YEAR PEAK FLOOD
105
CFS
5-YEAR PEAK FLOOD
210
CFS
10-YEAR PEAK FLOOD
294
CFS
25-YEAR PEAK FLOOD
411
CFS
50-YEAR PEAK FLOOD
515
CFS
Figure 4: StreamStats Watershed and Peak Flow Statistics for Dark Branch
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083.13 Hydraulics
The dimensional parameters for the proposed stream at Dark Branch were calculated by referencing the
work of Barbara Doll. Her work statistically analyzed the dimensional characteristics of pristine streams
within the coastal regions of North Carolina to determine the parameters of stable, healthy streams.
PARAMETER
VALUE
UNIT
AREA OF BANKFULL (Abkf)
25.4
SQFT
FLOW AT BANKFULL (Qbkf)
30.5
CFS
WIDTH OF BANKFULL (Wbkf)
14.9
FT
DEPTH AT BANKFULL (Dbkf)
1.7
FT
Figure 5: Dimensional Parameters of the Proposed Stream at Dark Branch
083.0 Proposed Design
The proposed section of stream at Dark Branch will implement multiple Log Sill structures as a means for
maintaining the designed grade while promoting beneficial pool scour. There are 16 proposed Log Sills
throughout the Dark Branch reach that will be installed at the start of each pool section. They will be
especially useful in maintaining grade at the upstream end, at the outlet of the existing culverts. Culverts
traditionally cause scour pools to form at both the upstream and downstream ends, and while they have
desirable characteristics, they also tend to increase in size over time. The Log Sill structures will prevent
the culvert scour pool from moving downstream and causing an excessively large pool area. The channel
banks will be graded back to stable slopes and the side slopes will be matted with fiber matting and staked
with live stakes to restore bank integrity.
043 — Sarecta Road
To repair the failing bank along Sarecta Road, stabilization of the slope is necessary. Stabilization of the
area will reduce sloughing and erosion of the roadside bank which is important to protect the adjacent
roadway and utilities. Due to the constraints of the project area and the risk to utility services, a structural
approach was favored over a natural approach. The bank will be graded back at a more stable slope and
secured with flexible concrete armor. In addition to the concrete armoring, the site will be reseeded and
vegetation will be able to take hold. The project site is at minimal flood risk in Flood Zone X.
(OLDS1 DUPLI
N COUNTY
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PERMITTING AND NEXT STEPS
It is our intent to permit all three sites under one NWP 37.
"Nationwide Permit 37 - Emergency Watershed Protection and Rehabilitation. Work done by or
funded by:
(a) The Natural Resources Conservation Service for a situation requiring immediate action under its
emergency Watershed Protection Program (7 CFR part 624);
(b) The U.S. Forest Service under its Burned -Area Emergency Rehabilitation Handbook (FSH 2509.13);
(c) The Department of the Interior for wildland fire management burned area emergency stabilization and
rehabilitation (DOI Manual part 620, Ch. 3);
(d) The Office of Surface Mining, or states with approved programs, for abandoned mine land reclamation
activities under Title IV of the Surface Mining Control and Reclamation Act (30 CFR subchapter R), where
the activity does not involve coal extraction; or
(e) The Farm Service Agency under its Emergency Conservation Program (7 CFR part 701).
In general, the prospective permittee should wait until the district engineer issues an NWP verification or
45 calendar days have passed before proceeding with the watershed protection and rehabilitation activity.
However, in cases where there is an unacceptable hazard to life or a significant loss of property or
economic hardship will occur, the emergency watershed protection and rehabilitation activity may proceed
immediately and the district engineer will consider the information in the pre -construction notification and
any comments received as a result of agency coordination to decide whether the NWP 37 authorization
should be modified, suspended, or revoked in accordance with the procedures at 33 CFR 330.5.
Notification: Except in cases where there is an unacceptable hazard to life or a significant loss of
property or economic hardship will occur, the permittee must submit a pre -construction notification to the
district engineer prior to commencing the activity (see general condition 32). (Authorities: Sections 10 and
404)"'
1https://www.swt.usace.army.miI/Portals/41 /docs/missions/requlatory/NationwidePermits/Nationwide%20Permit%203
7%20-%20Emeraencv%20Watershed%20Protection%20and%20Rehab ilitation. Ddf?ver=201 7-03-31 -150709-317
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