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ARCHIVED REPORTS_XR0008410
Environmental Health - Public
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3500 - Local Oversight Program
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PR0545864
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ARCHIVED REPORTS_XR0008410
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Last modified
7/21/2020 9:59:17 AM
Creation date
7/21/2020 9:45:46 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0008410
RECORD_ID
PR0545864
PE
3528
FACILITY_ID
FA0004530
FACILITY_NAME
MARLOWE PROPERTY
STREET_NUMBER
4648
STREET_NAME
WATERLOO
STREET_TYPE
RD
City
STOCKTON
Zip
95215
CURRENT_STATUS
02
SITE_LOCATION
4648 WATERLOO RD
P_LOCATION
99
P_DISTRICT
002
QC Status
Approved
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Quarterly Report - September 1997 <br /> MARLOWE PROPERTY <br />' 4648 East Waterloo Road, Stockton, California <br /> 1.0. INTRODUCTION AND SCOPE OF WORK <br /> In accordance with a request from Ms Jonathan Marlowe of Marlowe Properties, Advanced <br /> GeoEnvironmental, Inc (AGE) has prepared this Quarterly Report for 4648 East Waterloo Road, <br /> Stockton, California The location of the site and its surroundings are illustrated in Figure 1 - <br /> Location Map Structures and monitoring wells on the site are illustrated in Figure 2 - Site Plan <br /> The scope of work was to monitor dissolved petroleum hydrocarbon concentrations in ground water <br /> and to characterize ground water flow direction and gradient on the site This report is prepared in <br /> accordance with guidelines established by the San Joaquin County Public Health Services - <br /> Environrnental Health Division (PHS-EHD) and the Central Valley Regional Water Quality Control <br /> Board (CVRWQCB) for investigation of underground storage tank (UST) sites <br /> Background information and a description of prior investigations at the site has been included in the <br /> Quarterly Report -April 1996, dated 12 June 1996, prepared by AGE Up-to-date ground water <br /> monitoring results are included in this report <br /> 20 PROCEDURES <br /> 2 1 MONITORING WELL PURGE PROCEDURES <br /> I On 26 September 1997, the depth to ground water In monitoring wells MW-1 through MW-6 and <br /> VW-1 were measured to the nearest 0 01 foot utilizing a Solinst water Ievel meter Relative ground <br /> water elevations were calculated for each well by subtracting the depth to ground water from the <br />' relative casing elevation of each well, surveyed from a temporary benchmark assigned an arbitrary <br /> elevation (Table 1- Relative Ground Water Elevations) Relative ground water elevations were <br /> plotted and contoured on a scaled site map (Figure 3-Relative G ound Water Elevation Map) <br />' After water levels were measured, Ms Mary Meays of the PHS-EHD reviewed the ground water <br /> monitoring data and recommended that only wells MW-1, MW-5, MW-6 and VW-1 be sampled <br />' during this monitoring event Subsequently, a minimum of three well volumes (approximately 8 to <br /> 12 gallons) of ground water was purged from monitoring wells MWA, MW-5, MW-6 and VW-I <br /> using a disposable bailer and new nylon rope <br />' Temperature, pH and conductivity were measured at regular intervals from each well using an ICM <br /> Model 52200 water analyzer Stabilization data and field logs are contained in Appendix A Purged <br />' ground water was stored in labeled, 55-gallon drums on-site in an area lacking public access <br /> • <br />' Adi anted GeoEmlronmental,Inc <br />
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