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ARCHIVED REPORTS_XR0006026
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3500 - Local Oversight Program
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PR0545640
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ARCHIVED REPORTS_XR0006026
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Last modified
5/5/2020 3:44:04 PM
Creation date
5/5/2020 1:55:59 PM
Metadata
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Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0006026
RECORD_ID
PR0545640
PE
3528
FACILITY_ID
FA0003900
FACILITY_NAME
PACIFIC PRIDE COMMERCIAL FUEL
STREET_NUMBER
2402
STREET_NAME
PACIFIC
STREET_TYPE
AVE
City
STOCKTON
Zip
95204
APN
12506001
CURRENT_STATUS
02
SITE_LOCATION
2402 PACIFIC AVE
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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dated 01 November 2000 <br /> • October 200.1 -AGE advanced three cone penetrometer testing(CPT) soil bonngs (CPT-1, <br /> CPT-2 and CPT-2A) at the site to maximum depths of 150 feet bsg to assess the vertical <br /> extent ofpetroleum-impact and identify potential hydrologic units Based on CPT data,AGE <br /> interpreted the CPT data to identify nine potential hydrogeologic units at depths between 25 <br /> feet and 150 feet bsg informally identified as Hydrologic Units 1 through 9 Analytical <br /> results of grab water samples detected TPH-g at depths as great as 140 feet bsg from CPT-1 <br /> and CPT-2A at concentrations as high as 840µg/1 and BTEX constituents as high as 120µg/1 <br /> xylenes Results of the October 2001 investigation were reported by AGE in Cone <br /> Penetrometer Testing Site Investigation -Fourth Quarter 2001, dated 19 February 2002 <br /> • October, November & December 2002 - Due to internal damage at well MW-13 (casing <br /> separation),one multi-level ground water monitoring well(MW-13A,B and C)was installed <br /> on-site to a maximum depth of 150 feet bsg to replace the damaged well, well MW-13 was <br /> tnple-completed utilizing Sollmst CMT, 1 7--inch diameter teflon casing screened at depths <br /> of 95-100 feet bsg, 120-125 feet bsg and 145-150 feet bsg Due to the severe heaving sands, <br /> no sampling activities were performed during drilling of replacement well MW-13 (A-C) <br /> Analytical results of the initial water sample detected TPH-g at a concentrations as ingh as <br /> 330 µg/1 and BTEX constituents as high as 38 µg/1 toluene Results of the <br /> October/November/December 2000 investigation were reported by AGE in Multi-Level <br /> Monitoring Well Installation Report - 4`4 Quarter 2002, dated 13 May 2003 <br /> • January 2003 - One ground water extraction well (EW-1) was installed on-site to a <br /> maximum depth of 65 feet bsg, well EW-1 was single-completed utilizing 6-mch diameter <br /> PVC casing screened 40-65 feet bsg Analytical results of soil samples detected TPH-g from <br /> EW-1 as deep as 50 feet bsg at concentrations as high as 3,300 mg/kg and BTEX constituents <br /> at concentrations as high as 440 mg/kg xylenes Results of the January 2003 investigation <br /> were reported by AGE in Ground Water Aquifer Pumping Test Report-July 2003, dated 04 <br /> February 2004 <br /> • July 2003 - Ground water aquifer pump testing was performed from EW-1 at the site to (1) <br /> obtain general ground water aquifer characteristics and (2) to evaluate aquifer response to <br /> ground water extraction The pump test results indicated a radius of influence fiom EW-1 <br /> at approximately 62 feet at 5 GPM, transmissivity was calculated at 565 ft /day(equivalent <br /> to 4,216 gallons per day/ft)and a storativity value calculated at 0 11,hydraulic conductivity <br /> was calculated at 22 6 ft/day,or 0 008 cm/s which is consistent with a silty sand to fine sand <br /> Analytical Results of grab water samples collected during the pump test detected TPH-g at <br /> concentrations as high as 71,000 µg/l and BTEX constituents as high as 13,000 µg/1 xylene <br /> Results of the January 2003 investigation were reported by AGE in Ground WntPr Aquifer <br /> Pumping Test Report -July 2003, dated 04 February 2004 <br /> Between Augustl996 and June 2004, thirty ground water monitoring events were performed at the <br /> site to monitor dissolved petroleum hydrocarbon concentrations in ground water and to characterize <br /> ground water flow direction and gradient on the site, ground water flow direction was consistently <br /> oriented toward the east-northeast at a gradierits between 0 002 and 0 005 Initially,the most intense <br /> APPENDIX A <br />
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