Soil salinity
Soil salinization happens when the salt content in soil increases above normal, naturally occurring levels
Soil salinity is the salt content in the soil; the process of increasing the salt content is known as salinization (also called salination in American English). Salts occur naturally within soils and water. Salinization can be caused by natural processes such as mineral weathering or by the gradual withdrawal of an ocean. It can also come about through artificial processes such as irrigation and road salt.
Natural occurrence
Salts are a natural component in soils and water bodies. The ions responsible for salinization are: Na+, K+, Ca2+, Mg2+ and Cl−.
Over long periods of time, as soil minerals weather and release salts, these salts are flushed or leached out of the soil by drainage water in areas with sufficient precipitation or under irrigation, or may rise through capillarity and accumulate near the surface under intense evaporation during drought periods. In addition to mineral weathering, salts are also deposited via dust and precipitation. Salts may accumulate in dry regions, leading to naturally saline soils. This is the case, for example, in large parts of Australia.
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This entry incorporates text from “Soil salinity” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.