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h <br /> Mwj <br /> 7si.1 .s 5_ 1 <br /> W11 w _ Fywn SE _ <br /> 1. <br /> NOgCAI <br /> CH2M-Hill <br /> May 10, 1991 <br /> page 2 <br /> ie length from 11 to 15 feet for <br /> we performed 6 Werth-south and B east-west traverses as s own on <br /> plate 1 . These traverses range We also performed severe} <br /> a total coverage of 193 line feet' at•ion to confirm <br /> - traverses to the south ofthe apQpelinenVeOur9scope of work <br /> the GPR data and presenting our findings in <br /> the location of an underground <br /> includes interpreting <br /> a written report• <br /> GROUND PENETRATING RADAR <br /> Ground penetrating radar (GPR) <br /> is a method that provides a con- <br /> ting <br /> tins in <br /> uous, high resolute°escross-section <br /> s <br /> hallow esubsurfaceT.�aThe nmethod <br /> ivi- <br /> the electrical proper <br /> is particularly sensitive to variations inveofcarmaterialical dtothold <br /> ty and electrical permittivity (the abi] it, <br /> a charge when an electrical field is app <br /> lied) . <br /> continuously radiates an electromagnetic <br /> In operation, the systemas it is moved <br /> " pulse into the ground from a transducer (antenna) <br /> along a traverse. Since most aeaterialsthe radarrsignaleis to <br /> electromagnet energy, only portion resenting varia- <br /> whin the signal encounters a <br /> reflected back to the surface from interfaces r is reflected. <br /> tions in electrical properties. <br /> metal object, however, all of the in ' +-he and are <br /> pals are received by = records can <br /> The reflected signals hical recorder. The resulting <br /> the stratification, the thickness <br /> transmitted to a grail acts such <br /> provide infarmetion regarding the location of buried obi <br /> and extent of fill material , when the <br /> as utilities, and changes in material conditions such as satura- <br /> in some instances, chemical differences (when <br /> rela- <br /> tion and, properties are altered) , eneralltion <br /> subsurface electrical <br /> tively high electrical conductivities reduce the <br /> r capability and limit radar P <br /> Geophysical Survey Systems, <br /> Fez" this investigation, <br /> we use! RadarSystem equipped with a 500 <br /> inc. SIR-3 Subsurface Inerfacc <br /> antenna. This antenna is near the center of the <br /> megaHertz. (MHz) range and was used to provide high resolution <br /> available frequency <br /> at shallow depths. <br /> PROCEDURES <br /> We obtained GFR data by hand towing the 500 MHz antenna along the <br /> Horizontal control along each <br /> a- <br /> traverses shown on Plate electronically annotating there- <br /> verse was established by These distances were determined <br /> the from <br /> cords at 5 foot intsthe round along the length <br /> of <br /> a fibergiass tape placed an <br /> traverse. <br />