Abstract
Physical deterioration of soil involves the destruction of soil structure, dispersion of soil particles, sealing of pores, compression and increasing density, consolidation, compaction and reduced root penetration, low infiltration, waterlogging and runoff, and accelerated erosion. Along with denudation, these processes lead to desertification in the arid and semiarid regions. The ultimate result is the loss of the capacity to support ecosystems. There are about 68.3 M ha compacted soil globally which accounts for 4 % of human-induced soil degradation. Soil compaction is a global problem associated with mechanized agriculture. It has caused yield reductions of 25–50 % in some regions of Europe and North America and between 40 and 90 % in West African countries. Planned and integrated management involving reduced, conservation and timely tillage, generous addition of organic matter, mulching, crop rotation, subsoiling, and controlled trafficking are recommended for sustainable use of compacted soils. Desertification is a process of land degradation occurring mainly in the arid and semiarid regions due to human actions on ecosystems combined with adverse climatic conditions. The United Nations estimates that desertification affects 70 % of arid lands, amounting to about 30 % of the world cultivable land.
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Osman, K.T. (2014). Physical Deterioration of Soil. In: Soil Degradation, Conservation and Remediation. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-7590-9_2
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