Titlebook: Applied Soil Physics; Soil Water and Tempe Ronald J. Hanks,Gaylen L. Ashcroft Textbook 19801st edition Springer-Verlag Berlin Heidelberg 19

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Springer-Verlag Berlin Heidelberg 1980

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Water Potentials,lude that soil water content is not sufficient to specify the entire status of water in soil. Some of the observations that cause us to believe that there is a need to define some other property associated with soil water are:

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Water Flow in Soil,al is plotted as a function of depth, it results in a smooth curve even across the boundary between layers (see Fig. 3.1 A). When water content is plotted as a function of depth, there is normally a sharp discontinuity in the curve at the boundary between layers (see Fig. 3.1 B).

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