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ARCHIVED REPORTS_XR0004587
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ARCHIVED REPORTS_XR0004587
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Last modified
3/5/2020 1:14:26 PM
Creation date
3/5/2020 11:52:22 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004587
RECORD_ID
PR0507835
PE
2950
FACILITY_ID
FA0007793
FACILITY_NAME
SUPER STOP MARKET
STREET_NUMBER
290
Direction
N
STREET_NAME
MAIN
STREET_TYPE
ST
City
MANTECA
Zip
95336
APN
22309101
CURRENT_STATUS
02
SITE_LOCATION
290 N MAIN ST
P_LOCATION
04
P_DISTRICT
003
QC Status
Approved
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EHD - Public
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Geological Teclutics Inc Page 2 <br /> Groundwater Monitoring Report <br /> Project No 662 2 <br /> November 15,2004 <br /> ' on October 26 - 27, 2004 with the installation of one extraction well and two monitoring <br /> wells The performance of a dual phase extraction/aquifer pumping test is scheduled for <br /> ' December 6— 10, 2004 <br /> 1.0 GROUNDWATER MONITORING <br /> ' 1.1 H dro eolo of Site <br /> Y g gY <br /> ' The dominant soil type in the upper 40 feet of the subsurface geologic soils investigated is <br /> sand, fine to course grained, interbedded with thinner units of plastic clay The average <br /> groundwater elevation on August 18, 2004 was approximately 9 06 feet above MSL, which is <br /> ' about 31 feet below ground surface This represents a decrease of 2 37 feet since the June <br /> 2004 monitoring event, and a cumulative decrease of 4 54 feet since the February 2004 <br /> ' monitoring event <br /> A groundwater gradient was calculated for the event and the groundwater was found to flow <br /> ' N89°E at 0 001 ft/ft Groundwater elevation and gradient data are summarized in Table 1, <br /> Appendix A Gradient direction is shown on Figure 2 Gradient Map, and Figure 3 <br /> Groundwater Gradient Rose Diagram <br /> 1.2 Groundwater Sampling Procedure <br /> ' On August 18, 2004, Don Light of Del-Tech mobilized to the site to conduct groundwater <br /> monitoring of the four monitoring wells on site <br /> ' Before sampling was performed the wells were sounded for depth to water The wells were <br /> purged of at least three well volumes of stagnant water using a dedicated Waterra check-ball <br /> assembly and i/2 inch tubing Purging continued until the temperature, conductivity, and pH <br /> ' of the groundwater stabilized (<10% variation between three readings) indicating that <br /> formation water representative of aquifer conditions was entering the wells These water <br /> quality parameters were measured at intervals of each well volume purged <br /> ' Once purging was complete, a water sample was collected from the Waterra tube Care was <br /> taken to minimize sample agitation Once the sample container was filled and capped, the <br /> ' bottle was inverted, tapped, and checked for headspace bubbles The sample container was <br /> identified and labeled with a unique designation, inserted into foam holders and placed in an <br /> ice chest cooled to 4°C for transport to the laboratory <br /> A P sampling All non-disposable equipment was decontaminated using a hot water washer and <br /> P g g ui P <br /> detergent before and between uses Disposable gloves were used by the technician to collect <br /> ' all samples and were changed with each sample collection <br />
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