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'Permanent wilting point' ('PWP') or 'wilting point' ('WP') is defined as the minimum soil moisture at which a plant wilts and can no longer recover its turgidity when placed in a saturated atmosphere for 12 hours. The physical definition of the wilting point (symbolically expressed as θ_pwp or θ_wp) is defined as the water content at −1500 J/kg (or −15 bars) of suction pressure, or negative hydraulic head.
However, it is noted that the PWP values under field conditions are not constant for any given soil, but are determined by the integrated effects of plant, soil and atmospheric conditions.

Contents

History

References

See also

History

The concept was introduced in the early 1910s. Lyman Briggs and Homer LeRoy Shantz (1912) proposed the wilting coefficient, which is defined as ''the percentage water content of a soil when the plants growing in that soil are first reduced to a wilted condition from which they cannot recover in approximately saturated atmosphere without the addition of water to the soil''. See pedotransfer function for wilting coefficient by Briggs.
Frank Veihmeyer and Arthur Hendrickson from University of California-Davis found that it is a constant (characteristic) of the soil and is independent of environmental conditions. Lorenzo A. Richards proposed it is taken as the water content at −1500 J/kg.^[1]

References

1. Soil moisture at permanent wilting of plants, Veihmeyer, F.J. and Hendrickson, A.H., , , Plant Physiol., 1928

See also

★ Available water capacity

★ Field capacity

★ Moisture equivalent

★ Moisture stress

★ Nonlimiting water range

★ Soil plant atmosphere continuum