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ARCHIVED REPORTS XR0006103
EnvironmentalHealth
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2900 - Site Mitigation Program
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PR0542421
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ARCHIVED REPORTS XR0006103
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Last modified
6/21/2019 12:38:45 PM
Creation date
6/21/2019 10:30:49 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0006103
RECORD_ID
PR0542421
PE
2950
FACILITY_ID
FA0024377
FACILITY_NAME
COUNTRY CLUB BLVD/295950
STREET_NUMBER
1876
STREET_NAME
COUNTRY CLUB
STREET_TYPE
BLVD
City
STOCKTON
Zip
95204
APN
12319101
CURRENT_STATUS
01
SITE_LOCATION
1876 COUNTRY CLUB BLVD
P_LOCATION
01
QC Status
Approved
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EHD - Public
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• 0 <br /> The property owner has installed five monitoring wells in the course of investigating the sol] and <br /> groundwater conditions at the site <br /> Table 1 is a tabulation of groundwater monitoring results <br /> Table 2 is a tabulation of soil sample results <br /> Geology and Hydrogeology of the Site <br /> The site is located on surface soils belonging to the Stockton Adobe Clay and Honeycut Clay <br /> series They are derived from recent alluvial fan and floodplain deposits The 40 feet of explored <br /> section consisted of clay and silt overlying interbedded lenses of silty and clayey sands below 20 <br /> feet <br /> The groundwater in the vicinity of the site is assumed to be semiconfined Groundwater elevation <br /> at the site varies from a wet year high of 7 feet bgs to about 35-40 feet bgs during the previous <br /> drought period Groundwater flow direction at the site has generally been to the west since <br /> December 1997 Two water bearing sands have been delineated with the most recent well <br /> installations, April 9 and 10, 2001 <br /> This first sandy formation has been designated the A zone aquifer The base of the A zone is at <br /> approximately 17 - 18 feet below ground surface {bgs} An aquitard consisting of silty clay <br /> approximately 3 to 4 feet thick separates the silty clayey sand A zone aquifer from the B zone <br /> aquifer that is found at approximately 21 feet bgs and is approximately 6 to 7 feet thick The <br /> second sandy formation (B zone aquifer) consists of cleaner moderately sorted fine to coarse sand <br /> that shows graded bedding (fine to coarse with depth) Beneath the B zone aquifer is stiff clay that <br /> extends from approximately 27 feet bgs to 40 feet bgs The original five monitor wells did not <br /> encounter groundwater in the A zone aquifer when initially drilled and sampled Depth to water <br /> measurements taken between 1993 and February 1996 indicate that the A zone aquifer was dry <br /> (depth to water greater than 17 feet bgs) MW 1 through MW5 are screened across both the A and <br /> B zone aquifers Sometime after February 1996 depth to groundwater measurements indicated that <br /> groundwater was in contact with the A zone aquifer <br /> Groundwater flow direction in the A zone at the site has generally been to the west since December <br /> 1997 The B zone shows a similar flow direction, which would be expected due to the connection <br /> between zones at wells MW1 through MW5 <br /> Overview of Workplan <br /> The November 27, 2000 workplan is designed to remove soils contaminated with gasoline range <br /> hydrocarbons while in the process of installing an air sparging/vapor extraction trench The <br /> removal of the contaminated soils will expedite the remediation objectives for this site To perform <br /> the over-excavation it will be necessary to dewater the area to be excavated to approximately the <br /> 19-20 foot depth An aquifer test will be performed prior to dewatering, to evaluate the storativity <br /> and transmissivity for both the A and B zone aquifers Monitor wells MW 1, MW2 and MW3 <br /> would interfere with the evaluation of the aquifer test and would most likely make dewatering the <br /> A zone excavation area nearly impossible by acting as conduits to the estimated high transmissivity <br /> B zone Once the dewatering and over-excavation work has been accomplished the site will be <br /> 2 Sanchez Well Dest 1-10-02 <br />
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