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The higher pH of sodic soils results in nutrient imbalance stress in crop production by affecting bioavailability of phosphorus, iron, copper, boron and zinc ( than H + ) the activity of the OH ions comes into play, increasing alkalinity at pHs greater than 11, whereas below pH 11 forms of carbonates are responsible for alkalinity (Whipker et al., 1996)

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the periosteum, vascular supply between the muscle and periosteum, and the interconnections between muscle and bone were damaged and disrupted