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• <br /> The Geometrics G-858 cesium vapor magnetometer is typically used to obtain vertical magnetic <br /> ' gradient data. This instrument features a built-in memory that stores the vertical magnetic gradient <br /> and survey grid information. The information can be down loaded to a computer for further <br /> processing. <br /> ' Data Analysis <br /> ' Computer Processing <br /> ' The EM and VMG data are downloaded to a personal computer and converted it into a format for <br /> contouring. The contouring program (SURFER Version 8.0 by Golden Software) calculates an <br /> evenly spaced array of values(grid)based on the observed field data. Finally, these gridded values <br /> are contoured to produce EM(TC and IPC)and VMG contour maps. The contour intervals for each <br /> map are typically selected based upon the specific intensities, as well as for clarity of presentation. <br /> The contour maps are then analyzed to determine potential locations that may represent buried <br /> landfill material. <br /> Contour Map Interpretation <br /> The TC,IPC, and VMG contour maps show the respective variations in the electromagnetic terrain <br /> conductivity,electromagnetic in-phase component,and vertical magnetic gradient values within the <br /> ' survey area. Each contour map is characterized by a series of contour lines that represent specific <br /> values. Areas that lack contour lines,or where the contours are spaced far apart,indicate a minimal <br /> change or variation in the respective values. This is indicative of relatively uniform conditions. <br /> Areas where contours are closely spaced indicate variations that are not uniform and probably caused <br /> by local sources. <br /> ' In areas where there are significant quantities of above or below ground metal objects,the measured <br /> values are relatively large. These areas are characterized by numerous closely spaced contours. If <br /> ' the source of the anomaly is linear(e.g. underground utilities,railroad spurs, culvert, etc.),then the <br /> contours tend to parallel the object, and are closely spaced in close proximity to the object. If the <br /> below ground source is localized (e.g. buried drum, isolated metal debris, etc.), then the contours <br /> tend to form circular or elliptical closures that enclose the object. The larger the object and the <br /> closer it is to the geophysical instrument,the more contours there are in a given area. Variations that <br /> cannot be attributed to known above and/or below ground objects (metal well casings, reinforced <br /> ' concrete surface drain,above ground 55 gallon drums,utilities,etc.)are caused by unknown buried <br /> objects and are considered anomalous. <br /> ' Buried landfill material is often characterized by circular to elliptical contour closures. These <br /> closures can vary from large circular closures that cover broad areas,to clusters of small closures that <br /> ' A-2 <br />