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Magnetic
The magnetic method can be used to:
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Locate buried tanks and pipes
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Detect buried ordnance
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Map old waste sites and
landfill boundaries
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Locate abandoned steel well
casings
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Clear drilling locations
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Map basement faults and geology
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Investigate archaeological
sites
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Locate pits and trenches
containing buried metallic debris
The magnetic method involves the measurement of
the intensity of the earth's total magnetic field, a component of the
earth's magnetic field, or the horizontal or vertical gradient of the
earth's magnetic field. Anomalies in the earth's magnetic field are
caused by induced or remnant magnetism. Induced magnetic anomalies are
the result of secondary magnetization induced in a ferrous body by the
earth's magnetic field. The shape and amplitude of an induced magnetic
anomaly is a function of the orientation, geometry, size, depth, and
magnetic susceptibility of the body as well as the intensity and
inclination of the earth's magnetic field in the survey area. The
magnetic method is an effective way to search for small metallic
objects, such as buried ordnance and drums, because magnetic anomalies
have spatial dimensions much larger than those of the objects
themselves.

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