8th EEGS-ES Meeting 2002
DOI: 10.3997/2214-4609.201406177
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Gradient and Mid-Point-Referred measurements for multi-channel 2D resistivity imaging

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Cited by 15 publications
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“…When mapping with the TEM system, the soundings are generally placed with approximately 16–25 measuring points per square kilometre (Sørensen et al . ). To avoid corrupted data, a buffer zone of 100–150 m is kept on either side of electrical power lines, roads, buildings, etc.…”
Section: Introductionmentioning
confidence: 97%
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“…When mapping with the TEM system, the soundings are generally placed with approximately 16–25 measuring points per square kilometre (Sørensen et al . ). To avoid corrupted data, a buffer zone of 100–150 m is kept on either side of electrical power lines, roads, buildings, etc.…”
Section: Introductionmentioning
confidence: 97%
“…The limitations of this system have encouraged the development of new systems such as the pulled array transient electromagnetic (PATEM) system (Sørensen et al . , ; Sørensen ) and the high‐moment transient electromagnetic (HiTEM) system (Danielsen et al . ).…”
Section: Introductionmentioning
confidence: 99%
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“…Diverse LCI techniques have successfully been adapted to geophysical data (e.g. Auken et al, 2000 (pulled array DC data); (2-D geoelectrical data); Monteiro Santos, 2004 (ground frequencydomain electromagnetic (EM) data); (airborne time-domain EM data); Auken et al, 2005 (1-D geoelectrical data); (geoelectrical and borehole data); Wisén and Christiansen, 2005 (geoelectrical and surface wave seismic data); Tartaras and Beamish, 2006 (fixedwing frequency-domain EM data)). The LCI procedure used here is adapted to a one-dimensional inversion code developed at the HydroGeophysics Group (HGG) of the University of Aarhus, Denmark (Auken et al, 2002).…”
Section: Introductionmentioning
confidence: 99%
“…Electrical resistivity surveys are commonly used for geotechnical investigations and environmental surveys (Loke, 1999). Due to its efficiency and effectiveness in producing images of the subsurface, resistivity-imaging methods have now becomes more popular in electrical exploration (Dahlin and Zhou, 2002). The two dimensional (2D) direct current (DC) electrical resistivity methods measure the apparent resistivity of the subsurface, which can be inverted to develop a model of the subsurface structure and stratigraphy in terms of its electrical properties (Loke, 2003).…”
Section: Introductionmentioning
confidence: 99%