The mechanism by which the degradation of soil structure in sodic soil occurs are the swelling of the clays and the dispersion of the colloids, and the classic approach to improve the soil structure in sodic soil is by adding a source of calcium (this is a chemical approach based upon exchange phenomena which is reversible in theory, even in practice ) but what about the physical aspects of the improvement of soil structure (porosity, saturated hydraulic conductivity), are these properties reversible or not ?

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