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ARCHIVED REPORTS_XR0002784
EnvironmentalHealth
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3500 - Local Oversight Program
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PR0545262
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ARCHIVED REPORTS_XR0002784
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Last modified
2/3/2020 7:59:18 PM
Creation date
2/3/2020 10:17:00 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0002784
RECORD_ID
PR0545262
PE
3528
FACILITY_ID
FA0009940
FACILITY_NAME
SAN JOAQUIN CATHOLIC CEMETERY
STREET_NUMBER
719
Direction
E
STREET_NAME
HARDING
STREET_TYPE
WAY
City
STOCKTON
Zip
95204
APN
12720002
CURRENT_STATUS
02
SITE_LOCATION
719 E HARDING WAY
P_DISTRICT
001
QC Status
Approved
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SJGOV\sballwahn
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EHD - Public
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. 2.0 GROUNDWATER MONITORING, SAMPLING AND ANALYSIS <br /> On February 12, 1998, Ramage Environmental monitored and sampled groundwater at the site <br /> 21 Groundwater Monitoring <br /> were taken in all five groundwater monitoring wells except <br /> Depth-to-groundwater measurements <br /> MW-1 and the two deep soil vapor extraction wells (VW-1 and VW-2) to evaluate groundwater <br /> ' flow and gradient characteristics Monitoring Well MW-1 was inaccessible due to flooding The <br /> depth-to-groundwater beneath the site ranged from 44 72 feet below ground surface (bgs) in <br /> MW-4 to 45 56 feet bgs in MW-5 The groundwater elevation beneath the site ranged from <br /> 27 53 feet below mean sea level (MSL) in MW-4 to 27 35 feet below MSL in MW-3 <br /> Groundwater levels have risen an average of 3 52 feet since groundwater levels were last <br /> measured on November 13, 1997 In the past year, groundwater levels have risen an average <br /> of 1 35 feet Since May 1992, the groundwater levels have risen 21 84 feet The historical <br /> groundwater monitoring data are summarized in Table 1 <br /> The groundwater flow direction and gradient are illustrated on the groundwater surface map <br /> (Figure 3) In general, the groundwater gradient was calculated at 0 0021 footifoot in a north- <br /> northeast direction Because groundwater levels in the five groundwater wells are above the <br /> screened interval, the calculated flow and gradient characteristics may be unreliable The <br /> groundwater flow and gradient calculations do not utilize groundwater levels in the sod vapor <br /> extraction wells because their wellhead elevations have not been surveyed <br /> 22 Groundwater Sampling and Analysis <br /> Groundwater from the deep sod vapor extraction wells (VW-1 and VW-2) was sampled to <br /> evaluate the concentration of gasoline hydrocarbons at the groundwater table The groundwater <br /> monitoring wells (MW-1, MW-2, MW-3, MW-4 and MW-5) were not sampled because of <br /> groundwater levels significantly above the screened interval of these wells <br /> The deep soil vapor extraction wells (VW-1 and VW-2) were purged of at least three well <br /> volumes using a decontaminated bailer Following purging, groundwater samples were <br /> collected from the two wells using a disposable sampling bailer The groundwater samples were <br /> contained in laboratory-supplied glassware, labeled, sealed in a plastic bag and packed in an <br /> 2 <br />
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