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ARCHIVED REPORTS XR0002741
Environmental Health - Public
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3500 - Local Oversight Program
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PR0508502
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ARCHIVED REPORTS XR0002741
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Last modified
11/7/2018 9:20:41 AM
Creation date
11/6/2018 3:31:51 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0002741
RECORD_ID
PR0508502
PE
3526
FACILITY_ID
FA0008117
FACILITY_NAME
ARCO STATION #4932
STREET_NUMBER
16
Direction
E
STREET_NAME
HARDING
STREET_TYPE
WAY
City
STOCKTON
Zip
95204
APN
13902001
CURRENT_STATUS
01
SITE_LOCATION
16 E HARDING WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Atlantic Richfield Company 10 <br /> ARCO 4932 16 E Harding Way Stockton CA .Pune 7,2002 <br /> rate is the highest pumping rate that will not draw the water level down to the pump <br /> over the duration of the constant-rate pumping test (approximately 24 hours) <br /> Following the completion of the step-drawdown test on April 2, 2002, the constant-rate <br /> pumping test was initiated The objective of the test was to create hydraulic stress in the <br /> ' aquifer by pumping from well EW-1 at a constant pumping rate, while monitoring <br /> drawdown in observation wells MW-1, MW-4, MW-6, and MW-7 Dunng the <br /> constant-rate pumping test, groundwater was continuously extracted for 1,323 minutes, <br /> ' while water levels were continuously logged in the pumping well and the four <br /> observation wells <br /> Extracted groundwater was discharged to a 6,500 gallon-capacity holding tank on-site <br /> Flow rates were monitored using a rotometer to register water flow from the system to <br /> the holding tank At the conclusion of the constant-rate pumping test, groundwater <br /> ' recovery data was monitored and recorded until water levels in the wells recovered to at <br /> least 99 percent of their pre-pumping levels The resulting drawdown and recovery data <br /> were analyzed to estimate the aquifer parameters of transmissivity (T), hydraulic <br /> conductivity (K), and storativity (S) <br /> Results of aquifer testing are discussed below Data plots of drawdown and recovery <br /> within pumping well EW-1 are included in Attachment J A summary of calculated <br /> hydraulic parameters is provided in Table 7 <br /> Step-Drawdown Pumping Test <br /> Pumping rates of 3 gpm, 4 gpm, 5 gpm, and 6 gpm were applied on extraction well EW- <br /> 1 for 30-minute intervals After pumping at 6 gpm for 30 minutes, the constant-rate <br /> pumping test was initiated utilizing this pumping rate <br /> Constant-Rate Pumping Test and Aquifer Recovery <br /> ' At the beginning of the constant-rate pumping test on well EW-1, pumping was <br /> continued at 6 gpm immediately after the step drawdown test and before recharge <br /> occurred After pumping from well EW-1 for 210 minutes at a rate of 6 gpm, it <br /> ' appeared that this pumping rate would dewater the well before equilibrium conditions <br /> were reached The pumping rate was then decreased to 5 5 gpm for 30 minutes, <br /> followed by a decrease to 5 gpm for 150 minutes, and another decrease to 4 5 gpm for <br /> ' 180 minutes The 4 5-gpm pumping rate also appeared to be dewatering the well and <br /> the pumping rate was reduced to 4 gpm for the remainder of the test (780 minutes) For <br /> data analysis, a time-weighted value for Q (pumping rate) was used, which was <br /> calculated using the pumping rates for the step-drawdown test and the constant-rate <br /> pumping test The constant-rate pumping test created a maximum drawdown of 13 73 <br /> ' feet in extraction well EW-1, 0 4 feet in well MW-1, 0 82 foot in well MW-4, 0 05 foot <br /> �\ in well MW-6, and 0 16 foot in well MW-7 After continuously pumping from well <br /> EW-1 for 1,323 minutes, the pump was shut down, and groundwater recovery levels <br /> 1 <br /> ' I1ARCO149321Reports\Asmt&AgfrTslRpt doc <br />
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