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KLEINFEL DER <br /> File No. 23 -480020. D00 <br /> r August 26, 1994 <br /> 1 <br /> 4.0 FIELD ACTIVITIES <br /> Irl Prior to conducting any subsurface exploration, Kleinfelder contacted Underground Services Alert <br /> (USA) to locate underground utilities on or adjacent to the site. Additionally, Kleinfelder <br /> subcontracted Norcal Geophysical Consultants of Petaluma, California to conduct a geophysical <br /> survey on-site (both within the sidewalk and building areas). Kleinfelder then collected a total of <br /> [ I eight (8) soil samples for environmental purposes and fourteen (14) for geotechnical purposes <br /> from two soil borings advanced on site. All of the soil borings were advanced adjacent to the <br /> garage at one end of either of the USTs. <br /> 4.1 DRILLING AND SOIL SAMPLING <br /> I <br /> The soil borings were advanced on June 2, 1994 using a truck-mounted drill rig equipped with 8- <br /> inch hollow stem augers. For the location of the borings, please refer to Plate 1 . Soil cuttings <br /> from the soil borings were placed in 55-gallon drums and stored inside the garage. All borings <br /> were backfilled by pumping a neat cement grout with approximately 2 percent bentonite added to <br /> reduce shrinkage. <br /> While drilling, an experienced environmental and geotechnical engineer classified the subsurface <br /> soil and logged the boreholes. A copy of the Unified Soil Classification System used to classify <br /> I the soil and a log key are provided in Appendix A. Descriptions of the sample intervals and the <br /> L soil encountered in each boring are also presented in Appendix A. Kleinfelder's Field Procedures <br /> for drilling and sampling are provided in Appendix B . A copy of the drilling permit obtained <br /> F-) from San Joaquin County is provided in Appendix C. <br /> J The two borings were advanced a maximum depth of approximately 25 feet below grade. Soil <br /> samples were collected in these borings at 5400t intervals to the bottom of the boring. <br /> Generally, the soil encountered beneath the site consisted of alternating units of gray/black clayey <br /> sand/silty clay in the upper 9 to 15 feet. Below the clayey sand/silty clay was alternating units of <br /> gray/gray-brown clayey sand and clayey silt to the maximum depths explored. Groundwater was <br /> not encountered in our borings. <br /> 4.2 QUALITATIVE FIELD SCREENING <br /> To provide a qualitative indication of the presence of volatile organic constituents in the soil and <br /> to monitor the constituent concentrations in the breathing zone, a portable organic vapor analyzer <br /> IJ <br /> ETH:md 7EI94 <br /> Copyright 1994 Kleinfelder, Inc. Page 8 of 14 <br />