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ARCHIVED REPORTS_XR0012772
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3500 - Local Oversight Program
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PR0545246
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ARCHIVED REPORTS_XR0012772
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Last modified
1/30/2020 7:13:17 PM
Creation date
1/30/2020 3:41:13 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0012772
RECORD_ID
PR0545246
PE
3528
FACILITY_ID
FA0003611
FACILITY_NAME
PARKWOODS GAS & FOOD
STREET_NUMBER
1612
Direction
W
STREET_NAME
HAMMER
STREET_TYPE
LN
City
STOCKTON
Zip
95209
APN
07728002
CURRENT_STATUS
02
SITE_LOCATION
1612 W HAMMER LN
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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' Ms Diane Hinson <br /> - September 14, 1994 <br /> Page 4 <br /> ' ARCO No 760 <br /> The subsurface materials containing the majority of residual hydrocarbons beneath the ARCO <br /> ' Lodi site consist of laterally continuous units of sand/silty sand (fine- to coarse-grained sand)and <br /> silt with trace to little clay ranging in tluckness from 6 to 10 feet The silt units contain isolated <br /> ' sand and silty sand lenses Soil type of the upper portion of the aquifer (based on current <br /> groundwater elevation) has been clarified as fine- to coarse-grained sand Ranges of intrinsic <br /> permeabilities for sand and silty sand are approximately 10-3 to 107' cm/s and 10.5 to 10-3 cm/s, <br /> respectively (FetterC W Applied Hydrogeology, 1988 and Freeze and Cherry, Groundwater, <br /> 1979) Inic perrneabdities for slit range from 10' to 10'3 <br /> t nscm/s However, the presence of <br /> clay in the silt units will decrease the permeability, ranges of intrinsic permeabilities for clay are <br />' approximately 10-9 to 10-6 cm/s <br /> ARCO No 548 <br /> The subsurface materials containing the majority of residual hydrocarbons beneath the ARCO <br /> Stockton site consist predorrunantly of silt containing trace to some clay with laterally <br /> discontinuous beds and lenses of sandy silt The aquifer material consists primarily of silt with <br /> some clay Ranges of intrinsic permeabilitfes for silt and sandy silts are approximately 10-6 to <br /> 10' cm/s (Fetter, C W , Applied Hydrogeology, 1988 and Freeze and Cherry, Groundwater, <br />' 1979) The presence of clay in the soil will decrease the permeability <br /> PROXIMITY TO WATER SUPPLY WELLS <br /> A well survey is scheduled to be performed for the ARCO Lodi site during the next phase of <br /> work which includes further offsite assessment The results of the well survey will be included <br />' in the Problem Assessment Report (PAR) <br /> A well survey was previously conducted for the ARCO Stockton site to identify any municipal <br /> or domestic water supply wells within a 1/2 mile radius of the site The results of the survey <br /> were presented in the Preliminary Investigation and Evaluation Report, dated July 26, 1992 and <br /> also included in the Addendum to the PAR, dated August 16, 1994 Figure 11 presents the <br />' location of recorded water supply wells The nearest municipal well is approximately 1,000 feet <br /> to the south and the nearest domestic well is approximately 1,200 feet to the southeast <br />' RESULTS <br /> The estimated total mass of residual hydrocarbons beneath the ARCO Lodi site is approximately <br /> 489 lbs, where as the ARCO Stockton site contains a total mass estimated at approximately 383 <br /> lbs The groundwater flow direction does not appear to be consistent at the ARCO Lodi site, <br /> based on two quarters of monitoring The groundwater flow direction at the ARCO Stockton site <br /> I <br />
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