DOI: 10.18122/td.1860.boisestate
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Laboratory Measurement of Electrical and Hydraulic Properties of Regolith Over Granitic Bedrock

Abstract: Characterizing water flux within the critical zone (CZ) is essential for a multitude of studies and applications related to irrigation, drainage, water management, and contaminant transport. Trying to measure water flux in the critical zone, specifically in the subsurface, is difficult due to the associated structural heterogeneity and complex interactions taking place between biological, chemical, and physical processes. Current methods (i.e., inferred from soil suction and so… Show more

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“…Note that the calibrated hydraulic conductivity ratio K v /K h > 1 is consistent with the results from previous studies (Fullhart et al, 2019). The calibrated K v of the regolith layer is similar for all four cases and is close to the value measured in the lab (Bienvenue, 2021). The porosity 𝜙 of the regolith, however, varies considerably among the four cases.…”
Section: Model Calibrationsupporting
confidence: 89%
“…Note that the calibrated hydraulic conductivity ratio K v /K h > 1 is consistent with the results from previous studies (Fullhart et al, 2019). The calibrated K v of the regolith layer is similar for all four cases and is close to the value measured in the lab (Bienvenue, 2021). The porosity 𝜙 of the regolith, however, varies considerably among the four cases.…”
Section: Model Calibrationsupporting
confidence: 89%