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ARCHIVED REPORTS XR0011111
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ARCHIVED REPORTS XR0011111
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Last modified
9/5/2019 8:58:44 AM
Creation date
9/5/2019 8:38:17 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011111
RECORD_ID
PR0544806
PE
3528
FACILITY_ID
FA0000293
FACILITY_NAME
Pershing Holdings, Inc. DBA Esclon Arco
STREET_NUMBER
1329
STREET_NAME
ESCALON
STREET_TYPE
Ave
City
Escalon
Zip
95320
APN
22510003
CURRENT_STATUS
02
SITE_LOCATION
1329 Escalon Ave
P_LOCATION
06
P_DISTRICT
004
QC Status
Approved
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Geofogica(Technics Inc. <br /> Page 2 <br /> Groundwater Monitoring Report <br /> Project No. 750.2 <br /> August 24,2000 <br /> The average groundwater elevation on July 14 was about 56.45 feet above MSL, which is <br /> approximately 61.65 feet below ground surface. <br /> A groundwater gradient was calculated for the event and groundwater was flowing N720W at <br /> 0.0024 ft/ft. Data is summarized in Table 1, Appendix A. Gradient directions are shown on <br /> Figure 3: Gradient Map. The three monitoring events for grouondwater gradient shows that <br /> the gradient slope and direction are similar. <br /> 1.2 Groundwater Sampling Procedure <br /> On July 14, 2000 Don Light of Del-Tech mobilized to the site to develop the monitoring <br /> wells and conduct a groundwater monitoring event. The wells were installed April, June and <br /> July of 1999 but were finished off below grade so that road and sidewalk construction could <br /> take place. In early April of 2000 the wells were relocated and finished to ground surface. <br /> Before development'was attempted, the wells were sounded for depth to water. Since the <br /> wells had never been developed after installation, Don Light first developed the wells by <br /> surging and pumping them until a clear stream of water was obtained. Once all of the wells <br /> had been developed, Mr. Light returned to the first well that had been developed and began <br /> &Wr%or the following sampling process: <br /> • The wells were purged of at least three well volumes of stagnant water using a dedicated <br /> 4.4 Waterra pump. Purging continued until the temperature, conductivity, and pH of the <br /> groundwater stabilized (<10% variation between three readings) indicating that formation <br /> 9.9 water representative of aquifer conditions was entering the well. These water duality <br /> parameters were measured at intervals of each well volume purged. <br /> • A stainless steel bailer was used to collect each sample. Care was taken to minimize <br /> 6.0 sample agitation from the initial filling of the bailer to the transfer of the sample to the <br /> VOA vials. <br /> • Once the sample containers were filled and capped, the bottles were inverted, tapped, and <br /> checked for headspace bubbles. Each sample container was identified and labeled with a <br /> unique designation, inserted into foam holders and placed in an ice chest cooled to 4°C <br /> for transport to the laboratory. <br /> La • All non-disposable sampling equipment was decontaminated using a steam cleaner before <br /> and between uses. Disposable gloves were used by the technician to collect all samples <br /> and were changed with each sampling event. <br /> A field blank (prepared from water provided by the laboratory poured into a VOA vial on <br /> site) accompanied the samples to the laboratory to serve as checks against cross <br /> V <br /> contamination. <br /> %.. <br /> 4 <br /> 4 <br />
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