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Soil pH influences nutrient availability and uptake by altering the solubility of nutrients and toxic elements, with low pH leading to deficiencies in calcium, phosphorus, and nitrogen. Soil acidity is characterized by the dominance of hydrogen and aluminum ions, which can be measured through exchangeable and total acidity. Factors contributing to soil acidity include leaching, the use of acid fertilizers, and nutrient uptake by plants, particularly in regions with high rainfall.

Author

ngunoibrahim55

Language

EN