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Preliminary Investigation and Evaluation Report <br /> RALPH'S SQUARE <br /> 2122 South Airport Way, Stockton, California <br /> 1.0. INTRODUCTION <br /> At the request of Mr. Ralph Lee White,property owner,Advanced GeoEnvironmental,Inc. (AGE) <br /> has prepared the enclosed Preliminary Investigation and Evaluation Report(PIER)for 2122 South <br /> Airport Way, Stockton, California(site).The purpose of this investigation was to assess the lateral <br /> and vertical extent of petroleum hydrocarbon impacted soil and groundwater at the site. The scope <br /> of work included establishment of soil borings,collection and analysis of soil samples,installation <br /> of three ground water monitoring wells, collection of ground water samples from three wells and <br /> preparation of this report of findings.The location of the site is illustrated on Figure 1.A plan of the <br /> site is illustrated on Figure 2. <br /> This report has been prepared in accordance with guidelines issued by the Central Valley Regional <br /> Water Quality Control Board(CVRWQCB)for subsurface investigations of the former underground <br /> storage tank(UST)systems. <br /> 2.0. BACKGROUND <br /> The site is bounded on the west by Airport Way, on the south and east by a vacant lot, and on the <br /> south by a commercial property. A single structure housing a mini-mart presently occupies the <br /> eastern portion of the site. <br /> 2.1. REGIONAL GEOLOGIC SETTING <br /> According to a Geologic Map of California, published in 1966 by the California Department of <br /> Conservation Division of Mines and Geology,the site area is within the Great Valley Geomorphic <br /> Province(GVGP)of California,a large,elongate,northwest trending structural trough.The GVGP <br /> is subdivided into two major divisions designated the Sacramento and San Joaquin Valleys,which <br /> have been filled to the present elevation with thick sequences of sediment ranging in age from <br /> Jurassic to present day, creating a nearly flat lying alluvial plain extending from the Tehachapi <br /> Mountains in the south to the Klamath Mountains in the north.The western and eastern boundaries <br /> of this province are comprised of the California Coast Range and the Sierra Nevada,respectively. <br /> Based on a General Soil Map from the San Joaquin County Soil Survey,published by the United <br /> States Department of Agriculture Soil Conservation Service in 1992, the site area is described as <br /> within the Jacktone-Hollenbeek-Stockton(JHS)association.The JHS soils are located on basin runs <br /> and within basins, and generally consist of somewhat poorly drained and moderately well drained, <br /> fine-textured soils that are moderately deep and deep to a cemented hardpan.The JHS soils generally <br /> formed in alluvium from mixed rock sources. <br /> Advanced GeoEnvironrnental,Inc. <br />