Abstract
Soil fertility is a measure of the ability of soil to sustain satisfactory crop growth in the long-term, and can be determined by physical, chemical and biological processes intrinsically linked to soil organic matter content and quality (Fig. 7.1). Given that a decrease in soil fertility is a major constraint to productivity, investing in practices leading to soil fertility enhancement is likely to generate large returns (Syers 1997). In recent years, increased concerns for healthy food production and environmental quality, and increased emphasis on sustaining the productive capacity of soils, have raised interest in the maintenance and improvement of soil organic matter through appropriate land use and management practices (Loveland and Webb 2003; Puget and Lal 2005; Whitbread et al. 2003).
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Singh, B., Rengel, Z. (2007). The Role of Crop Residues in Improving Soil Fertility. In: Marschner, P., Rengel, Z. (eds) Nutrient Cycling in Terrestrial Ecosystems. Soil Biology, vol 10. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-68027-7_7
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