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ARCHIVED REPORTS XR0011739
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0544801
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ARCHIVED REPORTS XR0011739
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Last modified
11/19/2024 10:19:08 AM
Creation date
9/4/2019 10:56:57 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011739
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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---------------- <br /> Site Characterization Report: 7500 West Eleventh Street, Tracy, CA. Page 30 <br /> whether fuel hydrocarbons that leaked from those tanks migrated northward to affect soil <br /> beneath the 7500 West Eleventh Street property. This uncertainty is due, in part, to the <br /> presence of what appears to be a secondary plume of diesel and gasoline that originated <br /> on the 7500 West Eleventh Street site in the vicinity of boring PP-7. (See Figure 13 for <br /> _1 <br /> location.) <br /> 5.5.2 Secondary Plume of Diesel and Gasoline <br /> As noted previously, push-probe boring PP-7 was located close to the southeast corner of <br /> the former truck service bay, which is to the rear of the'Casa Mendoza restaurant. PP-7 <br /> was also close to the end of Pipe Trench No. 2, which had contained a pipeline running <br /> from 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 /> ji 1998. <br /> Boring PP-7 was also located a short distance down gradient from the previously- <br /> described site of the two 1,000-gal. underground fuel storage tanks formerly located at <br /> 24195 Chrisman Road, which is, as shown on Figure 13, the adjoining property to the <br /> south. <br /> Diesel, at a concentration of 25,200 pg/L and gasoline, at a concentration of 11,000 µg/L <br /> were detected in a sample of groundwater recovered from PP-7. The concentrations of <br /> t = gasoline and diesel detected in soil samples from this boring were also high. They were <br /> initially encountered near the surface and persisted to a depth of at least 16 ft. As is <br /> ..� shown on Table 1, 3,800 mg/Kg of gasoline was detected in a sample of soil recovered <br /> from that boring at a depth of 4 ft beneath the ground surface. At 12 ft, the concentration <br /> of that analyte was lower, at 280 mg/Kg. Although no gasoline was detected at 16 ft, <br /> r diesel, at a concentration of 2.50 mg/Kg, was detected at that depth, with the <br /> .1� concentrations of diesel at higher elevations reaching 2,690 mg/Kg. <br /> Given the persistence of those fuels in samples recovered from near the ground surface as <br /> well as from greater depths in PP-7, it would appear that, at some time in the past, there <br /> was a primary source of fuel hydrocarbons located in that vicinity. While it is true that <br /> fuel hydrocarbons may have migrated to that area from the leaking underground fuel <br /> storage tanks that were located at 24195 Chrisman Road, given the fact that PP-7 is <br /> separated from that property by a retaining wall, to the south of which the ground surface <br /> is 4-ft. lower than the surface elevation at PP-7, the presence of moderate- to-high <br /> concentrations of fuel hydrocarbons in the shallow soils in PP-7 indicates that there was <br /> separate source of leakage in the vicinity of that boring. <br /> ' 1 <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 /> supports the interpretation shown on Section A-A' that there is a secondary plume of <br /> diesel and gasoline emanating from that vicinity. It affects the subsurface to a depth of <br /> some 20 ft beneath that area and has migrated down the groundwater gradient to <br /> sic <br />
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