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Wm. J. Hunter & Associates 2220 Loma Vista Dr <br /> Registered Geologists Sacramento, CA 95825 <br /> Petroleum & Mineral Appraisers -- (916) 972-7941 <br /> ffl:�h San trim FAX (916) 972-1683 <br /> March 9 1996 REL;VRI) <br /> MAR 2 2 9996 <br /> Michael Infurna, Sr REHS ENVIRONMENTAL HEALTH <br /> San Joaquin County PHS PFRMfT/SERVICES <br /> Environmental Health Division <br /> 445 No San Joaquin Street <br /> Stockton, CA 95202 <br /> Ref FIRST QUARTER, 1996, GROUNDWATER MONITORING REPORT, 1876 <br /> Country Club Drive, Stockton; Site Code 1844 <br /> Dear Mr Infurna; <br /> We are enclosing the results of the tenth groundwater measure- <br /> ments, sampling & laboratory results done on February 1, 1996, <br /> covering the above property. Included are copies of the field <br /> logs made by Del-Tech, a table summarizing sampling results, <br /> laboratory reports, a site map showing the pieziometrzc surface <br /> based on the 2/1/96 data, including directions of all of the <br /> hydraulic gradients measured to date We have also maps showing <br /> lines of equal concentrations of benzene, ethylbenzene, toluene, <br /> xylene & TPHg based on the most recent data <br /> A review of this work is discussed below <br /> 1 The water table was measured at an average depth of 18 38 ' <br /> bgl, (-14 .22 ' msl, ) a drop of slightly over 1 ' since the December <br /> sampling. The average maximum change in groundwater elevation <br /> has been 3 . 821 since monitoring began. The lowest average depth <br /> was recorded at 22 201 bgl in January, 1994 , the highest was the <br /> latest event, February, 1996, at 18 38 ' bgl <br /> 2 The hydraulic gradient as calculated from the latest event , <br /> (shown on PLATE I, ) indicates a change in direction and slope <br /> near MW-2 & MW-3 . From MW-2 & MW--3 north, the slope is very <br /> flat, at about . 141 /1001 . From those two wells south, the slope <br /> increases to 3 .21 /1001 . This is the first time that such a <br /> complete reversal in the potentiometric surface has been <br /> observed. Although the gradients have varied widely as shown on <br /> PLATE 1, the direction generally was consistent from well to <br /> well We do not have an explanation for this event <br /> 3 A summary of all laboratory results of water samples taken <br /> since monitoring began is shown on TABLE I That data shows MW-1 <br /> continues to have the highest levels of BTEX & TPH--G, MW-3 has <br /> the second highest, and MW-2 the lowest This ratio has remained <br /> consistent since monitoring began MW-4 & MW-5 revealed minor <br /> amounts of BTEX from the December, 1995 sampling apparently <br /> caused by contamination from the baler blanks It is not known <br /> whether the contamination was a result of water used for cleaning <br /> 1 <br />