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Point pedotransfer functions for estimating soil water retention curve

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Figure

Fig. 1. Soil textural classes considered for the UNSODA andGRIZZLY�databases�used�in�this�study.
Table 1, water content at inflection point was strongly
Fig. 3, with negative MR values, which is in agreement with
Fig. 3. H3, b – model H4, c – model H5 versus measured one (cm Estimated water content (cm3cm-3) using Rosetta: a – model3 cm-3)for�59�samples�of�the�GRIZZLY�data�set.

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