Tohid Nooralvandi Soil becomes acidic and saline due to various natural and human-induced factors. Acidic soils are mainly caused by the leaching of basic nutrients such as calcium and magnesium, especially in areas with heavy rainfall. The continuous use of acid-forming fertilizers like ammonium sulfate and urea also contributes to soil acidity. Additionally, the decomposition of organic matter produces organic acids, and in some cases, the parent rock material itself is naturally acidic. On the other hand, saline soils develop due to poor drainage and high evaporation, which lead to the accumulation of salts on the soil surface. Irrigating with saline water, excessive use of chemical fertilizers, and the upward movement of groundwater containing dissolved salts also contribute to soil salinity.
To prevent and treat acidic soils, farmers can apply agricultural lime (calcium carbonate) to neutralize the acidity and improve soil pH. Proper nutrient management through balanced fertilization and the addition of organic matter like compost can help stabilize the soil. Acid-tolerant crops may also be planted when liming is not feasible. For saline soils, improving drainage is essential to allow salts to be flushed below the root zone. Using clean, non-saline irrigation water and applying gypsum (calcium sulfate) can help replace harmful sodium ions and improve soil structure. Additionally, adopting crop rotation with salt-tolerant crops and avoiding over-irrigation and fertilizer misuse are effective practices to manage and rehabilitate saline soils.