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Effect of Depth-Dependent Hydraulic Conductivity and Anisotropy on Transit Time Distributions

Journal of Hydrology(2019)

Cited 9|Views1
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Abstract
•New analytical solutions for Non-Dupuit–Forchheimer flow.•Influence of outflow boundary conditions on flow net structure.•Anomaly behavior of the particle travel time.
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Key words
Groundwater recharge,Vertical aquifer heterogeneity,Aquifer anisotropy,Flow net structure,Transit time distribution
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