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126                                          5  Chemical Soil Degradation


            Table 5.1  Global extent of soil degradation (M ha) by loss of nutrients, salinization, and acidification
            Regions          Loss of nutrients  Salinization  Acidification  Total
            Africa           65                15           1              62
            Asia             15                53           4              72
            South America    68               2             −              70
            Central America  4                2             −              6
            North America    −                +             +              +
            Europe           3                4             +             26
            Oceania          +                1             −             1
            World            136              77            6             229
            Data extracted from Oldeman (1994)


            of degraded soils are due to chemical degradation. In North America and Oceania,
            chemical degradation of soil is of little concern. Loss of nutrients is the major
            type of chemical soil degradation in Africa and South America, while salinization
            is the major type of soil chemical degradation in Asia. Chemical soil degradation is
            mainly caused by agricultural mismanagement (56 %) and deforestation (28 %)
            (Oldeman 1994). Table 5.1 shows the global extent of chemical degradation of soil.



            5.2  Loss of Nutrients and/or Organic Matter


            Although it is said that the loss of nutrients is a problem with low-input agriculture,
            it also occurs in several other situations. It may occur if agriculture is practiced on
            poor or moderately fertile soils, without sufficient application of manure and fertilizers.
            The rapid loss of organic matter and nutrients of the topsoil occurs due to clearing
            of the natural vegetation. Burning of biomass, shifting cultivation, and erosion are
            other important causes of loss of nutrients and organic matter. Human- induced soil
            nutrient depletion is the process by which the soil nutrient stock is shrinking due to
            continuous nutrient mining without sufficient replenishment of nutrients harvested
            in agricultural products and of nutrient losses by accelerated soil erosion and leaching
            (Tan et al. 2005). Natural erosion and leaching are exacerbated by human actions
            for the exploitation of vegetation and soil resources. The general cause of fertility
            depletion is a negative balance between output (through harvesting, burning,
            leaching, etc.) and input (through manure and fertilizers, returned crop residues,
            flooding, etc.) of nutrients and organic matter. The nutrient balance situations in some
            African countries are cited as an example below. International Fertilizer Development
            Center (IFDC) conducted some studies of soil nutrient balances in some African
            countries. The methodological approach to estimate nutrient balances, depletion
            rates, and requirements combines information on agricultural production, soil
            characteristics, and biophysical constraints with methods and procedures designed
            for making such estimates (Henao and Baanante 1999). The information and data
            related to agricultural production included land use, population- supporting capacity
            of land, crop production, and use of mineral and organic fertilizers. The approach
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