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- W2485487760 abstract "Abstract Unsaturated flow in coarse granular media must pass through hydraulic bridges (e.g., pendular water, porous connections) that form a physical connection between adjoining clasts. Previous studies suggest that volumetric flow through a porous clast (Q) will be linearly dependent on the cross-sectional area of the hydraulic bridges, and understate the importance of bridge conductivity. Numerical simulations were performed to explore steady-state flow through a spherical clast with identical bridges located at the top and bottom. The cross-sectional area of the bridges relative to that of the clast (A r ) was varied across six orders of magnitude. The ratio of hydraulic conductivity between bridges and clasts (K b /K c ) was varied across 12 orders of magnitude to consider resistive, neutral, and conductive bridges. Results show that hydraulic bridges place a primary control on both Q and flux distribution within the clast. For neutral and conductive bridges (K b /K c ≥1), A r is the dominant factor in determining Q, while K b /K c is the primary control for resistive bridges (K b /K c r and K b /K c . The intra-clast flow distribution shifts outwards as A r increases. Conductive bridges promote this process and resistive bridges impede it." @default.
- W2485487760 created "2016-08-23" @default.
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- W2485487760 date "2016-10-01" @default.
- W2485487760 modified "2023-09-27" @default.
- W2485487760 title "Hydraulic bridges in unsaturated coarse granular media: Influence of bridge size and conductivity on flow through clasts" @default.
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- W2485487760 doi "https://doi.org/10.1016/j.advwatres.2016.07.014" @default.
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