Soil salinity (the content of salts in soil) and salinization (an increase of salinity due to various reasons) is one of the most common forms of soil degradation and is considered to be a major cause of desertification. This problem has been intensified by climate change with rising temperatures and decrease of precipitation.
Soil salinity occurs when water-soluble salts accumulate in or near the upper horizons of the soil. These salts contain K+, Mg+, Ca+, Cl–, SO42-, CO32-, HCO3– and Na+ ions (mostly these salts are sodium chlorides and sodium sulphates). When soils accumulate the exchangeable sodium, this process is called sodification. If Mg+ and Ca2+ ions are accumulated in the soil, an alkalization process takes place and the soil becomes alkaline (with a pH above 8.5).
As a result of salinization, soil structure degrades and is more exposed to water and wind erosion, soil compaction, soil crust formation, soil desertification, soil fertility decreases, agronomic productivity decrease, the soil buffering capacity against pollution decreases, plant nutrient uptake is impaired, soil biota biodiversity is reduced and also groundwater quality is affected.
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