2018
DOI: 10.1007/978-981-10-5795-3_26
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A Critical Study on the Applicability of Forchheimer and Wilkins Equations for Nonlinear Flow Through Coarse Granular Media

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“…While there was no significant effect of hydraulic gradient for the sands (standard deviation was less than 1%), hydraulic gradient affected K sat for the gravels (average standard deviation was 11.9%). Specifically, K sat values for the gravels decreased (except sample #15) with an increase in gradient from 0.25 to 2.00, potentially caused by migration and clogging of small particles or effects of turbulent flow in the relatively large pore spaces of the gravels (e.g., [16][17][18]. Average K sat,avg was selected for use in all subsequent analyses.…”
Section: Hydraulic Conductivitymentioning
confidence: 99%
“…While there was no significant effect of hydraulic gradient for the sands (standard deviation was less than 1%), hydraulic gradient affected K sat for the gravels (average standard deviation was 11.9%). Specifically, K sat values for the gravels decreased (except sample #15) with an increase in gradient from 0.25 to 2.00, potentially caused by migration and clogging of small particles or effects of turbulent flow in the relatively large pore spaces of the gravels (e.g., [16][17][18]. Average K sat,avg was selected for use in all subsequent analyses.…”
Section: Hydraulic Conductivitymentioning
confidence: 99%