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ARCHIVED REPORTS XR0011743
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3500 - Local Oversight Program
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ARCHIVED REPORTS XR0011743
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Entry Properties
Last modified
11/19/2024 10:19:08 AM
Creation date
9/4/2019 10:58:29 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011743
RECORD_ID
PR0544801
PE
3528
FACILITY_ID
FA0003210
FACILITY_NAME
TEXACO TRUCK STOP
STREET_NUMBER
7500
Direction
W
STREET_NAME
ELEVENTH
STREET_TYPE
ST
City
TRACY
Zip
95378
APN
25015018
CURRENT_STATUS
02
SITE_LOCATION
7500 W ELEVENTH ST
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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Extended Site Characterization Report; 7500 West Eleventh Street, Tracy, CA. Page 46 <br /> Despite the limitation stated above, the estimates that have been made, when taken <br /> together with the calculated mean hydraulic conductivity of the formations through which <br /> components of hydrocarbon fuels have migrated, support the interpretation of the extent <br /> and geometry of the primary plume that is shown on Figures 13 through 16. <br /> 7.3.3 Secondary Plume <br /> Exploratory Boring PP-7, which was drilled during the first phase of site characterization <br /> in April of 2000, was Iocated, as shown on Figure 2, close to the southeast corner of the <br /> 4: former truck service bay, which is to the rear of the Casa Mendoza restaurant. PP-7 was <br /> also close to the end of Pipe Trench No. 2, which had contained a pipeline running from <br /> there in the direction of Tank Pits Nos. 1 and 2, the purpose of which could not be <br /> determined. However, Dietz Irrigation did report the presence of apparently-disturbed <br /> ground in that area when the pipeline was removed from Pipe Trench No. 2 in December <br /> 1998 (Dietz Irrigation 1999b). <br /> Boring PP-7 was also Iocated a short distance down gradient from the site of the two <br /> 1,000-gal, underground fuel storage tanks formerly located at 24195 Chrisman Road, <br /> 'y which, as shown on Figure 13, is the adjoining property to the south. <br /> Diesel, at a concentration of 25,200 µg/L and gasoline, at a concentration of 11,000 µg/L <br /> were detected in a sample of groundwater recovered from PP-7, which penetrated to a <br /> maximum depth of 16 ft BGS. The concentrations of gasoline and diesel detected in soil <br /> samples from that boring were also high. They were initially encountered near the surface <br /> and persisted to a depth of at least 16 ft. As is shown on Table 3, 3,800 mg/Kg of <br /> gasoline was detected in a sample of soil recovered from that boring at a depth of 4 ft <br /> _A beneath the ground surface. At 12 ft, the concentration of that analyte was Iower, at 280 <br /> : + mg/Kg. Although no gasoline was detected at 16 ft, diesel, at a concentration of 2.50 <br /> mg/Kg, was detected at that depth, with the concentrations of diesel at higher elevations <br /> =+ reaching 2,690 mg/Kg. <br /> Given the presence of those fuel hydrocarbons in samples recovered from near the <br /> ground surface as well as from greater depths in PP-7, it would appear that, at some time <br /> in the past, there was a primary source of fuel hydrocarbons located in that vicinity. <br /> While it is true that fuel hydrocarbons may have migrated to that area from the leaking <br /> underground fuel storage tanks that were located at 24195 Chrisman Road, given the fact <br /> that PP-7 is separated from that property by a retaining wall, to the south of which the <br /> ground surface is 4-ft. lower than the surface elevation at PP-7, the presence of moderate- <br /> to-high concentrations of fuel hydrocarbons in the shallow soils in PP-7 indicates that <br /> -� there was separate source of leakage in the vicinity of that boring. <br /> Consideration of the overall distribution of components of fuel hydrocarbons in samples <br /> of soil and groundwater recovered from other borings in the general area around PP-7 <br /> indicates that there is a secondary plume of diesel and gasoline emanating from that <br /> vicinity. It affects the subsurface to a depth of some 20 ft beneath that area and has <br /> = migrated down the groundwater gradient to commingle with the primary plume of <br /> "1 <br /> sic <br />
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