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4.0 INVESTIGATIVE METHODS <br /> 4.1 Visual Survey <br /> Geocon personnel conducted a visual survey of the Site prior to the geophysical survey and the <br /> advancement of soil borings. The visual survey was used to help identify areas of apparent petroleum <br /> hydrocarbon soil staining, indications of buried utilities, the possible location of the product lines <br /> associated with the AST, and possible obstructions to the advancement of borings. <br /> 4.2 Geophysical Survey <br /> Caltrans specified the geophysical methods used for this investigation. The methods chosen by <br /> Caltrans were the GPR and EM methods. GPR and EM are standard methods for the detection of <br /> buried objects and anomalies in the subsurface. Spectrum Geophysical performed the GPR and EM <br /> portions of the geophysical site investigation as a subcontractor to Geocon. <br /> 4.2.1 GPR Method <br /> The geophysical site investigation included a GPR survey as specified by Caltrans. GPR is a standard <br /> method for the detection of buried objects and anomalies in the subsurface. The GPR survey was <br /> undertaken using a Geophysical Survey Systems, Inc. (GSSI) Model l0A sled type 500-MHz antenna <br /> with an internal receiver with built-in hard drive and video display. This instrument has a color display <br /> that enabled convenient acquisition, storage, and preliminary analysis of data in the field. For each <br /> area of interest, GPR data were collected along parallel traverses spaced approximately 1-m(3.28 feet) <br /> apart. The instrument was calibrated to record over a 50-nanosecond (ns) vertical scale and dragged <br /> along each traverse. Records of each GPR profile were recorded for post survey processing, and <br /> reviewed in the field for indications of USTs or other suspect buried features. <br /> The GPR emits radio waves, which are focused and directed into the subsurface under the GPR <br /> antenna. Dense buried objects such as those made of metal reflect the radio waves. GPR can also be <br /> used to detect a former excavation or area of disturbed soil due to the density contrast between the <br /> backfill and the surrounding undisturbed soil. The higher the frequency of the waves emitted, the <br /> greater the imaging resolution. However, depth of investigation decreases with an increase in <br /> frequency. The 500-megahertz antenna and 50-ns vertical scale were used for this survey as they <br /> provided a good compromise between resolution and depth of investigation for this project. <br /> 4.2.2 Electromagnetic Method <br /> The EM survey was performed using an EM-61 transmitter. The EM-61 generates short pulses of EM <br /> energy which travel downward and outward and have a primary field associated with them. The energy <br /> associates with conductive materials and causes a secondary magnetic field. The receiver measures the <br /> voltage of the decay curve of the secondary magnetic field which is proportional to the conductivity of <br /> Project No 58475-06-70 -5- July 9,2003 <br />