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ARCHIVED REPORTS_XR0006625
Environmental Health - Public
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EHD Program Facility Records by Street Name
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YOSEMITE
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1012
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3500 - Local Oversight Program
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PR0545948
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ARCHIVED REPORTS_XR0006625
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Last modified
9/29/2020 10:29:30 PM
Creation date
8/5/2020 4:02:57 PM
Metadata
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Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0006625
RECORD_ID
PR0545948
PE
3528
FACILITY_ID
FA0005159
FACILITY_NAME
FILL-EM FAST
STREET_NUMBER
1012
Direction
W
STREET_NAME
YOSEMITE
STREET_TYPE
AVE
City
MANTECA
Zip
95336
APN
21903024
CURRENT_STATUS
02
SITE_LOCATION
1012 W YOSEMITE AVE
P_LOCATION
04
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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' submitted and analyzed for the above referenced tests. <br /> Laboratory analyses by the above methods detected no petroleum <br /> ' hydrocarbon constituents in the water sample collected from MW-6 <br /> or the trip blank (MW-7) . The water sample taken from monitoring <br /> well MW--4 was nondetectable for all hydrocarbon constituents <br /> except for a concentration of 0. 66 ppb ethylbenzene. The water <br /> sample from well MW-5 detected concentrations of TPHG and BTEX at <br /> concentrations of 860 ppb, 18 ppb, 4 . 1 ppb, 6. 1 ppb, and 120 ppb, <br /> ' respectively. Certified analytical data sheets and chain-or- <br /> custody documentation are included in Appendix C and the results <br /> of chemical analyses are summarized in Table 2 . <br /> 4 . 0 FINDINGS <br /> 4 . 1 Groundwater Hydraulic Gradient <br /> The groundwater hydraulic gradient was evaluated by triangulation <br /> of stabilized depth to water in monitoring wells MW--4, MW-5, and <br /> MW-6. The data collected from all 3 wells assumes that all wells <br /> are constructed within the same aquifer. TPE believes that all 3 <br /> well are hydraulically interconnected. Elevations of the <br /> groundwater are shown in Table 3 . Groundwater levels, measured <br /> on July 1, 1992, ranged from 9 . 30 to 9 . 10 feet MSL. The <br /> ' Groundwater Hydraulic Gradient Map (Figure 3) shows that <br /> groundwater beneath the site flows toward the north with a <br /> gradient of approximately 0. 002 ft/ft. <br /> 1 <br /> 5. 0 SUMMARY OF FINDINGS <br /> Groundwater beneath the site is estimated to flow in a <br /> northerly direction with a gradient of 0. 002 ft/ft. <br /> CGI measurements made during the field screening of <br /> ' soil samples detected only background (< 5 ppm) levels <br /> at monitoring wells MW-4 and MW-6. Monitorng well MW-5 <br /> GCI readings ranged from background to a high of 45 ppm <br /> at 20. 5 feet below grade. <br /> Soil samples located at the vadose zone / groundwater <br /> interface and showing the presence of hydrocarbons were <br /> ' selected for TPHG and BTEX laboratory analysis. In <br /> addition, the soil sample showing the highest GCI <br /> reading was analyzed for total lead. <br /> ' TPHG was not present at concentrations above analytical <br /> detection limits in any of the soil samples tested <br /> ' except for a sample taken at 20. 5 feet from MW-6. Some <br /> petroleum constituents were detected in bor1ng° MW=5' <br /> I I I soil samples, taken Gat 1 16 and 20. 5 feet below grade', and <br /> a sample taken at 20 . 5 feet from boring MW-6,. <br /> I I r r I r E 1 r <br /> ' ' e <br /> 7 <br /> I I � <br />
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