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ARCHIVED REPORTS_2006_1
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ARCHIVED REPORTS_2006_1
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Last modified
7/17/2020 3:53:23 PM
Creation date
7/3/2020 10:50:58 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2006_1
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
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4433_PR0440005_9999 AUSTIN_2006_1.tif
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EHD - Public
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The groundwater elevation data obtained during second quarter 2006 monitoring period <br /> were used to generate the groundwater elevation contour map shown on Figure 2-1, <br /> which indicates that groundwater at the site generally flows to the west and north at an <br /> average hydraulic gradient of approximately 0.001 to 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). The estimated maximum groundwater flow velocity was calculated using Darcy's <br /> Law: <br /> Ki cm * 0.003 *2835 sec– ft 0.972 /da <br /> V = —= [(0.04 cm ] ft y <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 z 0.003 for the site during the second quarter 2006. <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 second quarter <br /> 2006 are summarized in Table 2-2 and Appendix D presents time-series charts of select <br /> inorganic parameters. As shown on Table 2-2, one or more trace level VOCs were <br /> measured in the samples collected from wells MW-1B,MW-10,MW-14,MW-15, <br /> MW-16,MW-17,MW-19, MW-21, and DW-9690,while concentrations of <br /> tetrachloroethene(PCE) and trichloroethene(TCE)in well MW-1B and acetone in well <br /> DW-9690 were measured above the practical quantitation limit(PQL). On behalf of <br /> Forward Inc., GLA prepared a letter report dated February 14, 2001 (RWQCB Case No. <br /> 2209),to assess the source and potential impacts of low-level VOCs in groundwater <br /> adjacent to the Forward Landfill. The letter report concluded that the sporadic detection <br /> of low-level VOCs in groundwater and lysimeter samples at the Forward Landfill are <br /> most likely due to landfill gas from unlined unit WW-B. Forward has continued to <br /> minimize gas related impacts to groundwater by minimizing interim fill areas that <br /> promote ponding of water. Furthermore, in accordance with CCR Title 27, Section <br /> 20937,Forward continues to install additional landfill gas extraction wells. <br /> New Historical Intrawell Maximum Values <br /> As shown in the following table,the results of the second quarter 2006 monitoring period <br /> indicate that 16 new historical intrawell maximum values were measured, including <br /> seven first-time VOC detections, in samples collected from groundwater monitoring <br /> wells. <br /> D:\2003_021\ForwsrdAusdn_sp06.doc <br /> 6 GeoLogic Associates <br />
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