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Rates of vertical groundwater movement estimated from the Earth's thermal profile | Synapse

June 1, 1965

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Rates of vertical groundwater movement estimated from the Earth's thermal profile

JBJohn BredehoeftETH Zurich IPI. S. Papaopulos

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Resumen

An analytical solution is developed describing vertical steady flow of groundwater and heat through an isotropic, homogeneous, and fully saturated semiconfining layer. A type‐curve method for estimating groundwater velocities from temperature data is presented.

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Bredehoeft et al. (Tue,) studied this question.

synapsesocial.com/papers/69de94ce40ea0656795585be https://doi.org/https://doi.org/10.1029/wr001i002p00325

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