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- W2012808873 abstract "Laboratory observations of the redistribution of water and solute, following one‐dimensional and three‐dimensional constant flux infiltration, reveal distinctly different patterns of water and chemical transport. The geometry‐induced enhancement of capillarity over gravity in three dimensions is thought responsible for the rapid attainment during redistribution of a near‐constant water content θ*, some radial distance r around the dripper. This renders simple the prediction of the maximum radial extent of convective solute redistribution, r *. Nevertheless, molecular diffusion about r * is the dominant mode of solute transport during the weak convective redistribution in three dimensions." @default.
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- W2012808873 date "1991-08-01" @default.
- W2012808873 modified "2023-09-25" @default.
- W2012808873 title "Redistribution of Water and Solute Following Infiltration From a Surface Drip Source" @default.
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