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Intrinsic Relationship between Matric Potential and Cation Hydration

Exchangeable cations are important in water sorption, hydraulic conductivity, swelling, flocculation–deflocculation, and fertility. Intrinsic relationship exists between matric potential and cation hydration at very low water contents. Proposed model predicts soil water content at low matric potentials for different exchangeable cations in soil. Model is applicable for soil water retention models and quantification of different types of exchangeable cations.