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Frequency domain electromagnetic induction (EMI) data collected within and ad...
The electrical conductivity of the earth is used to help infer lithological and pore fluid properties. Various geophysical methods can provide estimates of the distribution of... -
Frequency domain electromagnetic induction (EMI) data collected within and ad...
The electrical conductivity of the earth is used to help infer lithological and pore fluid properties. Various geophysical methods can provide estimates of the distribution of... -
Electrical resistivity tomography (ERT) data collected within and adjacent to...
The electrical conductivity of the earth is used to help infer lithological and pore fluid properties. Various geophysical methods can provide estimates of the distribution of... -
Frequency domain electromagnetic induction (EMI) data collected within and ad...
The electrical conductivity of the earth is used to help infer lithological and pore fluid properties. Various geophysical methods can provide estimates of the distribution of... -
Fiber-optic distributed temperature sensing (FO-DTS) data collected in the Li...
Natural heat is used as a tracer for a variety of physical hydrogeological process, including zones of preferential exchange between groundwater and surface water. Several types... -
Fiber-optic distributed temperature sensing (FO-DTS) data collected in the Li...
Natural heat is used as a tracer for a variety of physical hydrogeological process, including zones of preferential exchange between groundwater and surface water. Several types...
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