THE PROCESS OF SOIL SALINIZATION UNDER CHANGING GROUNDWATER LEVELS.
Abstract
Soil salinization is one of the most serious environmental and agricultural problems affecting irrigated lands worldwide. The fluctuation of groundwater levels plays a crucial role in the accumulation and redistribution of salts within the soil profile. This study analyzes the relationship between the depth of groundwater and the intensity of salinization processes in meadow and meadow-marsh soils. The findings highlight that shallow groundwater levels accelerate salt migration toward the root zone, resulting in reduced soil fertility and crop productivity. Conversely, lowering the groundwater table through drainage or improved irrigation management significantly mitigates salinization risks.
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