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Subsurface Investigation and Well Installation Report <br /> ARCO Facility No 6100 <br /> Tracy, California <br /> Page 4 <br /> purpose of soil sampling were completed using the mud rotary drilling method Hollow <br /> stem augers were not used to advance any soil borings due to difficult drilling conditions <br /> and to permit wireline geophysical logging within the boreholes Electrical methods <br /> were used to conduct borehole geophysical logging Delta was unable to obtain a special <br /> use permit to conduct neutron and gamma-gamma logging in an open borehole <br /> Exploratory Soil Borings <br /> Delta oversaw Western Strata Exploration, Inc of West Sacramento (C-57 #552198) <br /> advance six onsite soil borings (B-33 through B-38) between August 29 and September 7, <br /> 2001 Soil boring locations are shown on Figure 2 The borings were advanced to depths <br /> ranging from approximately 135 to 140 feet bgs using the mud rotary drilling method <br /> Each soil boring was continuously sampled in five-foot intervals using a 3-inch diameter <br /> core barrel advanced ahead of a 5 5-mch diameter drill bit The drilling mud consisted of <br /> water and powdered bentonite On reaching total depth of each borehole, anA electnc log <br /> was performed on the boring Following removal of the logging tool, the drilling mud <br /> was removed and the borehole backfilled to surface grade with neat cement <br /> Soil recovered from the core barrel was placed into core boxes and labeled according to <br /> borehole ID and sampling interval The soil was logged onsite using the Unified Soil <br /> Classification System Geologic logs of the soil borings and a copy of the drilling permit <br /> are presented in Appendix B Soil collected from selected intervals was field screened <br /> for volatile organic compounds using a photoionization detector (PID) Soil types and <br /> PID results were used to determine sampling depths Soil samples from selected intervals <br /> were collected by dnving a pre-cleaned brass tube into the soil core The ends of each <br /> sample tube were covered with Teflon TM sheets, capped, and sealed Each sample tube <br /> was subsequently labeled, placed in a resealable plastic bag, and stored in an ice-chilled <br /> cooler <br /> Wireline Geophysical Logging <br /> Delta retained Dewey Data Down Hole Surveys of Acampo, California, to conduct open- <br /> hole geophysical logging of borings B-33 through B-38 Following removal of the drill <br /> rods from the borehole, a sonde was lowered through the drilling mud to the total depth <br /> of the borehole Logging was conducted as the sonde was pulled up the borehole at a <br /> fixed rate of speed using a winch Electrical conductivity/resistivity of the formation, <br /> spontaneous potentials, and natural gamma radiation emitted from the formation were <br /> measured Copies of the borehole geophysical logs are presented in Appendix C <br /> Electneal conductivity/resistivity measurements were collected using electrode spacings <br /> of 16 inches, 64 inches, and from focused electrode logging (lateral logging) The largest <br /> contrasts in electrical conductivity/resistivity of the formation around the borehole were <br /> observed in the lateral log measurements The Dewey Data representative indicated that <br /> lateral logging is often the most effective downhole electrical method for observing <br /> P 1ARCO\61001REPORTS16100-well install report doc <br />