HomeMy WebLinkAboutWS-9571_44769_G_C_20170823_RSPNSNOV
1818 Perimeter Road • Dawsonville, GA 30534
706-579-1607 PHONE • 1-706-265-4916 FAX • www.millcreekenvironmental.com
August 23, 2017
North Carolina Department of Environment Quality
UST Section, Division of Waste Management
450 West Hanes Mill Road, Suite 300
Winston-Salem, North Carolina 17105
Attn: Ms. Karen J. Hall, Environmental Senior Technician
karen.j.hall@ncdenr.gov
Subject: Response to NOV, Limited Site Assessment (LSA)
Nick’s Motor Cars
3384 West US Highway 421
Wilkesboro, Wilkes County, North Carolina 28697
Incident Number: 44769
Dear Ms. Hall,
Mill Creek Environmental, LLC (MCE) has received your letter dated June 15, 2017 concerning
the subject property. The purpose of this letter is to respond to your comments (italics) and
provide additional information for the site. The following are our responses to your comments:
1) Comment: Water Supply Well Survey (we need this to rank the site).
Response: The Expanded Well Survey map is attached as Figure 1 and Table 1. Based on the
results of the Expanded Well Survey, MCE has identified nine (9) water supply wells within
1,500 feet of the subject property. Seven (7) of the wells are unused and two (2) are used. The
following is a summary of the two used wells identified on the attached map:
Well #2
This well is located approximately 957 feet southwest of the tank basin on the subject
property. Well #2 serves a residence and was reported by the homeowner to be used on an as-
needed basis. The homeowner reported the well as being turbid during our site visit. They
switch a valve to the municipal water system as-needed. This well is located cross-gradient
and across a topographic divide from the subject property. Construction details and depth of
this well are unknown.
Well #8
This well is located approximately 650 feet southwest of the tank basin on the subject
property. Well #8 serves a small appliance repair and sales operations and was in use at the
time of our site visit. The well is located on the west side of a topographic divide that
separates the subject property from the well. This well is drilled into bedrock and constructed
with 6-inch PVC surface casing.
Ms. Karen J. Hall
August 23, 2017
Page 2 of 2
P:\Nicks Auto Cars Wilkesboro NC UST LSA\Report\Response Letter to NC Env Quality .docx
Much is known about the geology and hydrogeology of the region and generalizations can be
made to predict the fate and transport of contaminants in this geologic setting. The
generalizations are from “A Master Conceptual Model for Hydrogeological Site
Characterization in the Piedmont and Mountain Region of North Carolina” (Harry E. LeGrand,
Sr., North Carolina Department of Environment and Natural Resources Division of Water
Quality, Groundwater Section, 2004). The generalizations were compiled from large amounts of
data and were used to develop a conceptual model to assist in evaluating the potential risk
associated with this site. The following are key generalizations from LeGrand, 2004, that were
useful in conducting a risk evaluation for this site:
Groundwater occurs in two separate media in the Piedmont and Mountain Regions: 1)
clayey granular soil and saprolite, and; 2) fractures and linear openings in the bedrock.
The soil and saprolite have a relatively large groundwater storage capacity, but transmits
it slowly. The bedrock fracture system has a relatively low storage capacity, but can
transmit water readily where fractures interconnect.
Groundwater generally flows toward streams and discharges at seeps and springs in
lowland areas.
Streams are linear lows in the water table. Topography of the water table generally
mimics that of the ground surface, but with less relief.
The behavior of groundwater can be estimated using a slope aquifer model where natural
conditions prevail. This is a general concept which states that groundwater recharge
occurs in upland areas and discharge occurs in local perennial streams. Only under rare
conditions does groundwater pass beneath a perennial stream to a more distant stream or
cross a topographic high point.
Based on the aquifer slope model, it is inferred that groundwater flow in the surficial and
bedrock aquifers at the subject property mimic topography, and flow to the east towards the
nearest down slope stream. Under static conditions, groundwater would not typically cross a
hydraulic boundary such as a topographic high point or a stream. Due to the anticipated low
pumping volume of the 6-inch drilled wells at residences and small businesses, it would not be
expected that there is sufficient pumping rate or volume to overcome the large storage volume of
the aquifers and the natural flow gradients towards the east from the subject property.
Based on the slope aquifer model and the anticipated pumping rate of the two used wells, it is
our opinion that the potential for the used wells to be impacted by the release from the subject
property is low.
2) Comment: Soil samples at the pump island that were missed during the closure. I had asked
that they be taken as part of the LSA.
Response: MCE was not copied on correspondence concerning pump island sampling and
was unaware of this request when the site was drilled for the LSA.
Ms. Karen J. Hall
August 23, 2017
Page 3 of 2
P:\Nicks Auto Cars Wilkesboro NC UST LSA\Report\Response Letter to NC Env Quality .docx
Based on the data collected during the LSA, it does not appear that additional testing is
warranted at this time. The bases for this determination is as follows:
Soil boring SB-1 was drilled to 50 feet below ground surface (BGS) without
encountering groundwater.
Benzene was detected in soil sample SB-1, 48-50’ at a concentration that exceeds the
Soil-to-Water Maximum Contaminant Concentration (MSCC) by 0.0001 milligram per
kilogram. No other regulated compounds exceeded their respective MSCC,
Industrial/Commercials CL, or Residential CL values.
The large unsaturated soil zone above groundwater serves to provide treatment of
residual petroleum through natural attenuation processes such as biodegradation,
dispersion, volatilization, and absorption.
The former pump islands are located sufficiently close to the former UST basin that the
soil samples from the UST basin, collected at depths of approximately 25, 40, and 50 feet
BGS are sufficient to evaluate potential soil contamination from the pump island
locations. This evaluation is sufficient due to the increased dispersion of petroleum in soil
with depth, allowing a near surface release to be evaluated for risk by collecting a deep
soil sample in the general vicinity.
The petroleum release does not pose a threat of explosion due the accumulation of vapors
in a confined space nor does the release pose a risk to public health or the environment.
Based on the data collected during the LSA and our additional evaluation described above, MCE
recommends a “No Further Action Required” (NFAR) status for this site.
If you have any questions, or if MCE can be of assistance in any other capacity, please don’t
hesitate to call the undersigned at 706-579-1607.
Sincerely,
MILL CREEK ENVIRONMENTAL, LLC
Dan Centofanti, PG, EP Steven Van Johnson, PG
Technical Director Senior Geologist
Table 1
Well Survey Key
Well ID Property Information
1 421 Motor Sales
3290 U.S. 421
Wilkesboro, NC 28697
6 inch Drilled Well - Unused
2 Residence
2462 County Road 1313
Wilkesboro, NC 28697
6 inch Drilled Well - Used
3 Residence
2154 Congo Road
Wilkesboro, NC 28697
Well - Unused
4 Jester's Auto
2462 Congo Road
Wilkesboro, NC 28697
Block Well - Unused
5 Residence
586 Buck Road
Wilkesboro, NC 28697
24 inch Concrete Casing Well - Unused
6 Residence
260 Buck Road
Wilkesboro, NC 28697
Well - Unused
7 Residence
161 Laurelwood Drive
Wilkesboro, NC 28697
Suspected Well - Unused
8 Bob Young Appliances
3481 U.S. 421
Wilkesboro, NC 28697
Well - Used
9 Residence
3481 U.S. 421
Wilkesboro, NC 28697
Well - Unused