2017
DOI: 10.1088/1755-1315/62/1/012008
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Evaluation of Semanggol Formation (Permian Facies) Using Electrical Resistivity Tomography and Seismic Refraction Tomography Parameter

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Cited by 4 publications
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“…ERT is a technique developed to observe subterranean structures and processes through electrical pulses emitted from electrodes [66]. Probes are laid in a line or encircling an object to obtain data on a specific transect, such as CO 2 fluxes deep in underground pools [67], monitoring the rate of water infiltration into concrete [68], or to determine different geological layers across a survey site [69]. However, if electrodes are buried and arrayed in a grid, then 3D resistivity measurements can also be obtained [70] and have been used to observe the dynamics of sub-surface gas-liquid mixing [71], CO 2 fluxes [72], and high-resolution variances in soil water content [73].…”
Section: Electrical Resistance Tomography To Map 4d Water Availabilitymentioning
confidence: 99%
“…ERT is a technique developed to observe subterranean structures and processes through electrical pulses emitted from electrodes [66]. Probes are laid in a line or encircling an object to obtain data on a specific transect, such as CO 2 fluxes deep in underground pools [67], monitoring the rate of water infiltration into concrete [68], or to determine different geological layers across a survey site [69]. However, if electrodes are buried and arrayed in a grid, then 3D resistivity measurements can also be obtained [70] and have been used to observe the dynamics of sub-surface gas-liquid mixing [71], CO 2 fluxes [72], and high-resolution variances in soil water content [73].…”
Section: Electrical Resistance Tomography To Map 4d Water Availabilitymentioning
confidence: 99%