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ARCHIVED REPORTS_2011_1
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ARCHIVED REPORTS_2011_1
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Last modified
9/14/2020 1:02:22 AM
Creation date
7/3/2020 11:07:32 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2011_1
RECORD_ID
PR0440006
PE
4434
FACILITY_ID
FA0004515
FACILITY_NAME
FRENCH CAMP LANDFILL
STREET_NUMBER
0
STREET_NAME
MANTHEY
STREET_TYPE
RD
City
STOCKTON
Zip
95231
APN
16307035
CURRENT_STATUS
02
SITE_LOCATION
MANTHEY RD
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
SJGOV\rtan
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FilePath
\MIGRATIONS\SW\SW_4434_PR0440006_0 MANTHEY_2011_1.tif
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EHD - Public
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laboratory data generated for the current monitoring period are generally acceptable and <br /> the water quality samples collected from the French Camp Landfill appear to be <br /> representative of water quality at the site. <br /> 4.3 GROUNDWATER ELEVATIONS AND CONTOURS <br /> Prior to purging and sampling, each well was sounded for water depth using a weighted <br /> electronic sounder, and the static water level was recorded on a Well Data Sheet <br /> (Appendix Q. The groundwater elevations were calculated for each well by subtracting <br /> the depth-to-water measurement from the top-of-casing reference elevation. The current <br /> and historical groundwater elevation data for the French Camp Landfill is summarized in <br /> Table 5. <br /> The groundwater elevation data obtained during the monitoring period were used to <br /> generate the groundwater elevation contour maps shown on Figures 1 and 2. During the <br /> first quarter 2011 (Figure 1 A) groundwater flowed to the east-northeast with an average <br /> hydraulic gradient of 0.001 ft/ft. During the second quarter 2011 (Figure 1 B) <br /> groundwater flowed to the northeast with an average hydraulic gradient of 0.005 ft/ft. <br /> To calculate the approximate linear groundwater flow velocity for the site, conservative <br /> assumptions were used, including a hydraulic conductivity of 300 gallons per day per <br /> square foot(0.014 cm/sec), and an estimated effective porosity of 35 percent (CH2M Hill <br /> 2000). An estimated range in groundwater flow velocity was calculated using Darcy's <br /> Law: <br /> (( . <br /> r�i r.•nt 0.005 sec- 11 <br /> t' = - = 0014 .. )* -. 1* 2835 -� fi- -- -_ 0.57 fi clay, <br /> Ene sec 0,35 em - rliiv <br /> where: V=Groundwater flow velocity. <br /> K=Hydraulic conductivity of the water-bearing unit(0.014 cm/sec). <br /> i=Maximum hydraulic gradient: i-0.005 for the site during the monitoring period. <br /> ne=Effective porosity(n,=0.35);an estimated value. <br /> The groundwater flow rate is calculated to be 0.57 feet/day (207 feet/year). <br /> 4.4 DETECTION MONITORING PROGRAM <br /> Field and laboratory results for DMP monitoring wells (MW-6A,MW-7A, MW-8A, <br /> MW-9A, MW-9B, and MW-lOA)from the current monitoring period are summarized in <br /> Table 2. During the monitoring period, no VOCs were detected in any of the <br /> groundwater monitoring wells at the French Camp Landfill. <br /> Concentration Limits <br /> For DMP monitoring wells at the French Camp Landfill, concentration limits (CLs) as <br /> established in the WDRs are used for the water quality protection standards (WQPS). <br /> Based on a comparison of the data obtained during the current monitoring period, the <br /> following analytes were found to exceed a CL: <br /> MUM 1-0051TC_1SAI Ldoex 3 GeoLoglc Associates <br />
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