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ARCHIVED REPORTS_2017
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ARCHIVED REPORTS_2017
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Last modified
7/17/2020 3:53:46 PM
Creation date
7/3/2020 10:59:30 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2017
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
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SJGOV\rtan
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FilePath
\MIGRATIONS\SW\SW_4433_PR0440005_9999 AUSTIN_.tif
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EHD - Public
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Water Quality Monitoring Report <br /> Forward Landfill <br /> acceptable and the water quality samples collected from the Forward Unit appear to be <br /> representative of water quality at 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 a <br /> Well Data Sheet (Appendix F). The groundwater elevations were calculated for each well by <br /> subtracting the depth-to-water measurement from the top-of-casing reference elevation. The <br /> current groundwater elevation data for the Forward Unit is summarized in Table 2-3. <br /> The groundwater elevation data obtained on November 14, 2016, were used to generate the <br /> groundwater elevation contour map shown on Figure 2-1 for the fourth quarter 2017 <br /> monitoring period, which depicts groundwater beneath the northern half of Forward Unit <br /> generally flowing to the east-northeast at an average hydraulic gradient of 0.001 to 0.004 ft/ft, <br /> while groundwater beneath the southern half of Forward Unit generally flowing to the <br /> southeast at an average hydraulic gradient of 0.002 ft/ft, potentially controlled by agricultural <br /> well pumping on adjacent properties. <br /> To calculate the approximate linear groundwater flow velocity for the Forward Unit, <br /> conservative assumptions were used, including a hydraulic conductivity of 255 feet per day <br /> (CDM, 1997), and an estimated effective porosity of 35 percent (CH2M Hill, 2000). The <br /> maximum groundwater flow rate is calculated to be 2.9 feet per day(1064 feet/year). <br /> 2.1.4 Detection Monitoring Program <br /> Field and laboratory results for the Forward Unit groundwater monitoring wells for the fourth <br /> quarter 2017 monitoring period are summarized in Table 2-2. <br /> Non-Statistical Data Analysis <br /> The California Non-Statistical Data Analysis Method (CNSDAM) was performed for VOCs <br /> detected less than 10 percent of the time in background samples. Under the CNSDAM, a <br /> measurably significant indication of release occurs in a given sample when: two or more VOCs <br /> exceed their respective Method Detection Limits (MDLs); or one or more VOCs equals or <br /> exceeds its respective practical quantitation limit (PQL). During the fourth quarter 2017 <br /> monitoring period, non-statistical indications of a release was identified at well MW-17 as a <br /> result of a trace concentrations of 1,1-dichloroethane (1,1-DCA), dichlorodifluoromethane <br /> (DCDFM); tetra chloroethene (PCE), trichloroethene (TCE); and quantifiable concentrations of <br /> chloroform, carbon tetrachloride, and trichlorofluoromethane (TCFM). In a letter dated <br /> January 30, 2018, the RWQCB was notified of the CNSDAM exceedances in well MW-17. <br /> Quantifiable VOC constituents were place in "tracking mode" and are being evaluated quarterly <br /> for temporal trends (discussed below). <br /> Project No.5017.1030 I Water Quality Monitoring Report 6 <br /> January 2018 <br />
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