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ARCHIVED REPORTS_XR0006719
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ARCHIVED REPORTS_XR0006719
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Last modified
5/5/2020 10:35:44 AM
Creation date
5/5/2020 9:46:10 AM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0006719
RECORD_ID
PR0543479
PE
2960
FACILITY_ID
FA0024679
FACILITY_NAME
CANEPA'S CAR WASH
STREET_NUMBER
6230
STREET_NAME
PACIFIC
STREET_TYPE
AVE
City
STOCKTON
Zip
95204
APN
081360030
CURRENT_STATUS
01
SITE_LOCATION
6230 PACIFIC AVE
P_LOCATION
01
QC Status
Approved
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al � <br /> Canepa s Car Wash <br /> 6230 Pacific Avenue,Stockton,CA <br /> First Quarter Groundwater Monitoring Report,January 2005 <br /> Page 3 of 8 <br /> GROUNDWATER ELEVATIONS AND GRADIENT <br /> Groundwater elevation contours estimated for the shallow monitoring wells (MW-1, MW-2, MW-4, <br /> MW-5, MW-6, MW-7, MW-9, and MW-10) on January 21, 2005 indicate a groundwater gradient <br /> generally toward the northwest (consistent with historic gradients) but with a localized gradient toward <br /> MW-1 (cone of depression) MW-1 is currently used as the primary groundwater extraction well for the <br /> treatment system (Figure 2, Attachment A) The cone of depression around MW-1 on January 21, 2005, <br /> indicated a relatively small radius of influence (apparently measurable to a radius of less than 20 feet) <br /> because it was measured approximately 20 hours after the pumping was re-initiated following a down <br /> period of approximately 10 days The treatment system had been off for the 10 days prior to the <br /> monitoring event to repair a failed ring compressor The small cone of depression, therefore, is partly the <br /> result of insufficient time for the cone of depression to expand In addition, the pumping rate, once the <br /> pumping was re-initiated, was at a reduced rate of approximately 3 5 gallons per minute (down from a <br /> maximum rate of approximately 6 gallons per minute) The pumping rate, following the repair, was <br /> reduced because of scaling Subsequent efforts have been made to reduce the scaling and return the <br /> system to optimal performance <br /> An estimated groundwater gradient of 0 0051 ft/ft towards the northeast was measured using water level <br /> data from monitoring wells MW-6 and MW-9 MW-6 and MW-9 are upgradient and down-gradient, <br /> respective to MW-1, and were outside the radius of influence of the cone of depression formed by <br /> groundwater extraction activities in MW-1 during the monitoring event The average depth to <br /> groundwater measured in the shallow monitoring wells for this event, excluding MW-1, decreased <br /> (increase in groundwater elevation) by approximately 1 64 feet since October 14, 2004 A hydrograph of <br /> historic groundwater elevations is attached as Figure 3 It should be noted that the top of the well screens <br /> for shallow monitoring wells MW-1 through MW-7 were below the water table, consistent with much of <br /> the monitoring history at the site <br /> Table 2 <br /> Groundwater Elevation Data (January 21, 2005) <br /> WELL <br /> Well Casing Screen Well Collar Depth to Water Groundwater <br /> Interval (feet-bgs) Elevation' (feet) (feet) El nation <br /> fe <br /> MW-1 50-70 1548 4527 -2979 <br /> MW-2 50-70 1529 3907 -2378 <br /> MW-3 50-70 1553 3984 -2431 <br /> MW-4 50-70 15 83 4011 -2428 <br /> MW-5 50-70 1471 39 17 -2446 <br /> MW-6 45-65 1489 38 13 -2324 <br /> MW-7 45-65 15 80 3920 -2340 <br /> MW-9 25-45 1484 3925 -2441 <br /> MW-10 25-45 1472 38 19 -2347 <br /> MW_1125-45 15 12 3870 -2358 <br /> MW-12D 100-110 1499 3833 -2334 <br /> ` Well Collar Elevations are measured from a mark on the top of the well casing and are referenced to NCS benchmark HS0391 using NAVD 88 <br /> datum <br /> bgs=below ground surface <br /> �� CONDOR <br />
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