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r <br /> 01- <br /> PRELIMINARY INVESTIGATION AND EVALUATION REPORT <br /> October 1996 <br /> Gemelos Property (Paladin Center) <br /> 2421 East Holly Drive <br /> Tracy, California <br /> I <br /> 10. INTRODUCTION AND SCOPE OF'WORK <br /> In accordance with the request of Mr John Gemelos Advanced GeoEnvironmental, Inc (AGE) has <br />' prepared the enclosed Preliminary Investigation and Evaluation Report(PIER) for the site located <br /> at 2421 East Holly Drive, Tracy, California (the site) <br /> The objective of the investigation was to detennine the lateral and vertical extent of hydrocarbon- <br /> impacted soil and ground water at the site The scope of work included the installation of one soil <br /> boring, three groundwater monitoring wells and the collection of groundwater samples The field <br /> work was pez formed on 11 July 1996 The location of the site is illustrated on Figure 1 - Location <br /> Map Structures, boring and monitoring well locations are shown on Figure 2 - Site Plan <br /> The work was performed in accordance with San Joaquin County Public Health Services - <br /> Environmental Health Division (PHS-EHD) and Central Valley Regional Water Quality Control <br /> Board guidelines for investigation of underground storage tank (UST) sites <br />' 20. BACKGROUND <br /> 21 SITE LOCATION <br />' The site is located 3n a residential area of central Tracy, California, in San Joaquin County (Figure <br /> 1) One building used for auto repair is currently located on the property The building is <br />' immediately west of the former UST area Another auto repair business is located east of the site <br /> 2 2 UNDERGROUND STORAGE TANK REMOVAL <br /> Two 10,000-gallon underground storage tanks (USTs) were removed from the property in April <br />' 1988 Approximately 100 to 120 cubic yards of soil were removed during the excavation Upon <br /> removal of the USTs, soil and ground water samples were collected from the excavation areas <br />' Laboratory results from the samples indicated that hydrocarbon-impacted ground water was present <br /> at the site <br /> 1 <br /> .t <br /> 1 <br />