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- W1584395184 abstract "The knowledge on water behavior in soils as well as successful water management practices are based on a proper understanding of the soil hydraulic functions and characteristics. These are the soil water retention curve (SWRC), saturated hydraulic conductivity, unsaturated hydraulic conductivity as a function of the soil water content, or of the soil water potential, and soil water diffusivity as a function of the soil water content. Water at hydrostatic equilibrium, the flow of water and transport of chemical solutions, all of these are realized in the porous space of the soil. The chapter presents a discussion on the soil porous system in Vertisols, especially with regard to its dynamics as the reaction to volumetric changes of Vertisols related to the soil water content change. Normal and residual swelling or shrinkage in the field soil cause rising or sinking of the topographical surface. The upward or downward shift of the soil has been observed at depths greater than 2 m when the surface was ponded by water for a very long period. The system of micropores depends predominantly on the development of the soil structure. Peds are separated from the adjoining peds by natural surfaces of weakness. When the principle of the representative elementary volume (REV) is applied to the studied volume of soil, distinct multimodal porous systems should be obtained." @default.
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- W1584395184 date "1996-01-01" @default.
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- W1584395184 title "Chapter 6 Water relations and water management of vertisols" @default.
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- W1584395184 doi "https://doi.org/10.1016/s0166-2481(96)80008-0" @default.
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