Process / pipelineSoil Hydrology

Soil Moisture Curve

The soil moisture curve (or soil water retention curve, SWRC) describes the relationship between soil water content and soil matric potential (water tension). It characterizes how tightly water is bound in pores of different sizes: large pores drain at low tensions (wet soils), while smaller pores retain water at high tensions (dry soils). Quantifying this relationship is essential for water balance modeling, unsaturated flow prediction, and assessing plant-available water.

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Sources

  1. Gardner, W. R. (1956). Representation of soil aggregate-size distribution by a logarithmic-normal distribution. Soil Science Society of America Journal, 20(2), 151-153. DOI: 10.2136/sssaj1956.03615995002000020003x
  2. Brooks, R. H., & Corey, A. T. (1964). Hydraulic properties of porous media. Hydrology Papers No. 3, Colorado State University, Fort Collins. link
  3. van Genuchten, M. T. (1980). A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Science Society of America Journal, 44(5), 892-898. DOI: 10.2136/sssaj1980.03615995004400050002x

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Referenced by

ScholarGateSoil Moisture Curve (Soil Water Retention Curve (Soil Moisture Characteristic Curve)). Retrieved 2026-06-04 from https://scholargate.app/en/agronomy/soil-moisture-curve