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[FIGURE 1 OMITTED] [FIGURE 2 OMITTED] [FIGURE 3 OMITTED] Field capacity and wilting points are relatively static in nature and denote only the end points of the soil water characteristic curve over the range of which soil water is available to plants.
2003), but most have concentrated on the prediction of the soil water characteristic curve and the saturated hydraulic conductivity for rigid (non-swelling) soils.
Goodness-of-fit for both the soil water characteristic curve and the shrink swell relationships was defined in terms of the root mean square error (RMSE), which is defined as: (3) [MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] where Nd is the number of datapoints, [[?