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ARCHIVED REPORTS_XR0008575
Environmental Health - Public
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3500 - Local Oversight Program
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PR0545857
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ARCHIVED REPORTS_XR0008575
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Last modified
7/15/2020 4:45:53 PM
Creation date
7/15/2020 3:01:42 PM
Metadata
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Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0008575
RECORD_ID
PR0545857
PE
3528
FACILITY_ID
FA0005147
FACILITY_NAME
E-Z FOOD
STREET_NUMBER
2537
STREET_NAME
WATERLOO
STREET_TYPE
RD
City
STOCKTON
Zip
95205
APN
11914035
CURRENT_STATUS
02
SITE_LOCATION
2537 WATERLOO RD
P_LOCATION
99
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Data collected during the aquifer test will be evaluated using various graphical and numerical methods, <br /> depending on flow (steady or unsteady state) well construction (fully or partially penetrating) and aquifer <br /> type (confined, leaky, unconfined, or sena-confined) The aquifer test will be evaluated using more than one <br /> method Analysis of the aquifer test data will be conducted utilizing computer software <br /> A majority of the aquifer test will be conducted using partially penetrating wells in unconfined aquifers <br /> under steady state conditions In general, the curve-fining method presented by Neuman (1975) or by <br /> Boulton (1954) will be used to evaluate transmissivity, storativity and vertical hydraulic conductivity under <br /> these conditions (the Boulton method assumes nonsteady state conditions) The Stretitsova's curve-fitting <br /> method presented by Kniseman and de Ridder (1990) may also be used for unconfined conditions In <br /> addition, the steady state well equation may be applied (Todd, 1980) to evaluate the hydraulic conductivity <br /> (away from the pumping well) <br /> If it is determined that the test was performed under confined aquifer conditions and enough time has elapsed <br /> for steady-state conditions to have been met(as defined in the literature), the Jacob distance-draw down and <br /> time-draw down methods (Cooper & Jacob, 1946) will generally be applied to evaluate storativity and <br />' transmissivity Alternatively, the Theis curve-fitting method (Theis, 1935) may be employed if steady-state <br /> conditions were not reached In leaky aquifers, the Hantush method(Hantush, 1956)will generally be used <br /> The capture zone will also be determined using the transmissivity values obtained through the evaluation and <br /> following the method initially outlined by Janvandei and Tsang (1986) The data will then be used to <br /> determine the construction and design specifications of the proposed system, based on the requirements of <br /> the system conceptual design(migration control, dewatering,plume capture) <br /> It must be recognized that even using theoretical models for the data evaluation, some judgment will be <br /> necessary in conducting the analyses and applying the calculated parameters to the system design <br /> Different types of aquifers may have similar draw down or response behaviors, and this must be <br /> accounted for A complete explanation of the method used and the reasoning behind the choice of method <br /> and an analysis of the results will be presented with the data evaluation The pump test will be performed <br /> in general accordance with ATC's Standard Operating Procedure — Constant Discharge Aquifer Test, <br /> which is included in Appendix A <br /> 5.11 Data Evaluation and Corrective Action Plan <br /> Following installation of the groundwater monitor wells and completion of the vapor extraction, air sparge <br /> and groundwater extraction pilot studies, ATC will evaluate the information and provide a written CAP to <br /> the SJC The CAP will conform to the guidelines established in the most recent version of the SJC <br /> Guidelines <br /> 6.0 ASSUMPTIONS <br /> • ATC will not be responsible for any unforeseen conditions (i e , shallow groundwater conditions, hard <br /> soils, unknown utilities) <br /> i <br /> EZ 100966SAFSWP ATC Associates Inc <br /> S 1EZ Sme\EZ 1009661Reports1100966SAFSWP ATC Project No 43 25 82 7 0026 <br /> 13 <br />
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