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ARCHIVED REPORTS_2008
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ARCHIVED REPORTS_2008
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Last modified
9/14/2020 3:17:15 AM
Creation date
7/3/2020 11:07:18 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2008
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_2008.tif
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EHD - Public
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® 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, which <br /> indicates that groundwater flow varied from 0.002 ft/ft to the northwest during the first <br /> quarter 2008 monitoring period to 0.001 ft/ft to the southeast during the second quarter <br /> 2008 monitoring period. <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 /> Kicm 0.002 sec– ft <br /> V = —_ [(0.014 —)* ]*2835 0.227 ft/day <br /> ne sec 0.35 cm – day <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 a 0.002 for the site during the monitoring period. <br /> ne=Effective porosity(ne=0.35);an estimated value. <br /> The maximum groundwater flow rate is calculated to be 0.227 feet/day (83 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 and time-series plots are presented in Appendix D. As shown in the time-series <br /> plots, general chemistry and metals constituent concentrations are generally consistent <br /> with historical concentrations. During the monitoring period,no organic constituents <br /> were detected. <br /> Concentration Limits <br /> For DMP monitoring wells at the French Camp Landfill, concentration limits (CLs) are <br /> used for the water quality protection standards �WQPS). The CLs shown in Table 2 were <br /> calculated by Herst &Associates using Sanitas , a state-approved statistical software <br /> ® program, using historical data from background wells MW-6A and MW-7A, and are <br /> DA2005-0012TC_1SAOBro Ldot <br /> Geologic Associates <br />
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