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�C." it + Cl <br /> ALISTO ENGINEERING GROUP , <br /> September 18, 1995 <br /> AFI, ? z 1995 <br /> Mr Scott Hooton -J <br /> BP Oil Company fir v'.L ,.0 <br /> Environmental Resources Management ENVIRONMENTAL DEPT. <br /> 295 S W 41st Street vVEST COAST REGION OFFICE <br /> Building 13, Suite N <br /> Renton, Washington 98055 10-136-04-001 <br /> Subject Revised Analysis of Baildown Test Results <br /> BP Cil Company Service Station No 11193 <br /> 3202 West Hammer Lane <br /> Stockton, California <br /> Dear Mr Hooton <br /> On February 21, 1995, Alisto Engineering submitted the results of the baildown testing at BP <br /> Oil Company Service Station No 11193, 3202 West Hammer Lane, Stockton, California <br /> After further review of the test data and results of analysis, it was determined that the <br /> reported values of hydrogeologic properties for MW-1 needed to be revised <br /> The time-displacement plots of the test data revealed a "double straight line effect" This <br /> phenomena was described by Herman Bouwer in an article titled The Bouwer and Rice Slug <br /> Test_- An Update published in the May/June 1989 issue of Ground Water In accordance <br /> with the recommendations presented therein, the second straight line portion of the plot was <br /> considered more indicative of flow in the undisturbed aquifer and was used for calculations <br /> The interpretation of the test data for MW-1 was previously based on the "first leg" of the <br /> plot, which was not consistent with the data analysis for MW-2 and MW-5 or <br /> recommendations in the Bouwer article The revised calculation of hydrogeologic parameters <br /> for MW-1 is shown in the enclosed graph, and the revised test results are presented in Table <br /> 1 <br /> During testing of MW-1, the submersible pump was only capable of drawing down 15 feet <br /> of groundwater in MW-1 at a maximum pumping rate of 6 gallons per minute The rapid <br /> recovery may be due to the sand unit encountered in the lower portion of MW-1 and may <br /> not be representative of the material in the saturated zone <br /> Based on a review of the boring logs, the predominant soil types of the water-bearing zone <br /> are silt and silty sand underlain by fine to medium sand, which generally have K values <br /> ranging from approximately 1 to 1 x 10-5 cm/s (Freeze and Cherry, 1979) The values of the <br /> aquifer parameters calculated from the baildown tests are within the lower range of expected <br /> values and consistent with the types of soils encountered at the site <br /> 1575 TREAT BOULEVARD SUITE 201 -WALNUT CREEK CA 94598 • (510) 295-1650 • (5I0) 295-1823 <br /> CONTRACTORS LICENSE NO A-652544 <br />