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ARCHIVED REPORTS XR0003384
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0544596
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ARCHIVED REPORTS XR0003384
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Last modified
6/24/2019 2:44:30 PM
Creation date
6/24/2019 1:43:54 PM
Metadata
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Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0003384
RECORD_ID
PR0544596
PE
3528
FACILITY_ID
FA0002064
FACILITY_NAME
7-ELEVEN INC. STORE #14117
STREET_NUMBER
2725
STREET_NAME
COUNTRY CLUB
STREET_TYPE
BLVD
City
STOCKTON
Zip
95204
CURRENT_STATUS
02
SITE_LOCATION
2725 COUNTRY CLUB BLVD
P_LOCATION
01
P_DISTRICT
003
QC Status
Approved
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EHD - Public
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REPORT ON ADDITIONAL SITE ASSESSMENT AND RECOMMENDATIONS 5 <br /> 7-Eleven Store No 14117 2725 Country Club Blvd Stockton CA December 12,2001 <br /> 40 RESULTS <br /> ' <br /> 41 Geology and Hydrogeology <br /> The site is located in the northern part of the San Joaquin Valley at an elevation of approximately <br /> one foot above sea level Shallow stratigraphy In the area consists of Quaternary alluvial/deltaic <br /> ' deposits The sand units are generally fresh-water-bearing east and southeast of Stockton, but <br /> brackish or saline water is present In these strata In the delta area west of Stockton (California <br /> ' Department of Water Resources, 1967, Bulletin No 146) The saline water/fresh-water boundary <br /> trends north to south across the western part of Stockton The brackish/saline water west of this <br /> boundary is often overlain by a layer of fresh groundwater to about 50 feet below grade, therefore, <br /> ' shallower groundwater monitoring wells may encounter fresh groundwater on both sides of the <br /> boundary <br /> ' Sod types encountered during drilling generally consist of Interbedded clayey fine sand, silty clay <br /> and clayey silt, with a laterally-continuous silty/very fine sand layer at about 18 feet to total depth <br /> (about 20 feet below grade) In the previously drilled deeper boring MW-2 silty sand was <br /> encountered from 18 to 28 feet and fine to medium sand from 38 feet to total depths of 51 feet <br /> below grade During drilling, groundwater was encountered at about 10 feet below grade, <br /> equilibrating at similar depths (Table 1) <br /> The groundwater flow on November 5, 2001, was southerly at a hydraulic gradient of about 0 006 <br /> foot per foot (Table 2, Figure 2) Historically(based on data collected over the last two years), the <br /> ' gradient fluctuates between south to northwest The shallow groundwater and proximity of some of <br /> the monitoring wells to the former and current underground storage tank pits are probably <br /> ' responsible for local perturbations and fluctuations in groundwater flow direction which may not <br /> reflect regional flow direction <br /> rA formal 2,000-foot sensitive receptor investigation (to identify all municipal and/or domestic wells in <br /> the area) has not been conducted for this site <br /> ' <br /> 42 Results of Soil Sample Analyses <br /> Recent sod analytical data (Table 2) indicate the lateral extent of TPH-G, BTEX, MTBE, and other <br /> oxygenates has been delineated by non-detectable levels (except for 0 006 mg/kg total xylenes In <br /> well MW-7)to the west, northwest, and south of the known plume area Historical data are included <br /> in Table 2A <br /> Copies of the analytical results and chain-of-custody documents are included In Appendix D <br />
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