Near Surface Geophysics Site Map
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A 2D profile of apparent resistivity generated from multiple 1-D TEM measurements using a 100-m loop was used along with magnetic readings to interpret the location of the fault illustrated in the
profile. |
Electromagnetic methods are used at Southwest
Research Institute (SwRI) to measure subsurface electrical conductivity. SwRI scientists can perform electromagnetic surveys using
frequency domain electromagnetic instruments or transient electromagnetic instruments.
Transient Electromagnetics
Transient electromagnetic (TEM) instruments allow greater depth of penetration of an induced current by using large transmitter loops and lower frequency signals.
TEM methods, also known as time-domain electromagnetics, measure the electrical conductivity of soil and rock by inducing pulsating currents in the ground with a transmitter coil and monitoring the decay of the induced current over
time with a separate receiver coil.
Multiple one-dimensional soundings are used to generate two- and three-dimensional images of the subsurface. TEM measurements can be applied to:
Advantages of Transient Electromagnetics
Limitations of Transient Electromagnetics
For more information about near surface geophysics
and transient electromagnetics capabilities at SwRI or how you can contract with SwRI,
please contact
Ronald T. Green, Ph.D. at
rgreen@swri.org or (210) 522-5305, or
James
Prikryl at
jprikryl@swri.org or (210) 522-5667.
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Southwest Research Institute® (SwRI®), headquartered
in San Antonio, Texas, is a multidisciplinary, independent, nonprofit, applied
engineering and physical sciences research and development organization with 11
technical divisions.
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