HomeMy WebLinkAboutNC0005088_CSS Assessment Work Plan_Final_20140925
Cliffside Steam Station Ash Basin
Proposed Groundwater
Assessment Work Plan
NPDES Permit NC0005088
September 25, 2014
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
TABLE OF CONTENTS
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Table of Contents
Page
Table of Contents ......................................................................................................................... i
Executive Summary .............................................................................................................. ES-1
1.0 Introduction ..................................................................................................................... 1
2.0 Site History ...................................................................................................................... 2
2.1 Plant Description ...................................................................................................... 2
2.2 Ash Basin Description ............................................................................................... 2
2.3 Regulatory Requirements ......................................................................................... 3
3.0 Receptor Information ....................................................................................................... 5
4.0 Regional Geology and Hydrogeology .............................................................................. 7
5.0 Site Geology and Hydrogeology ...................................................................................... 8
6.0 Groundwater Monitoring Results ..................................................................................... 9
7.0 Assessment Work Plan ..................................................................................................10
7.1 Ash and Soil Sampling Plan .....................................................................................10
7.1.1 Boring and Sampling Methods .......................................................................10
7.1.2 Proposed Soil and Ash Sampling Locations and Depths ...............................11
7.2 Groundwater Sampling Plan ....................................................................................12
7.2.1 Well Installation and Development .................................................................13
7.2.2 Hydrogeologic Evaluation ..............................................................................14
7.2.3 Groundwater Sampling ..................................................................................14
7.3 Surface Water Sampling Plan ..................................................................................14
7.3.1 Ash Basin Surface Water Samples ................................................................14
7.3.2 Seep Samples ...............................................................................................14
7.3.2 Suck Creek Surface Water Samples ..............................................................15
7.4 Site Hydrogeologic Conceptual Model .....................................................................15
7.5 Site-Specific Background Concentrations ................................................................15
7.6 Groundwater Model .................................................................................................15
8.0 Proposed Schedule ........................................................................................................17
9.0 References .....................................................................................................................18
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Cliffside Steam Station Ash Basin
TABLE OF CONTENTS
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Appendix A – Notice of Regulatory Requirements Letter from John E. Skvarla, III, Secretary,
State of North Carolina, To Paul Newton, Duke Energy, dated August 13, 2014.
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Cliffside Steam Station Ash Basin
TABLE OF CONTENTS
iii
List of Figures
1. Site Location Map
2. Site Layout Map
3. Proposed Well and Sample Locations
List of Tables
1. Groundwater Monitoring Requirements
2. Exceedances of 2L Standards April 5, 2011 – August 4, 2014
3. Proposed Additional Exploration and Sampling Plan
4. Soil and Ash Parameters and Analytical Methods
5. Groundwater, Surface Water, and Seep Parameters and Analytical Methods
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
EXECUTIVE SUMMARY
ES-1
Executive Summary
Duke Energy Carolinas, LLC (Duke Energy), owns and operates the Cliffside Steam Station
(CSS) which is located in Rutherford and Cleveland Counties at 573 Duke Power Road,
Cliffside, North Carolina (Figure 1). CSS is a coal-fired, generating station that currently
operates Units 5 and 6 only. The original Units 1 through 4 were retired in October 2011. Coal
ash residue and other liquid discharges from CSS’s coal combustion process have been
historically disposed in the station’s ash basins, which consist of the active ash basin, the Units
1-4 inactive ash basin, and the Unit 5 inactive ash basin (Figure 2). The discharge from the
active ash basin is permitted by the North Carolina Department of Environment and Natural
Resources (NCDENR) Division of Water Resources (DW R) under the National Pollutant
Discharge Elimination System (NPDES) Permit NC0005088.
On August 13, 2014, NCDENR issued a Notice of Regulatory Requirements (NORR) letter to
Duke Energy, pursuant to Title 15A North Carolina Administrative Code (15A NCAC) Chapter
02L.0106. The NORR stipulates that for each coal-fueled plant owned, Duke Energy will
complete a Groundwater Assessment Work Plan (Work Plan) for conducting a comprehensive
site assessment (CSA) and complete a receptor survey. In accordance with the requirements of
the NORR, HDR is in the process of completing a receptor survey to identify all receptors within
a 0.5-mile radius (2,640 feet) of the CSS ash basin compliance boundary. This receptor survey
will also address the requirements of the General Assembly of North Carolina Session 2013
Senate Bill 729 Ratified Bill (SB 729).
Soil and groundwater sampling will be performed to provide information pertaining to the
horizontal and vertical extent of potential soil and groundwater contamination. This will be
performed by sampling existing wells, installing and sampling approximately 49 additional
nested pairs of shallow and deep wells, and collecting soil and ash samples. This work will
provide information on the chemical and physical characteristics of site soils and ash, as well as
the geological and hydrogeological features of the site that influence groundwater flow and
direction and transport of constituents from the ash basin and ash storage areas. Samples of
ash basin water will be collected and used to evaluate potential impacts to groundwater and
surface water. In addition, water samples will be collected from seep sample locations identified
in July 2014 (as part of Duke Energy’s NPDES permit renewal application) to evaluate potential
impacts to surface water.
The information obtained through implementation of this W ork Plan will be utilized to prepare a
CSA report in accordance with the requirements of the NORR. If it is determined that additional
investigations are required during the review of existing data or data developed from this
assessment, Duke Energy and HDR will notify the NCDENR regional office prior to initiating
additional sampling or investigations.
HDR will also perform an assessment of risks to human health or safety and to the
environment. This assessment will include the preparation of a conceptual site model
illustrating potential pathways from the source to possible receptors.
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
INTRODUCTION
1
1.0 Introduction
Duke Energy Carolinas, LLC (Duke Energy), owns and operates the Cliffside Steam Station
(CSS), which is located in Rutherford and Cleveland Counties at 573 Duke Power Road,
Cliffside, North Carolina (Figure 1). CSS is a coal-fired, generating station that currently
operates Units 5 and 6 only. The original Units 1 through 4 were retired in October 2011. Coal
ash residue and other liquid discharges from CSS’s coal combustion process have been
historically disposed in the station’s ash basins, which consist of the active ash basin, the
Units 1-4 inactive ash basin, and the Unit 5 inactive ash basin (Figure 2). The discharge from
the active ash basin is permitted by the North Carolina Department of Environment and Natural
Resources (NCDENR) Division of Water Resources (DW R) under the National Pollutant
Discharge Elimination System (NPDES) Permit NC0005088.
On August 13, 2014, NCDENR issued a Notice of Regulatory Requirements (NORR) letter to
Duke Energy, pursuant to Title 15A North Carolina Administrative Code (15A NCAC) Chapter
02L.0106. The NORR stipulates that for each coal-fueled plant owned, Duke Energy will
conduct a comprehensive site assessment (CSA) which includes a Groundwater Assessment
Work Plan (Work Plan) and a receptor survey. In accordance with the requirements of the
NORR, HDR is in the process of completing a receptor survey to identify all receptors within a
0.5-mile radius (2,640 feet) of the CSS ash basin compliance boundary. The NORR letter is
included as Appendix A.
On behalf of Duke Energy, HDR has prepared this proposed Work Plan for performing the
groundwater assessment as prescribed in the NORR. If it is determined that additional
investigations are required during the review of existing data or data developed from this
assessment, Duke Energy and HDR will notify the NCDENR regional office prior to initiating
additional sampling or investigations.
HDR will also perform an assessment of risks to human health or safety and to the
environment. This assessment will include the preparation of a conceptual site model
illustrating potential pathways from the source to possible receptors.
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
SITE HISTORY
2
2.0 Site History
2.1 Plant Description
CSS is a coal-fired, electricity-generating facility located along the south bank of the Broad River
in Rutherford and Cleveland Counties at 573 Duke Power Road, Cliffside, North Carolina
(Figure 1). CSS currently operates Units 5 and 6 only. The original Units 1-4 were retired in
October 2011.
The site is located on the southern bank of the Broad River and lies in both Cleveland and
Rutherford Counties. The site is located north of McCraw Road and the surrounding area
generally consists of residential properties, undeveloped land, and the Broad River. McCraw
Road runs from northwest to southeast in the vicinity of the site.
2.2 Ash Basin Description
The station has one active ash basin and two inactive ash basins; the Units 1-4 inactive ash
basin, and the Unit 5 inactive ash basin as shown on Figure 1. The active ash basin and the
Units 1-4 inactive ash basin are located in Cleveland County to the east and southeast of the
CSS. The Unit 5 inactive ash basin is located in Rutherford County west of the CSS.
The active ash basin is located approximately 1,700 feet to the east-southeast of CSS adjacent
to the Broad River as shown on Figure 2. The active ash basin is impounded by earthen dikes
located between the west portion of the basin and Suck Creek and between the northeast
portion of the basin and the Broad River. The waste boundary associated with the active ash
basin is approximately 117 acres in area. The approximate maximum pond elevation of the
active ash basin is 770 feet. The main section of the pond is operated below 765 feet to have
extra storage capacity during a heavy flood event.
The two ash storage areas are located adjacent to the active ash basin. The ash located in
these storage areas was removed from the active ash basin.
The Units 1-4 inactive ash basin is located approximately 400 feet to the southeast of the retired
Units 1-4 and approximately 1,300 feet to the northeast of Unit 6, adjacent to the Broad River
(Figure 2). The Units 1-4 inactive ash basin is impounded by an earthen dike located along the
north and northeast side of the basin. The waste boundary associated with the Units 1-4
inactive ash basin is approximately 14.5 acres in area.
The Unit 5 inactive ash basin is located approximately 1,000 feet to the southwest of Unit 5 and
approximately 1,000 feet west of Unit 6, south of the Broad River (Figure 2). The Unit 5 inactive
ash basin is impounded by two earthen dikes located along the north and northeast sides of the
basin. The waste boundary associated with the Unit 5 inactive ash basin is approximately 58
acres in area.
The ash basin system has been an integral part of the station’s wastewater treatment system
which has received inflows from the ash removal system, station yard drain sump, stormwater
flows, and station wastewater. Currently, the inflows from the ash removal system and the
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Cliffside Steam Station Ash Basin
SITE HISTORY
3
station yard drainage basin are discharged through High Density Polyethylene Pipe (HDPE)
sluice lines into the active ash basin. The inflows are variable based on Unit 5 and Unit 6
operations.
Effluent from the ash basin system is discharged from the active basin to the Broad River
through a concrete discharge tower located in the northeast portion of the basin. The concrete
discharge tower drains through a 42-inch reinforced concrete pipe (RCP) into a rip-rap lined
channel that discharges to the Broad River. The ash basin pond elevation is controlled by the
use of concrete stop logs.
2.3 Regulatory Requirements
The NPDES program regulates wastewater discharges to surface waters, to ensure that surface
water quality standards are maintained. CSS is permitted to discharge wastewater under
NPDES Permit NC0005088, which authorizes discharge from the active ash basin (Outfall 002)
to the Broad River in accordance with effluent limitations, monitoring requirements, and other
conditions set forth in the permit. The Yard Drainage Basin has an emergency permitted outfall
(Outfall 002A) in the event the pumps cannot pump the water from the Yard Drainage Basin to
the active ash basin. Treated flue gas desulfurization (FGD) wastewater (Outfall 004) is routed
through an internal outfall and drains to the Yard Drainage Basin, which then pumps to the
active ash basin.
The NPDES permitting program requires that permits be renewed every five years. The most
recent NPDES permit renewal at CSS became effective on March 1, 2011, and expires on July
31, 2015.
In addition to surface water monitoring, the NPDES permit requires groundwater monitoring.
Groundwater monitoring has been performed in accordance with the permit conditions
beginning in April 2011. NPDES Permit Condition A (11), Version 1.1, dated June 15, 2011,
lists the groundwater monitoring wells to be sampled, the parameters and constituents to be
measured and analyzed, and the requirements for sampling frequency and reporting results.
These requirements are provided in Table 1.
The compliance boundary for groundwater quality at the CSS ash basin site is defined in
accordance with Title 15A NCAC 02L .0107(a) as being established at either 500 feet from the
waste boundary or at the property boundary, whichever is closer to the waste. The location of
the ash basin compliance monitoring wells, the ash basin waste boundary, and the compliance
boundary are shown on Figure 2.
The locations for the compliance groundwater monitoring wells were approved by the NCDENR
DWR Aquifer Protection Section (APS). All compliance monitoring wells included in Table 1 are
sampled three times per year (in April, August, and December). Analytical results are submitted
to the DWR before the last day of the month following the date of sampling for all compliance
monitoring wells.
The compliance groundwater monitoring system for the CSS ash basin consists of the following
monitoring wells: MW -20D, MW -20DR, MW -21D, MW -22DR, MW-23D, MW-23DR, MW -24D,
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Cliffside Steam Station Ash Basin
SITE HISTORY
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MW -24DR, and MW -25DR (shown on Figures 2 and 3). The compliance monitoring wells were
installed by Duke Energy in 2010 and 2011.
One or more groundwater quality standards (2L Standards) have been exceeded in
groundwater samples collected at monitoring wells MW -20D, MW -20DR, MW-21D, MW -22DR,
MW -23D, MW -23DR, MW-24D, MW -24DR, and MW-25DR. Exceedances have occurred for
chromium, iron, manganese, pH, sulfate, and total dissolved solids (TDS). Table 2 presents
exceedances measured at each of these groundwater monitoring wells from April 2011 through
August 2014.
Monitoring wells MW-24D and MW -24DR are considered by Duke Energy to represent
background water quality as both wells are located south of the active ash basin (i.e.,
upgradient). Monitoring wells MW -21D and MW-22DR are located to the east of the active ash
basin. Monitoring wells MW -20D and MW-20DR are located to the north of the ash basin main
dam. MW -23D and MW -23DR are located west of the active ash basin and MW -25DR is
located to the north of the ash basin across the Broad River. The locations of these compliance
monitoring wells are shown on Figure 2.
Monitoring wells MW -20D, MW -21D, MW -23D, and MW -24D were installed by rotary drilling
methods using hollow stem augers with the well screen placed at the zone where saprolite
transitions to competent bedrock (i.e., the transition zone). Upon auger refusal, the transition
zone well borings were extended approximately 10 feet into competent bedrock using HQ-sized
rock coring techniques. The well screens were placed to extend both above and below the top
of the saprolite/competent bedrock interface. Total depths for the transition wells ranged from
21.5 feet below ground surface (bgs) in MW -20D and MW -21D to 53.4 feet bgs in MW -24D.
The screen lengths ranged from 5 feet to 20 feet.1
With the exception of monitoring wells MW -24D and MW-24DR, the ash basin monitoring wells
were installed at or within the CSS ash basin compliance boundary. Monitoring wells MW -24D
and MW24DR are located approximately 150 feet outside of the most southern portion of the
compliance boundary.
Several monitoring wells were installed by Duke Energy in 1995/1996, 2005, and 2007 as part
of the voluntary monitoring system for groundwater near the ash basin. Monitoring wells
CLMW -1, CLMW -2, CLMW -3S, CLMW -3D, CLMW-4, CLMW-5S, and CLMW-6 were installed in
1995 and 1996. Monitoring wells MW -8S, MW-10S, and MW -11S were installed in 2005.
Monitoring wells MW -2D, MW -4D, MW -8D, MW -10D, and MW-11D were installed in 2007. In
addition, MW -2D-A was installed in 2011 to replace MW -2D. No groundwater samples are
currently collected from these wells under the compliance monitoring program. The locations of
the existing voluntary monitoring wells are shown on Figure 3.
1 Ash Basin Monitoring Well Installation Report, Cliffside Steam Station, MACTEC Project No. 6228-10-
5371, May 6, 2011.
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Cliffside Steam Station Ash Basin
RECEPTOR INFORMATION
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3.0 Receptor Information
The August 13, 2014, NORR states:
No later than October 14th, 2014 as authorized pursuant to 15A NCAC 02L
.0106(g), the DWR is requesting that Duke perform a receptor survey at each of
the subject facilities and submitted to the DWR. The receptor survey is required
by 15A NCAC 02L .0106(g) and shall include identification of all receptors within
a radius of 2,640 feet (one-half mile) from the established compliance boundary
identified in the respective National Pollutant Discharge Elimination System
(NPDES) permits. Receptors shall include, but shall not be limited to, public and
private water supply wells (including irrigation wells and unused or abandoned
wells) and surface water features within one-half mile of the facility compliance
boundary. For those facilities for which Duke has already submitted a receptor
survey, please update your submittals to ensure they meet the requirements
stated in this letter and referenced attachments and submit them with the others.
If they do not meet these requirements, you must modify and resubmit the plans.
The results of the receptor survey shall be presented on a sufficiently scaled
map. The map shall show the coal ash facility location, the facility property
boundary, the waste and compliance boundaries, and all monitoring wells listed
in the respective NPDES permits. Any identified water supply wells shall be
located on the map and shall have the well owner's name and location address
listed on a separate table that can be matched to its location on the map.
In accordance with the requirements of the NORR, HDR is in the process of completing a
receptor survey for CSS to identify all receptors within a 0.5-mile radius (2,640 feet) of the CSS
ash basin compliance boundary to be submitted to NCDENR no later than October 1, 2014.
This receptor survey will also address the requirements of SB 729. The receptors include, but
are not limited to, public and private water supply wells (including irrigation wells and unused or
abandoned wells) and surface water features within a 0.5-mile radius of the CSS ash basin
compliance boundary. The compliance boundary for groundwater quality, in relation to the ash
basin, is defined in accordance with Title 15A NCAC 02L .0107(a) as being established at either
500 feet from the waste boundary or at the property boundary, whichever is closer to the
source.
The receptor survey will include a map showing the coal ash facility location, the facility property
boundary, the waste and compliance boundaries, and all monitoring wells listed in the NPDES
permit. The identified water supply wells will be located on the map and the well owner's name
and location address are listed on a separate table that can be matched to its location on the
map.
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Cliffside Steam Station Ash Basin
RECEPTOR INFORMATION
6
During completion of the CSA, HDR will update the receptor information as necessary, in
general accordance with the CSA receptor survey requirements. If necessary, an updated
receptor survey will be submitted with the CSA report.
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Cliffside Steam Station Ash Basin
REGIONAL GEOLOGY AND HYDROGEOLOGY
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4.0 Regional Geology and Hydrogeology
North Carolina is divided into distinct regions by portions of three physiographic provinces: the
Atlantic Coastal Plain, Piedmont, and Blue Ridge (Fenneman, 1938). CSS is located within the
Piedmont zone, one of several northeast-trending geologic belts of the southern crystalline
Appalachians. The zone lies between the Charlotte Terrane of the Carolina zone to the east
and the Blue Ridge Terrane to the west. Rocks in the Piedmont zone have undergone intense
metamorphism, folding, faulting, and igneous intrusion.
The Piedmont zone is a fault-bounded composite stack of thrust sheets containing a variety of
gneisses, schists, amphibolites, sparse ultramafic bodies, and intrusive granitoids (Horton and
McConnell, 1991; Nelson and others, 1998). The general structure within the zone is
characterized by irregular foliation of low dip and folds transverse to the northeast regional
trend. The stratified rocks consist of thinly layered mica schist and biotite gneiss that are
interlayered with lesser amounts of amphibolite, calc-silicate rocks, hornblende gneiss, and
quartzite. Protoliths of these rocks were largely sedimentary and in part volcanic. Large and
small masses of granite and granodiorite are present throughout the belt and form concordant to
semi-concordant bodies in the country rock. Some of these granitoid bodies are gneissic and
are probably older than the poorly foliated to non-foliated facies. Small, ultramafic masses are
present along the eastern and western edges of the belt. The rocks of the central core of the
Western Piedmont zone are in the sillimanite zone of amphibolite metamorphism with the flanks
primarily in the staurolite-kyanite zone (Butler, 1991).
In the Piedmont zone, a variable thickness and degree of soil, saprolite, and weathered rock,
referred to as regolith, typically overlie crystalline bedrock. The degree of weathering typically
decreases with depth with a thoroughly weathered and structureless material at the surface
termed residuum. The residuum grades into a relatively coarse-grained material that retains the
structure of the parent bedrock and is termed saprolite (can extend to greater than 150 feet in
depth below the ground surface). Beneath the saprolite, partially weathered bedrock occurs
with depth until sound bedrock is encountered.
A transition zone may occur at the base of the regolith between the soil-saprolite and the
unweathered bedrock. This transition zone of partially weathered rock is a zone of relatively
high permeability compared to the overlying soil-saprolite and the underlying bedrock (LeGrand
2004).
Groundwater flow paths in the Piedmont are almost invariably restricted to the zone underlying
the topographic slope extending from a topographic divide to an adjacent stream. LeGrand
describes this as the local slope aquifer system. Under natural conditions, the general direction
of groundwater flow can be approximated from the surface topography (LeGrand 2004).
Groundwater recharge in the Piedmont is derived entirely from infiltration of local precipitation.
Groundwater recharge occurs in areas of higher topography (i.e., hilltops) and groundwater
discharge occurs in lowland areas bordering surface water bodies, marshes, and floodplains
(LeGrand 2004).
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Cliffside Steam Station Ash Basin
SITE GEOLOGY AND HYDROGEOLOGY
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5.0 Site Geology and Hydrogeology
Based on a review of soil boring and monitoring well installation logs provided by Duke Energy,
subsurface stratigraphy consists of the following material types: fill, alluvium, residuum,
saprolite, partially weathered rock (PWR), and bedrock. In general, residuum, PWR and
bedrock were encountered beneath most areas of the site. Alluvium was encountered in
borings advanced east of Suck Creek and north of the Broad River. Bedrock was consistently
encountered at varying depths across the site. The general stratigraphic units, in sequence
from the ground surface down to boring termination, are defined as follows:
Fill – Fill material generally consisted of re-worked sands and silts that were borrowed
from one area of the site and re-distributed to other areas. Fill was used in the
construction of dikes and presumably as cover for the ash storage area.
Ash – Although previous exploration activities, for which Duke Energy provided boring
logs, did not evaluate ash management areas of the site, ash is expected to be present
within the ash management areas (i.e., active ash basin, two inactive ash basins, and
the ash storage areas).
Alluvium – Alluvium is unconsolidated soil and sediment that has been eroded and re-
deposited by streams and rivers. Alluvium may consist of a variety of materials ranging
from silts and clays to sands and gravels. Alluvium was encountered in two boring
locations east of Suck Creek and north of the Broad River. Alluvium in these borings
was described as orange, tan, or brown fine- to coarse-grained sand.
Residuum – Residuum is in-place weathered soil that was encountered at varying
thickness (5 feet to 58 feet) across the site. Residuum was described as gray, orange,
tan, red, or brown micaceous fine-grained to coarse-grained sand or fine-grained sandy
silt.
Saprolite – Saprolite is soil developed by in-place weathering of rock. The primary
distinction from residuum is that saprolite typically retains some structure (e.g., mineral
banding) from the parent rock. Saprolite was encountered as a relatively thick layer (25
feet) in borings completed along the southern and western property boundaries.
Saprolite was described as reddish yellow to brown micaceous, stiff silty fine-grained to
medium-grained sand, silty clay and clayey silt with relict rock structure.
Partially Weathered Rock (PWR) – PW R occurs between the saprolite and bedrock
consisting of saprolite and rock remnants. This unit was encountered in most boring
locations and was described as orange, tan, gold, brown, maroon, or black micaceous
fine to coarse sand with rock fragments.
Bedrock – Bedrock was encountered across the site. Bedrock was encountered as
shallow as 18 feet below ground surface (bgs) in borings on the eastern extent of the
site and as deep as 58 feet bgs in a boring located on the southern extent of the site.
Bedrock was described as gray to bluish gray garnetiferous biotite gneiss with white to
gray quartzite seams.
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Cliffside Steam Station Ash Basin
GROUNDWATER MONITORING RESULTS
9
6.0 Groundwater Monitoring Results
From April 2011 through August 2014, the compliance groundwater monitoring wells at CSS
have been sampled a total of 11 times. During this period, these monitoring wells were sampled
in:
April 2011
August 2011
December 2011
April 2012
August 2012
December 2012
April 2013
August 2013
December 2013
April 2014
August 2014
With the exception of chromium, iron, manganese, pH, sulfate, and total dissolved solids (TDS)
the results for all monitored parameters and constituents were less than the 2L Standards.
Table 2 lists the range of 2L Standard exceedances for chromium, iron, manganese, pH,
sulfate, and TDS for the sampling events listed above.
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Cliffside Steam Station Ash Basin
ASSESSMENT WORK PLAN
10
7.0 Assessment Work Plan
Soil and groundwater sampling will be performed to provide information pertaining to the
horizontal and vertical extent of potential soil and groundwater contamination. Based on readily
available site background information, and dependent upon accessibility, HDR anticipates
collecting soil and/or ash samples during installation of approximately 49 nested monitoring well
pairs (shallow and deep). Groundwater samples will be collected from the proposed monitoring
wells. The proposed well and boring locations are listed in Table 3 and shown on Figure 3.
HDR may also resample select existing monitoring wells to supplement groundwater quality
data. This work will provide additional information on the chemical and physical characteristics
of site soils and ash, as well as the geological and hydrogeological features of the site that may
influence groundwater flow and transport of constituents from the ash basin.
Samples of ash basin water will also be collected and used to evaluate potential impacts to
groundwater and surface water. Surface water samples will also be collected from Suck Creek
at the approximate locations shown on Figure 3. If conditions allow for representative sampling,
water samples will be collected from seep sample locations (S-1 through S-11) identified in July
2014 (as part of Duke Energy’s NPDES permit renewal application) to evaluate potential
impacts to surface water. The seep sample locations identified as part of the NPDES permit
renewal were a combination of seeps and surface water sample locations. For consistency and
comparison of historical analytical data, the nomenclature for these samples will remain the
same.
A summary of the proposed exploration plan, including estimated sample quantities and soil
boring and monitoring well depths, is presented in Table 3. If it is determined that additional
investigations are required during the review of existing data or data developed from this
assessment, Duke Energy and HDR will notify the NCDENR regional office prior to initiating
additional sampling or investigations.
7.1 Ash and Soil Sampling Plan
7.1.1 Boring and Sampling Methods
Prior to drilling each boring, all down-hole equipment and tools will be cleaned by washing with
high-pressure hot water. A designated remote cleaning area will be established in the field.
Water for cleaning will be obtained from a tap or hydrant (to be designated) at CSS, or supplied
by the drilling contractor from an off-site source. Cleaning water will not require collection,
treatment, or disposal.
Borings will be advanced using hollow stem auger or roller cone drilling techniques to facilitate
collection of down-hole data. Standard Penetration Testing (SPT) (ASTM D 1586) and split-
spoon sampling will be performed at 2.5-foot to 5-foot increments using an 18-inch split-spoon
sampler. The sampler will be decontaminated with a non-phosphate detergent wash between
sampling depths. Ash and soil samples will be collected by the Project Scientist/Engineer.
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Cliffside Steam Station Ash Basin
ASSESSMENT WORK PLAN
11
Borings will be logged by the Project Scientist/Engineer and ash/soil samples will be observed,
visually classified, and photographed in the field for origin, consistency/relative density, color,
and soil type in accordance with the Unified Soil Classification System (ASTM D2487/D2488).
Samples will be identified with a unique boring number and approximate collection depth (e.g.,
AB-1 (20-25’)). Sample containers will be provided by HDR’s contracted laboratory prior to
commencement of the on-site investigation. Samples will be delivered to the analytical
laboratory in time to extract the samples within their specified hold times (to be provided by the
laboratory). HDR will provide the name, phone number, and email address of the laboratory
project manager to facilitate sample analysis coordination. Laboratory constituents and
methods for analysis of environmental ash and soil samples are presented in Table 5.
Boring locations will be surveyed for horizontal and vertical control upon completion of the field
exploration program.
7.1.2 Proposed Soil and Ash Sampling Locations and Depths
HDR anticipates collection of soil and ash samples for laboratory analysis at 8 locations within
the Unit 5 inactive ash basin waste boundary (i.e., from monitoring well borings designated as
U5-1 through U5-8), 4 locations within the Units 1-4 inactive ash basin waste boundary
(designated as IB-1 through IB-4), 5 locations within the active ash basin waste boundary
(designated as AB-1 through AB-5), and 4 locations within and immediately down gradient of
the ash storage areas (designated as AS-1 through AS-4). The borings located within these
ash management areas will extend approximately 20 feet below the ash/native soil interface or
to refusal, whichever is encountered first. In addition, HDR anticipates collection of soil samples
at four background locations (designated as BG-1, BG-2, MW -30, and MW-32).
Soil samples will not be collected for laboratory analysis during installation of monitoring wells
located outside the Unit 5 inactive ash basin, Units 1-4 inactive ash basin, and active ash basin
waste boundaries (designated as GWA-series wells) and during installation of the Unit 5 inactive
ash basin compliance groundwater monitoring wells (except for MW -30S/D and MW -32S/D).
Proposed boring locations are shown on Figure 3.
CONSTITUENT SAMPLING AND ANALYSES
In general, ash is expected to be encountered in U5-series, IB-series, AB-series, and AS-series
borings. Where present, ash samples will be collected from shallow and deeper vertical
intervals to evaluate variations in type (e.g., fly ash or bottom ash) and chemical profile of the
ash. In locations where ash thickness is expected to be greater than 30 feet, a third ash sample
may be collected from a depth mid-way between the shallow and deeper intervals in a particular
boring. Shallow ash samples will be collected from the 4-foot to 5-foot intervals and deeper ash
samples will be collected from the 1-foot to 2-foot intervals overlying the ash/native soil
interface. The depth of deeper ash samples is expected to vary based on ash thickness at each
specific boring location. Ash samples will be analyzed by HDR’s subcontract laboratory for total
and leachable inorganic compounds, as presented in Table 4.
Soil samples will be collected below the ash/native soil interface and from the terminus of each
boring to characterize soil quality beneath the ash management areas. Soil samples will be
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
ASSESSMENT WORK PLAN
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analyzed by HDR’s subcontract laboratory for total inorganics using the same constituents list
proposed for the ash samples.
INDEX PROPERTY SAMPLING AND ANALYSES
Physical characteristics of ash and soil will be tested both in the field and in the laboratory to
provide data for use in groundwater modeling. The location and depth of the index property
samples will be based on site-specific geology and decided upon in the field. Based on HDR’s
current understanding of site-specific geology, five hydrostratigraphic units are present on-site.
In general, a minimum of five in-situ permeability tests, either falling or constant head tests, will
be performed in each of the hydrostratigraphic units. In addition, a minimum of five packer tests
will be performed in bedrock.
Laboratory testing of soil and ash collected from SPT samples will include tests for grain size
(with hydrometer), specific gravity, and porosity (calculation).
7.2 Groundwater Sampling Plan
Groundwater samples will be collected from the proposed 49 nested well pairs shown on
Figure 3. Groundwater quality data may be supplemented through evaluation of historical data
or re-sampling of select existing monitoring wells. The purpose and anticipated construction
details of the proposed monitoring wells are as follows:
U5-series Wells – One shallow well screened across the water table (10-foot to 15-foot
well screen) and one deep well screened in the transition zone (5-foot well screen in
weathered rock below auger refusal) will be installed at each location. The U5-series
well locations were selected to provide water quality data in and beneath the Unit 5
inactive ash basin.
IB-series Wells – One shallow well screened across the water table (15-foot well screen)
and one deep well screened in the transition zone (5-foot well screen in weathered rock
below auger refusal) will be installed at each location. The IB-series well locations were
selected to provide water quality data in and beneath the Units 1-4 inactive ash basin.
AB-series Wells – One shallow well screened across the water table (10-foot to 15-foot
well screen) and one deep well screened in the transition zone (5-foot well screen in
weathered rock below auger refusal) will be installed at each location. The AB-series
well locations were selected to provide water quality data in and beneath the active ash
basin.
AS-series Wells – One shallow well screened across the water table (10-foot to 15-foot
well screen) and one deep well screened in the transition zone (5-foot well screen in
weathered rock below auger refusal) will be installed at each location. The AS-series
well locations were selected to provide water quality data in, beneath, and immediately
down gradient of the ash storage areas.
GWA-series Wells – One shallow well screened across the water table (15-foot well
screen) and one deep well screened in the transition zone (5-foot well screen in
weathered rock below auger refusal) will be installed at each location. The GWA-series
well locations were selected to provide water quality data beyond the waste boundary for
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
ASSESSMENT WORK PLAN
13
use in groundwater modeling (i.e., to evaluate the horizontal and vertical extent of
potentially impacted groundwater around the ash basins).
MW -30S/D, MW -32S/D, MW -34S/D, MW-36S/D, MW -38S/D, MW-40S/D, and MW -
42S/D Wells – One shallow well screened across the water table (15-foot well screen)
and one deep well screened in the transition zone (5-foot well screen in weathered rock
below auger refusal) will be installed at each location. These wells were proposed in the
station’s July 2014 NPDES permit renewal application and will be installed as part of this
assessment work.
BG-series Wells – One shallow well screened across the water table (15-foot well
screen) and one deep well screened in the transition zone (5-foot well screen in
weathered rock below auger refusal) will be installed at each location. Note that Unit 5
inactive ash basin compliance wells MW -30S/D and MW -32S/D are considered to be
background wells at this time. The background well locations were selected to provide
additional physical separation from possible influence of the ash basin on groundwater.
These wells will also be useful in the statistical analysis to determine the site-specific
background water quality concentrations (SSBCs).
7.2.1 Well Installation and Development
SHALLOW MONITORING WELLS
At each monitoring well location specified on Figure 3 with an “S” qualifier in the well name (e.g.,
AB-1S), a shallow well will be constructed with a 2-inch-diameter, schedule 40 PVC screen and
casing. Each of these wells will have a 10-foot to 15-foot well screen (0.010-slot) set to bracket
the water table at the time of installation.
DEEP MONITORING WELLS
At each monitoring well location specified on Figure 3 with a “D” qualifier in the well name (e.g.,
AB-1D), a double-cased deep well will be constructed with a 6-inch-diameter PVC outer casing
and a 2-inch-diameter PVC inner casing and well screen. The purpose of installing cased wells
at the site is to restrict vertical mixing within the shallow and deeper portions of the unconfined
aquifer during well installation. Outer well casings (6-inch casing) will be advanced to auger
refusal and set approximately 1 foot into PWR. Note that location-specific subsurface geology
will dictate actual casing depths on a per-well basis. Air rotary drilling will be used to advance
the borehole a minimum of 10 feet into PWR or bedrock with the intent of setting a 5-foot well
screen at least 10 feet below the bottom of the outer casing.
All newly installed monitoring wells will be developed using appropriate measures (e.g.,
agitation, surging, pumping, etc.). Water quality parameters (specific conductance, pH,
temperature, and turbidity) will be measured and recorded during development and should
stabilize before development is considered complete. Development will continue until
development water is visually clear (target < 50 Nephelometric Turbidity Units (NTU) Turbidity)
and sediment free. Following development, sounding the bottom of the well with a water level
meter should indicate a “hard” (sediment free) bottom. Development records will be prepared
under the direction of the Project Scientist/Engineer and will include development method(s),
water volume removed, and field measurements of temperature, pH, conductivity, and turbidity.
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
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7.2.2 Hydrogeologic Evaluation
Hydraulic conductivity (slug) tests will be completed in select monitoring wells under the
direction of the Project Scientist/Engineer. Slug tests will be performed to meet the
requirements of the NCDENR Memorandum titled, “Performance and Analysis of Aquifer Slug
Tests and Pumping Tests Policy, dated May 31, 2007.” Water level change during the slug
tests will be recorded by a data logger.
In addition, approximately 5 to 10 packer tests will be conducted during installation of the
Type III wells to facilitate permeability testing of the upper five feet of rock.
7.2.3 Groundwater Sampling
Subsequent to monitoring well installation and development, each newly installed well will be
sampled using low-flow sampling techniques. During low-flow purging and sampling,
groundwater is pumped into a flow-through chamber at flow rates that minimize or stabilize
water level drawdown within the well. Indicator parameters are measured over time (usually at
5-minute intervals). When parameters have stabilized within ±0.2 pH units and ±10 percent for
temperature, conductivity, and dissolved oxygen (DO), and ±10 millivolts (mV) for oxidation
reduction potential (ORP) over three consecutive readings, representative groundwater has
been achieved for sampling. Turbidity levels of 10 NTU or less will be targeted prior to sample
collection. Groundwater samples will be analyzed by a North Carolina certified laboratory for
the constituents included in Table 5. Select constituents may be analyzed for total and
dissolved concentrations.
7.3 Surface Water Sampling Plan
7.3.1 Ash Basin Surface Water Samples
Surface water samples will be collected from the approximate open water locations in the Unit 5
inactive ash basin and the active ash basin shown on Figure 3. At each open water location,
two water samples will be collected – one sample close to the surface (i.e., 0 to 1 foot from
surface) and one sample at the approximate middle depth of the water body. The middle depth
sample will vary based on the water level in the water body. In areas where the water body is
less than 5 feet deep, one water sample will be collected from the location at the approximate
middle depth of the water body. Ash basin surface water samples and surface water samples
will be analyzed for the same constituents as groundwater samples listed in Table 5. Select
constituents may be analyzed for total and dissolved concentrations.
7.3.2 Seep Samples
Water samples will be collected from the seep sample locations shown on Figure 3 (S-1 through
S-11). The seep samples will be collected for laboratory analysis of the constituents listed in
Table 5. Select constituents may be analyzed for total and dissolved concentrations. Duke
Energy collects surface water samples from the Broad River at upstream and downstream
locations for their existing NPDES permit requirements. If seep analytical results indicate
potential for impacts to the Broad River, then surface water quality data collected in the river will
be reviewed.
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Cliffside Steam Station Ash Basin
ASSESSMENT WORK PLAN
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7.3.3 Suck Creek Surface Water Samples
Water samples will be collected from Suck Creek upstream and downstream of the active ash
basin from the locations shown on Figure 3. The creek samples will be collected for laboratory
analysis of the constituents listed in Table 5. Select constituents may be analyzed for total and
dissolved concentrations.
7.4 Site Hydrogeologic Conceptual Model
The data obtained during the proposed assessment will be supplemented by available reports
and data on site geotechnical, geologic, and hydrologic conditions to develop a site
hydrogeologic conceptual model (SCM). The NCDENR document, “Hydrogeologic Investigation
and Reporting Policy Memorandum,” dated May 31, 2007 (Reference 6), will be used as general
guidance. In general, the SCM will utilize site information to characterize the geologic and
hydrogeologic characteristics of the area of interest, and, where appropriate, lead directly to the
proper construction of a groundwater flow and transport model.
7.5 Site-Specific Background Concentrations
Statistical analysis will be performed to determine the SSBCs to assess whether or not
exceedances can be attributed to naturally occurring background concentrations or attributed to
potential contamination. Specifically, the relationship between exceedances and turbidity will be
explored to determine whether or not there is a possible correlation due to naturally occurring
conditions and/or well construction.
7.6 Groundwater Model
Groundwater flow and chemical constituent fate and transport at the site will be modeled in
three dimensions using the MODFLOW -2005 groundwater flow numeric engine and the MT3D
transport model with linear isotherm sorption to predict chemical constituent concentrations over
time at the compliance boundary.
The groundwater model layers will be developed based on hydrogeologic properties and other
data obtained during the site investigation and the SCM. The model will include the effects of
recharge from precipitation.
Site soil samples will be collected and used to develop site-specific distribution coefficient, Kd,
terms using batch methods (US EPA Batch-type procedures for estimating soil adsorption of
chemicals Technical Resource Document 530/SW-87/006-F).
The selection of the initial concentrations and the predictions of the concentrations for
constituents with respect to time are to be developed with consideration of the following data:
Site-specific analytical results from leach tests and from total digestion of ash samples
taken at varying locations and depths within the ash basin and ash storage piles (if
present).
Analytical results from appropriate groundwater monitoring wells or surface water
sample locations outside of the ash basin.
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Analytical results from monitoring wells installed in the ash basin pore-water (screened
in ash).
Published or other data on sequential leaching tests performed on similar ash.
The groundwater modeling will be conducted in general conformance with the requirements of
the May 31, 2007, NCDENR Memorandum titled, “Groundwater Modeling Policy.”
The groundwater model and the report on the results of the groundwater modeling will be
prepared by Dr. William Langley, P.E., Department of Civil and Environmental Engineering,
University of North Carolina at Charlotte. Dr. Langley will perform the work under contract with
HDR, and the groundwater model report will be included as an attachment to the CSA. The
groundwater model will be used, as required, to evaluate options for potential corrective action
in the subsequent phase of work.
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
PROPOSED SCHEDULE
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8.0 Proposed Schedule
Duke Energy will submit the CSA Report within 180 days of NCDENR approval of this Work
Plan. The anticipated schedule for implementation of field work, evaluation of data, and
preparation of the Work Plan is presented in the table below.
Activity Start Date Duration to Complete
Field Exploration Program 10 days following Work Plan approval 75 days
Receive Laboratory Data 14 days following end of Exploration Program 15 days
Evaluate Lab/Field Data, Develop SCM 5 days following receipt of Lab Data 30 days
Prepare and Submit CSA 10 days following Work Plan approval 170 days
Duke Energy Carolinas, LLC | Proposed Groundwater Assessment Work Plan
Cliffside Steam Station Ash Basin
REFERENCES
18
9.0 References
1. Butler, J. R., 1991, Metamorphism, p. 127-141, in Horton, J. W., Jr. and Zullo, V. A.,
eds., The Geology of the Carolinas: The University of Tennessee Press, Knoxville, TN,
406p.
2. Fenneman, Nevin Melancthon. “Physiography of eastern United States.” McGraw-Hill.
1938.
3. Horton, J. W., Jr. and McConnell, K. I., 1991, The western Piedmont, p. 36-58, in Horton,
J. W., Jr. and Zullo, V. A., eds., The Geology of the Carolinas: The University of
Tennessee Press, Knoxville, TN, 406p.
4. LeGrand, Harry E. 2004. A Master Conceptual Model for Hydrogeological Site
Characterization in the Piedmont and Mountain Region of North Carolina, A Guidance
Manual, North Carolina Department of Environment and Natural Resources Division of
Water Quality, Groundwater Section.
5. Nelson, A. E., Horton, J. W., Jr., and Clarke, J. W., 1998, Geologic map of the Greenville
1o x 2o quadrangle, Georgia, South Carolina, and North Carolina: United States
Geological Survey, Miscellaneous Investigations Series Map I-2175, Scale 1:250,000.
6. NCDENR Memorandum “Performance and Analysis of Aquifer Slug Tests and Pumping
Tests Policy,” May 31, 2007.
7. NCDENR document, “Hydrogeologic Investigation and Reporting Policy Memorandum”,
dated May 31, 2007.
8. US EPA Batch-type procedures for estimating soil adsorption of chemicals
TechnicalResource Document 530/SW -87/006-F.
Figures
TAFFTJULY 31, 2014
SEPT. 19, 2014
Tables
TABLE 1 – GROUNDWATER MONITORING REQUIREMENTS
Well Nomenclature Constituents and Parameters Frequency
Monitoring Wells: MW-20D,
MW-20DR, MW-21D, MW-22DR,
MW-23D, MW-23DR, MW-24D,
MW-24DR, MW-25DR
Antimony Chromium Nickel Thallium
April,
August,
December
Arsenic Copper Nitrate Water Level
Barium Iron pH Zinc
Boron Lead Selenium
Cadmium Manganese Sulfate
Chloride Mercury TDS
TABLE 2 – EXCEEDANCES OF 2L STANDARDS APRIL 5, 2011 – AUGUST 4, 2014
Parameter Chromium Iron Manganese pH Sulfate TDS
Units µg/L µg/L µg/L SU mg/L mg/L
2L
Standard 10 300 50 6.5 - 8.5 250 500
Well ID Range of Exceedances
MW-20D No
Exceedances 3,470 – 8,620 459 – 649 No
Exceedances
No
Exceedances
No
Exceedances
MW-20DR No
Exceedances 330 600 – 704 No
Exceedances
No
Exceedances
No
Exceedances
MW-21D No
Exceedances
No
Exceedances 57 – 84 4.6 – 5.2 No
Exceedances
No
Exceedances
MW-22DR No
Exceedances 3,220 – 9,890 82 – 148 5.4 – 6.4 No
Exceedances
No
Exceedances
MW-23D 14 349 – 1,130 410 – 759 No
Exceedances 280 – 430 590 – 820
MW-23DR No
Exceedances 828 – 1,240 51 – 54 No
Exceedances
No
Exceedances
No
Exceedances
MW-24D No
Exceedances 382 – 2,170 87 5.1 – 5.4 No
Exceedances
No
Exceedances
MW-24DR No
Exceedances 934 – 1,710 54 – 61 No
Exceedances
No
Exceedances
No
Exceedances
MW-25DR 45 347 – 6,610 213 5.9 – 6.5
8.7 – 9.5
No
Exceedances
No
Exceedances
TABLE 3 – ENVIRONMENTAL EXPLORATION AND SAMPLING PLAN
CLIFFSIDE STEAM STATION
Exploration Area Soil Borings Shallow Monitoring Wells Deep Monitoring Wells Surface Water
Boring IDs Quantity
Estimated
Boring Depth
(ft bgs)
Well IDs Quantity
Estimated
Well Depth
(ft bgs)
Screen
Length
(ft)
Well IDs Quantity
Estimated
Casing Depth
(ft bgs)
Estimated
Well Depth
(ft bgs)
Screen
Length
(ft)
Quantity
of
Locations
Quantity
of
Samples
Unit 5 Inactive
Ash Basin
U5-1 through
U5-8 8 40-90 U5-1S through
U5-8S 8 15-50 10-15 U5-1D through
U5-8D 8 25-75 40-90 5 1 2
Units 1-4 Inactive
Ash Basin
IB-1 through
IB-4 4 55-105 IB-1S through
IB-4S 4 30-60 10-15 IB-1D through
IB-4D 4 40-90 55-105 5 N/A N/A
Active Ash Basin AB-1 through
AB-5 5 65-115 AB-1S through
AB-5S 5 40-80 15 AB-1D through
AB-5D 5 50-100 65-115 5 3 6
Ash Storage
Areas
AS-1 through
AS-4 4 55-105 AS-1S through
AS-4S 4 30-60 10-15 AS-1D through
AS-4D 4 40-90 55-105 5 N/A N/A
Beyond Waste
Boundary N/A 0 N/A
GWA-1S through
GWA-6S,
GWA-10S through
GWA-14S,
GWA-20S through
GWA-27S
19 20-50 15
GWA-1D through
GWA-6D,
GWA-10D through
GWA-14D,
GWA-20D through
GWA-27D
19 30-80 45-95 5 N/A N/A
Unit 5 Inactive
Ash Basin
Compliance
Boundary 6
MW -30, MW -32,
MW -34, MW -36,
MW -38, MW -40,
MW -42
7 45-95
MW -30S, MW -32S,
MW -34S, MW -36S,
MW -38S, MW -40S,
MW -42S
7 20-50 15
MW -30D, MW -32D,
MW -34D, MW -36D,
MW -38D, MW -40D,
MW -42D
7 30-80 45-95 7 N/A N/A
Background BG-1 and
BG-2 2 55-105 BG-1S and
BG-2S 2 30-50 15 BG-1D and
BG-2D 2 40-90 55-105 5 N/A N/A
Notes:
1. Estimated boring and well depths based on data available at the time of work plan preparation and subject to change based on site-specific conditions in the field.
2. Laboratory analyses of soil, ash, groundwater, and surface water samples will be performed in accordance with the constituents and methods identified in Tables 4 and 5.
3. Additionally, soils will be tested in the laboratory to determine grain size (with hydrometer), specific gravity, and perm eability.
4. During drilling operations, downhole testing will be conducted to determine in-situ soil properties such as horizontal and vertical hydraulic conductivity.
5. Actual number of field and laboratory tests will be determined in field by Field Engineer o r Geologist in accordance with project specifications.
6. Unit 5 Inactive Ash Basin Compliance Boundary monitoring wells MW -30S/D and MW -32S/D are considered to be background locations.
TABLE 4 – SOIL AND ASH PARAMETERS AND ANALYTICAL METHODS
INORGANIC COMPOUNDS UNITS METHOD
Antimony mg/kg EPA 6020
Arsenic mg/kg EPA 6020
Barium mg/kg EPA 6010
Boron mg/kg EPA 6010
Cadmium mg/kg EPA 6020
Chloride mg/kg SM4500-Cl-E
Chromium mg/kg EPA 6010
Copper mg/kg EPA 6010
Iron mg/kg EPA 6010
Lead mg/kg EPA 6020
Manganese mg/kg EPA 6010
Mercury mg/kg EPA Method 7470A/7471
Nickel mg/kg EPA 6010
pH SU EPA 9045
Selenium mg/kg EPA 6020
Thallium (low level) mg/kg EPA 6020
Zinc mg/kg EPA 6010
Notes:
1. Soil samples to be analyzed for Total Inorganics using U.S. Environmental Protection Agency
(USEPA) Methods 6010/6020 and pH using USEPA Method 9045, as noted above.
2. Ash samples to be analyzed for Total Inorganics using USEPA Methods 6010/6020 and pH using
USEPA Method 9045; select ash samples will also be analyzed for leaching potential using Synthetic
Precipitation Leaching Procedure (SPLP) Extraction Method 1312 in conjunction with USEPA Methods
6010/6020. SPLP results to be reported in units of mg/L for comparison to 2L Standards.
TABLE 5 – GROUNDWATER, SURFACE WATER, AND SEEP PARAMETERS AND ANALYTICAL
METHODS
PARAMETER UNITS METHOD
FIELD PARAMETERS
pH SU Field Water Quality Meter
Specific Conductance mmho/cm Field Water Quality Meter
Temperature ºC Field Water Quality Meter
Dissolved Oxygen mg/L Field Water Quality Meter
Oxidation Reduction Potential mV Field Water Quality Meter
NPDES CONSTITUENTS
Antimony µg/L EPA 200.8 or 6020
Arsenic µg/L EPA 200.8 or 6020
Barium µg/L EPA 200.7 or 6010
Boron µg/L EPA 200.7 or 6010
Cadmium µg/L EPA 200.8 or 6020
Chloride mg/L EPA 300.0
Chromium µg/L EPA 200.7 or 6010
Copper mg/L EPA 200.7 or 6010
Iron µg/L EPA 200.7 or 6010
Lead µg/L EPA 200.8 or 6020
Manganese µg/L EPA 200.7 or 6010
Mercury µg/L EPA 245.1
Nickel µg/L EPA 200.7 or 6010
Nitrate as Nitrogen mg-N/L EPA 300.0
Selenium µg/L EPA 200.8 or 6020
Sulfate mg/L EPA 300.0
Thallium (low level) µg/L EPA 200.8 or 6020
Total Dissolved Solids mg/L EPA 160.1 or SM 2540C
Zinc mg/L EPA 200.7 or 6010
ADDITIONAL GROUNDWATER CONSTITUENTS
Alkalinity (as CaCO3) mg/L SM2320B
Calcium mg/L EPA 200.7
Ferrous Iron mg/L SM4500-Fe
Magnesium mg/L EPA 200.7
Potassium mg/L EPA 200.7
Sodium mg/L EPA 200.7
Sulfide mg/L SM4500S-F
Total Organic Carbon mg/L SM5310
Notes:
1. Select constituents may be analyzed for total and dissolved concentrations.
Appendix A
Notice of Regulatory Requirements Letter from
John E. Skvarla, III, Secretary, State of North
Carolina, to Paul Newton, Duke Energy, dated
August 13, 2014.