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ARCHIVED REPORTS XR0009475
Environmental Health - Public
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3500 - Local Oversight Program
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PR0544711
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ARCHIVED REPORTS XR0009475
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Last modified
7/30/2019 3:10:02 PM
Creation date
7/30/2019 2:20:17 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009475
RECORD_ID
PR0544711
PE
3528
FACILITY_ID
FA0005478
FACILITY_NAME
CUTTER LUMBER
STREET_NUMBER
4004
Direction
S
STREET_NAME
EL DORADO
STREET_TYPE
ST
City
STOCKTON
Zip
95206
APN
17525005
CURRENT_STATUS
02
SITE_LOCATION
4004 S EL DORADO ST
P_LOCATION
99
P_DISTRICT
001
QC Status
Approved
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i <br /> Pilot Testing Report and Conceptual Corrective Action Plan July 15, 1994 <br /> Manna Pro, 4004 South EI Dorado, Stockton, CA 14 <br />' 513 Results <br /> Before analyzing the drawdown data, the values were compared to background water level trends <br />' occurring at the site before the pumping testing program As shown on the transducer hydrograph <br /> for well EW-1 (Appendix D), there were no significant fluctuations in groundwater levels in the data <br /> before the test started <br /> A flow rate of 1 3 gpm was maintained during the 3-day aquifer test This average rate was <br /> maintained throughout the aquifer test and was used in subsequent data analysis After 2,870 <br /> minutes of pumping at 1 3 gpm, a maximum drawdown of between 5 7 and 5 3 feet was maintained <br /> Drawdown during the 3-day aquifer test, as recorded by the data logger, are presented in <br />' Appendix D The data include date, elapsed time, and drawdown for each data logger probe <br /> location Table 3 summarizes the wells that were monitored, shows the maximum drawdown <br />' experienced at each well during the pumping test, and the radial distance from each monitored well <br /> to the pumping well <br /> Analytical results of samples collected from well EW-1 on October 19 and 26, 1993, during and after <br /> the pumping test are summarized in Table 4 Laboratory analytical reports are included in <br />' Appendix A <br />' 514 Data Analysis <br /> Graphical analyses for each well were performed based on the field-derived data The graphical <br />' analyses were obtained by computer-assisted matching of type-curves and field data When a <br /> successful match was achieved, the computer calculated the aquifer characteristics of storativity, <br /> hydraulic conductivity, and transmissivity <br /> The drawdown data from each of the monitoring wells was analyzed using Thus curve matching <br />' techniques Theis type curve matches made for the drawdown at the pumping well and three <br /> monitored observation wells (EW-1, OB-1, OB-2, and 013-3) are presented in Appendix E Table 5 <br />' summarizes the results of the aquifer analysis <br />' Storativity (S) is defined as the volume of water released from storage per unit surface area of the <br /> aquifer per unit change in head In confined aquifers, this is the result of compression of the aquifer <br />' 2819R034 070 <br /> GROUNDWATER <br />' HF9 TECHNOLOGY, INC <br />
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