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ARCHIVED REPORTS_XR0004400
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PR0545486
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ARCHIVED REPORTS_XR0004400
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Last modified
3/10/2020 5:03:34 PM
Creation date
3/10/2020 2:59:54 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0004400
RECORD_ID
PR0545486
PE
3528
FACILITY_ID
FA0005611
FACILITY_NAME
ROYAL OAKS SAVINGS
STREET_NUMBER
510
Direction
N
STREET_NAME
MAIN
STREET_TYPE
ST
City
MANTECA
Zip
95336
CURRENT_STATUS
02
SITE_LOCATION
510 N MAIN ST
P_LOCATION
04
P_DISTRICT
003
QC Status
Approved
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SJGOV\sballwahn
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EHD - Public
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' Royal Oak Savings & Loan <br /> Page 4 <br /> SIO N. Main Street, Manteca, Camornia <br />' Quarterly Ground Nater Sampling Report <br /> October, 1992 -January, 1993 <br /> Ground Water Gradient <br />' Ground water level measurements were camed out monthly during the quarter on October <br /> 24, November 24, and December 28, 1992, as well as during the the sampling event on <br /> January 27, 1993 The vapor extraction system installed on MW-2 prevented level <br />' measurements from this well during November and December The ground water <br /> elevation measurements are tabulated in Table 1 and gradients for the respective months <br /> are contoured on Figures 2, 3, 4 and 5 <br /> IThe ground water elevations in the momtonng wells on the Royal Oak site were vi rti ally <br /> unchanged for the months of August through December, 1992 (Figures 24) Water <br />' measurements taken during the monitoring event on January 27, 1993, show that , not only <br /> did the water levels all of the wells nse, but also the gradient had reversed with the water <br /> table contours forming a southeasterly-trending trough(Figure 5) <br />' The ground water contours for this pend form a westerly-trending trough, whernt <br /> reversed from an easterly-trending trough Incomplete information suggests that the <br />' westerly-trending trough in the piezometnc surface prevails in the late summer and <br /> through most of the winter months The pattern then changes to an easterly-trending <br /> trough under the influence of recharge of the aquifer from winter rainfall <br /> Summary of Analytical Findings <br /> Monitoring wells 7 and 8 were sampled on November 4, 1992, and tested "none detected" for all <br /> analytes Well 2 was not tested at that time as a soil vapor extract{on system was installed on <br /> I MW-2, and access was temporarily restricted However, all three wells were sampled on January <br /> 27, 1993, and were N D for all analytes tested(see Table 2) <br /> It is worth noting that au samples tested from the soil vapor system at the start up showed TPH <br /> concentrations of greater than 2,500 ppm The levels have declined rapidly and, as of December <br /> 25, 1992, the levels are "none detected" We have enclosed a summary of the air testing performed <br /> at the site since the soil vapor system was turned on(Table 4) <br /> Recommendations <br /> WHF recommends that the soil vapor extraction system be removed from the site We also <br /> recommend that the site be considered for closure The San Joaquin County Environmental Health <br /> Department has condended that the contaminated soils left in place at the comer was the <br /> cause of the mternuttent ground water contamination in wells 2 and 7 The soils are now <br /> clean, via the soil vapor extraction system, and ground water samples indicate that the <br /> ground water is no longer contaminated <br /> I <br />
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