Abstract
Soil salinity (the readily soluble salts present in the soil; essentially the inorganic electrolytes contained in the soil solution) can be determined or estimated from measurements made: (1) on aqueous extracts of soil samples; (2) on samples of soil water, per se, obtained from the soil; (3) in situ using either buried porous salinity sensors which imbibe and equilibrate with soil water or four-electrode probes or time domain reflectometric electrode systems, and (4) remotely using electromagnetic induction electrical conductivity sensors.
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Rhoades, J.D., Frenkel, H. (1984). Diagnostic Criteria and Methodology. In: Shainberg, I., Shalhevet, J. (eds) Soil Salinity under Irrigation. Ecological Studies, vol 51. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-69836-1_5
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