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• W1973670398 abstract "It is known well that macropores such as shrinkage cracks give effective pathways for water movement in agricultural fields. However, models for such phenomena have not been completely successful as yet. In this paper, a quantitative description of water movement towards a drain pipe in a clayey agricultural field including shrinkage cracks is discussed in order to evaluate the role of cracks on water movement. In the evaluation, cracks are treated as a network spreading widely in the entire field, and characteristics of water flow through the crack network in the whole field are estimated from hydrological properties of pipe drainage from the field. Drain flow resulting from flow of water through a crack network can be well described by equations derived from Darcy's law. Hydraulic conductivities of the field with cracks are estimated to be of the order of 10−4 m/s in spite of very low permeability of soil matrix of the field (10−8 to 10−9 m/s)." @default.
• W1973670398 created "2016-06-24" @default.
• W1973670398 creator A5077678787 @default.
• W1973670398 date "1993-11-01" @default.
• W1973670398 modified "2023-09-26" @default.
• W1973670398 title "Lateral water flow in a clayey agricultural field with cracks" @default.
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• W1973670398 doi "https://doi.org/10.1016/0016-7061(93)90076-w" @default.
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