Determination of the Soil Water Retention Curve around the Wilting Point: Optimized Protocol for the Dewpoint Method

Abstract

Core Ideas Soil water retention curve over the entire moisture range with high accuracy. Combination of evaporation method and dewpoint method. No a priori knowledge on soil texture needed. Experimental methodology that is reliable, efficient, and easy to use. Accurate knowledge of the soil water retention curve (WRC) is essential for various hydrological and plant‐physiological studies. Currently, there is a lack of a uniform protocol for measuring the wilting point water content (WP) with the dewpoint method (DP), despite its ecological relevance and frequent use to calculate available water capacity. We present a new protocol for measuring the WP with the dewpoint method. In contrast to existing methods which add or remove specific amounts of water to moist, air‐dry, or oven‐dry soil, we propose to apply the dewpoint method after the evaporation method in which tensiometers measure the pressure head of the soil. We suggest to stop the evaporation experiment when the air‐entry of one tensiometer cup is reached, to slice the soil core into slabs, and to apply the dewpoint method to subsamples of the slabs. We test the method by numerical simulations and laboratory experiments on five soils covering a broad range of texture. We investigate the accuracy, robustness, and practicability of the new method and compare it to the existing protocols for the dewpoint method and the pressure plate technique. We find that the proposed method allows a precise determination of the WP and the WRC across the full moisture range. It is easy to perform, robust, accurate, and does not require any a priori guess about the amount of water to be added or removed. By fitting a retention curve to the measured data, any water content, including the WP, can be obtained with great confidence.