Summary
In almost all conditions in the field, transport of soluble salts in soils results from movement (convection) of the soil solution as a whole, and molecular diffusion within the soil solution.
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© 1971 Australian Academy of Science
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Peck, A.J. (1971). Transport of Salts in Unsaturated and Saturated Soils. In: Talsma, T., Philip, J.R. (eds) Salinity and Water Use. Palgrave Macmillan, London. https://doi.org/10.1007/978-1-349-01391-3_7
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DOI: https://doi.org/10.1007/978-1-349-01391-3_7
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