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SITE INFORMATION AND CORRESPONDENCE_1985-1997
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PR0522692
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SITE INFORMATION AND CORRESPONDENCE_1985-1997
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Last modified
4/2/2020 2:47:19 PM
Creation date
4/2/2020 2:16:02 PM
Metadata
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EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
SITE INFORMATION AND CORRESPONDENCE
FileName_PostFix
1985-1997
RECORD_ID
PR0522692
PE
2957
FACILITY_ID
FA0015465
FACILITY_NAME
FORMER MONTGOMERY WARDS AUTO SRV CTR
STREET_NUMBER
5400
STREET_NAME
PACIFIC
STREET_TYPE
AVE
City
STOCKTON
Zip
95207
APN
10227008
CURRENT_STATUS
01
SITE_LOCATION
5400 PACIFIC AVE
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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5 feet below ground surf ee.The screens were installed <br /> adjacent to each other, perpendicular to the direction hw a11i <br /> of flow. As shown in Figure 1, the field site consisted .Ew-t <br /> 1 Z] 4 <br /> of lines of monitoring points or wells oriented along the <br /> natural ground water flow direction. Samples were col- <br /> lected + 9+ -upgradient and downgradient of the oxygen RKGD + o+ • Oct ORC-CONCRETE LINE <br /> source within each line (briquet or pure powder). Two + ++ • AL AQUIFER LINE <br /> lines were used as controls to determine the benzene + • PL PENCIL LINE <br /> and toluene degradation behavior at the site in the <br /> absence of ORC. P•n<il. .EW-2 <br /> The experiment was designed to be interpreted after +.onif.,wg P.mt <br /> ...ming ..II <br /> steady-state concentration distributions were achieved . ..11 0.0 10 tm) <br /> or approached,i.e.,similar to the methods typically used oto• ..II .<r..n <br /> to interpret laboratory column tests of transformation <br /> reactions. Thus, a significant difference between the Figure 1. Site plan and monitoring locations. <br /> steady-state distributions for benzene and toluene <br /> downgradient of an ORC source and that downgradient <br /> of the comparable position in the control line could be <br /> taken as evidence of enhancement of transformation of <br /> the two compounds by the ORC source. This simple OCL-1 OCL- OCL-3 OCL-A <br /> comparative approach assumes that other solute trans- 0.0 <br /> port processes are similar along the flowpaths to be I Ii <br /> compared (advection, dispersion, and sorption), an <br /> assumption that seems warranted in the relatively homo- <br /> geneous Borden Aquifer.Since sorption and retardation <br /> V. <br /> of benzene and toluene are known to be slight in the 10 o„n <br /> Borden Aquifer (Barker et al. 1987), it was expected <br /> that the primary limit to the approach to steady state <br /> would be the acclimation of the native microorganisms <br /> to the injected substrates. <br /> Background samples were collected from a drive a.a <br /> point sampler located approximately 4 m upgradient of <br /> the source wells. The transport of the organic solutes 0.0 0.5 1.0 1.5 2.01m1 <br /> was monitored along lines of monitoring points('/4-inch <br /> stainless steel sampling points with a 1-inch screen) and Figure 2. Cross section of the site along the ORC-Concrete <br /> drive points (1-foot stainless steel screens) placed Line. <br /> approximately 4 feet below the ground surface. <br /> As stated previously, the lines of monitoring points and those prepared with cement only (concre <br /> and wells were oriented along the expected natural- briquets). The ORC-concrete briquets containe <br /> gradient flow direction. However, to minimize effects approximately 20 percent by weight ORC powder. Tl <br /> of temporal variations in the gradient due to snowmelt briquets were placed in two well screens installed in <br /> and other localized factors, two parallel lines of sheet- manner similar to that used for the source wells. Tl <br /> piling were driven 5 feet into the ground on both sides well screen in the Concrete Line contained concre <br /> of the field setup. As an additional method to maintain- briquets.Its purpose was to serve as a reference for tl <br /> a constant flow direction,two extraction wells were used ORC-Concrete Line, within which the well screen w- <br /> to extract ground water at approximately 1.5 gallons per filled with CIRC-concrete briquets. Figure 2 shows <br /> minute (gpm) each; the extraction rate and well Iota- cross section of the site along the ORC-Concrete Lir <br /> tions were selected based on 2-D modeling results. <br /> Water table elevation data were not collected during Pencil Section <br /> the experiment. Given the very small average regional <br /> gradient (0.0043), the low pumping rate (1.5 gpm per In one section gr the site, rows of app "pencil <br /> extraction well), and the short distance between moni- were placed in the ground, st a depth of approximate <br /> in <br /> toring points (approximately 40 to 50 cm along a moni- s feet. The pencils were installed by driving a ]r sa <br /> toring line), the absolute value of the head differences steel casing into the ground,jetting out the interior sat <br /> between the available monitoring points would have with water, and pouring 350 mL of an approximate <br /> been on the order of,or smaller than,the error inherent 60 percent vol/vol ORC water slurry into the emp <br /> in the head measurements. casing. The casing was then removed using a jack, aI <br /> another 150 mL of ORC slurry were added to fill t <br /> Briquet Section hole. As shown in Figure 1, pencils were installed <br /> Two types of briquets were used: those prepared rows perpendicular to the direction of flow. Each pen <br /> with cement mixed with ORC(ORC-concrete briquets), was approximately 6 inches away from the nearest pen <br /> 122 is WINTER 1994 GWMR <br />
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