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II2 0GEOL E <br /> t . <br /> A GROUNDWATER CONSULTANCY <br /> I <br /> PO Box 2165 ■ Livermore, Cahfomia 94551 ■ (925)373-9211 v F , /0 41, <br /> Local Oversight Program October 01, 2001 <br /> San Joaquin County <br /> Department of Health Services <br /> P O Box 2009 <br /> Stockton, CA 95201 <br /> RE Third Quarter, 2001 Groundwater Monitoring Report - Underground Storage Case <br /> Former Cheaper) #37, 15 Grant Line Road, Tracy, San Joaquin County <br /> Dear Local Oversight Program; <br /> This Third Quarter, 2001 Groundwater Monitoring Report is submitted by H20GEOL on behalf <br /> of The Customer Company for the former Cheaper) Store #37, 15 Grant Lane Road in Tracy, San <br /> Joaquin County, California. The site location is shown on Figure 1 and is now More for Less #37. <br /> The Third Quarter, 2001 groundwater monitoring event occurred on August 18, 2001 <br /> r <br /> 10 POTENTIOMETRIC SURFACE <br /> Depth to water in each monitoring well was measured to +/- 0.01 feet using a Sohnst Model <br /> water level meter between 11 22 and 1128 on August 18, 2001 The depths to water were <br /> converted to potentiometric surface elevation by subtracting the measured depths to water from <br /> the casing top elevations derived from the well survey performed in 1995 by Benchmark <br /> Consultants The depth to water, casing top elevations, and potentiometne surface elevations are <br /> presented in Table 1 All available previous water level measurements are sumnnarized an Table C1 <br /> in Attachment C <br /> Figure 2 as a map showing the approximate potentiometnc surface for the monitoring wells at the <br /> site on August 18, 2001 Table 2 lists the slope(gradient) and direction of gradient of the <br /> potentaometric surface for each of the triangles with a well at each apex The average gradient of <br /> the potentaometnc surface was 0 0029 feet per foot. The average gradient direction was oriented <br /> N 12 5°E. <br /> All available previous potentiometnc surface slope (gradient) and direction of gradient are <br /> summarized in Table C2 m Attachment C. <br />