Soil salinity

Visibly salt-affected soils on rangeland in Colorado. Salts dissolved from the soil accumulate at the soil surface and are deposited on the ground and at the base of the fence post.

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).^[1] 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.

^ Allaby, Michael, ed. (2019). "salinization". A Dictionary of Plant Sciences (fourth ed.). Oxford University Press. ISBN 978-0-19-883333-8 – via Oxford Reference.

[1] Allaby, Michael, ed. (2019). "salinization". A Dictionary of Plant Sciences (fourth ed.). Oxford University Press. ISBN 978-0-19-883333-8 – via Oxford Reference.

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Soil salinity

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