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ARCHIVED REPORTS_XR0008888
Environmental Health - Public
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3500 - Local Oversight Program
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PR0545786
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ARCHIVED REPORTS_XR0008888
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Last modified
6/1/2020 2:37:03 PM
Creation date
6/1/2020 2:09:21 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0008888
RECORD_ID
PR0545786
PE
3526
FACILITY_ID
FA0004969
FACILITY_NAME
CHASE CHEVROLET
STREET_NUMBER
424
Direction
N
STREET_NAME
VAN BUREN
STREET_TYPE
ST
City
STOCKTON
Zip
95205
CURRENT_STATUS
02
SITE_LOCATION
424 N VAN BUREN ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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LSauers
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EHD - Public
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' 10 December 2001 <br /> AGE NG Project No 95-0143 <br />' Page 4 of 10 <br />' MW-9 (located 140 feet toward the north) at 0 08 feet after 350 minutes of purnpmg <br /> operation <br />' The maximum ground water draw-down in the seven observation wells versus the distance of each <br /> well from the extraction point were graphed on semi-logarithmic paper(Appendix B) Inferred radii <br />' of influence of 100 feet (6 gpm), 120 feet (8 gpm) and 120 feet (10 gpm)were determined utilizing <br /> the semi-loganthmuc plots of draw-down versus distance(Appendix B) Ground water levels In the <br /> observation wells all appeared to be influenced and had measurable draw-down during each step of <br /> the pumping test However, decreased draw-down(increased ground water elevation) was noted In <br /> observation wells VW-1, MW-7, VW-4 and MW-9 during the 10 gpm test after 410 minutes of <br /> pumping operation(165 minutes of pumping at 10 gpm) At 480 minutes of pumping operation(235 <br />' n-nnutes ofpumping at 10 gpm), decreased draw-down was observed in each of the observation wells <br /> and the top of the pump was exposed In addition, the extracted water discharged from the pump <br /> contained significantly more fine-grained material than had been noted at 6 and 8 gpm Decreased <br /> draw-down may be related to a shift from laYrnnar flow to turbulent flow conditions at the extraction <br /> well Results of the aquifer ground water pumping test are summarized in Table 2 <br /> An optimum pumping rate of 8 gpm was determined based on the inferred radius of influence and <br /> the relatively stable pumping conditions observed during the 8-hour test <br /> 3 1 2 Extracted t acted Water Sampling Procedures <br /> Nine grab ground water samples were collected prior to discharge into the Baker tank Three samples <br /> were collected during each step of the variable rate pumping test, one at the beginning, one near the <br /> middle and one at the end of the step The samples were collected as follows <br /> • Sample EW-3/08 30 was collected after 20 minutes of pumping at 6 gpm, <br /> • Sample EW-3109 15 was collected after 65 minutes of pumping at 6 gpm, <br /> • Sample EW-3/10 15 was collected after 135 minutes of pumping at 6 gpm, <br /> • Sample EW-3/10 25 was collected immediately after increasing the pumping rate to 8 gpm <br /> (total pumping duration of 145 minutes), <br /> • Sample EW-3/11 45 was collected after 80 nunutes of pumping at 8 gpm (total pumping <br /> duration of 225 minutes), <br /> • Sample EW-3/12 25 was collected after 120 minutes of pumping at 8 gpm.(total pumping <br /> • duration of 265 minutes), <br /> Advanced GeoEnwronmenta4 Inc <br />
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