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ARCHIVED REPORTS XR0012946
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3500 - Local Oversight Program
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PR0544236
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ARCHIVED REPORTS XR0012946
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Entry Properties
Last modified
3/6/2019 8:13:27 PM
Creation date
3/6/2019 4:24:36 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012946
RECORD_ID
PR0544236
PE
3526
FACILITY_ID
FA0024238
FACILITY_NAME
JM EQUIPMENT COMPANY
STREET_NUMBER
1245
Direction
W
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95206
APN
16323034
CURRENT_STATUS
02
SITE_LOCATION
1245 W CHARTER WAY
P_LOCATION
01
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
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Cltologkal7eckafcslrrc Page 17 <br /> Revised Site Conceptual Model Report <br /> Project No.507.2 <br /> �.. April 3,2008 <br /> 4.0 DISCUSSION AND CONCLUSIONS <br /> 4.1 Discussion <br /> ' The data indicate that a localized plume of contamination persists in vicinity of wells MW-4, <br /> ... MW-5 and MW-9. Previous field investigations in this location utilizing a five foot sampling <br /> interval supported a conclusion that the site possessed predominantly very fine grained clayey <br /> soils. But the advancement of three 36 foot continuously cored borings in 2006 revealed that <br /> w more sandy units are present than previously thought. The above photographs confirm this <br /> situation. <br /> �. The data from borings SB-7 through SB-9 confirm that shallow soils at depths of 0— 12 feet <br /> are clayey. This material would tend to absorb gasoline emanating from piping or dispenser <br /> leaks presumed to be located in the alley south of the Hesston Shop UST excavation. The <br /> a gasoline entrained in the soil would slowly move downward until it encountered the water <br /> table with associated dissolving to source the groundwater plume. The gasoline in the <br /> shallow clay soils has probably not been significantly affected by natural biodegradation <br /> �- given that the buildings and cement road surface prevents infiltration and the water table has <br /> historically been at 13— 1 S feet bgs and as such below the clayey units. <br /> �- But the three borings also revealed that from 12—30 bgs the soils are mostly sands,including <br /> silty or clayey sands. This situation allows the dissolved gasoline contaminant mass to move <br /> with groundwater and attenuate with distance away from the release point as evidenced in <br /> well MW-6 located approximately 55 feet down gradient of well MW-9. <br /> Recent advancement of two shallow 30 ft GeoProbe borings indicate the presence of clay and <br /> �- sandy clay, with a shallow clayey sand unit approximately 20 ft below ground surface. <br /> �- 4.2 Conclusions <br /> Based on our interpretation of the data collected over the course of this subsurface <br /> ` investigation, GTI has reached several conclusions. These conclusions are based on the <br /> premise that the data considered, although incomplete, are representative of actual site <br /> conditions. We acknowledge that there may be undiscovered conditions, which would upon <br /> their consideration,change our interpretation and thus our conclusions. <br /> Geological Technics Inc. makes the following conclusions. <br /> • The shallow clayey soils from surface to 12 feet contain a significant amount of <br /> gasoline mass that has not been affected by natural biodegradation processes due to <br /> the cement road surface and low water table. <br /> �. • The contamination entrained in the shallow clays is sourcing a groundwater plume <br /> that is decaying very slowly. <br />
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