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Porosity reflects the capacity of soil to hold air and water, and permeability describes the ease of transport of fluids and their dissolved components.
Rocky desertification results in the reduction capacity of soil for water conservation.
Open image in new window Fig. 2 Effect of organic residue on phosphorus fixation capacity of soil.
High organic matter increases the water holding capacity of soil which may enhance the sporulation of AMF.
The nutrient supplying capacity of soil declines steadily under continuous and intensive cropping (Shukla et al. 2016).
An organic fertilizer does more than supplying organic nutrients: it improves the water and nutrient holding capacity of soil.
Similar(18)
Decades of acid deposition in these sensitive regions have depleted the acid-neutralizing capacity of soils.
Calcium, magnesium, sodium, and potassium, which are the base cations that account for most of the acid-neutralizing capacity of soils, are derived from the weathering of rocks and from wet and dry deposition.
The potential buffering capacity of soils in relation to the elements of plant nutrition.
The IWUE and Imax were related to available water holding capacity of soils.
Organic matter increases buffering and exchange capacity of soils and makes nutrient available to crops (McCauley et al. 2009).
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