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ARCHIVED REPORTS_2010_11
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ARCHIVED REPORTS_2010_11
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Last modified
7/17/2020 3:53:35 PM
Creation date
7/3/2020 10:55:15 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2010_11
RECORD_ID
PR0440005
PE
4433
FACILITY_ID
FA0004516
FACILITY_NAME
FORWARD DISPOSAL SITE
STREET_NUMBER
9999
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
MANTECA
Zip
95336
APN
20106001-3, 5
CURRENT_STATUS
01
SITE_LOCATION
9999 AUSTIN RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
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FilePath
\MIGRATIONS\SW\SW_4433_PR0440005_9999 AUSTIN_2010_11.tif
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EHD - Public
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hexavalent chromium and nitrate as nitrogen concentrations reported for well MW-1 are <br /> within the historical range of values reported for this well. Based on the results of the <br /> laboratory QA/QC analyses, it is concluded that the laboratory data generated for the <br /> third quarter 2010 monitoring period are generally acceptable and the water quality <br /> samples collected from the Forward Unit appear to be representative of water quality at <br /> the site. <br /> 2.1.3 Groundwater Elevations and Contours <br /> Prior to purging and sampling, each well was sounded for water depth using a weighted <br /> electronic sounder to an accuracy of 0.01 foot, and the static water level was recorded on <br /> a Well Data Sheet(Appendix C). The groundwater elevations were calculated for each <br /> well by subtracting the depth-to-water measurement from the top-of-casing reference <br /> elevation. The current groundwater elevation data for the Forward Unit is summarized in <br /> Table 2-3. <br /> The groundwater elevation data obtained during the third quarter 2010 monitoring period <br /> were used to generate the groundwater elevation contour map shown on Figure <br /> 2-1, which indicates that groundwater generally flows to the northeast towards the Austin <br /> Unit, at an average hydraulic gradient of approximately 0.003 ft/ft. <br /> To calculate the approximate linear groundwater flow velocity for the site, conservative <br /> assumptions were used, including a hydraulic conductivity of 875 gallons per day per <br /> square foot(0.04 cm/sec) and an estimated effective porosity of 35 percent (CH2M Hill <br /> 2000). An estimated groundwater flow velocity was calculated using Darcy's Law: <br /> Ki cm 0.003 sec– ft <br /> V = — = [(0.04 —)* 1*2835 0.972 ftlday <br /> ne sec 0.35 cm – day <br /> where: V=Groundwater flow velocity. <br /> K=Hydraulic conductivity of the water-bearing unit(0.04 cm/sec). <br /> i=Hydraulic gradient: i�0.003 for the site during the third quarter 2010. <br /> ne=Effective porosity(ne=0.35);an estimated value. <br /> The groundwater flow rate is calculated to be 0.972 feet/day(355 feet/year). <br /> 2.1.4 Detection Monitoring Program <br /> Field and laboratory results for the groundwater monitoring wells for the third quarter <br /> 2010 are summarized in Table 2-2. In the sample collected from well DW-9690, trans- <br /> 1,4-dichloro-2-butene was measured above the practical quantitation limit (PQL); acetone <br /> was measured above the PQL in the sample collected from well MW-19; and <br /> tetrachloroethane(PCE), and trichloroethene(TCE) were detected at estimated trace <br /> concentrations (between the method detection limit [MDL] and the PQL) in the sample <br /> collected from well MW-14. <br /> D:\20t0 0013\FA_3Q10.doc <br /> 5 <br />
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