Factors Causing Land Degradation

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Understanding Land Degradation

Part of the book series: SpringerBriefs in Geography ((BRIEFSGEOGRAPHY))

Abstract

Land degradation, a decline in land quality caused by many factors, was a major global issue during the twentieth century and will continue to be so in the twenty-first century. Globally, around 3.2 billion people especially in rural communities are affected by land degradation. A number of factors cause land degradation. Among these are natural hazards such as heavy rainfall which cause soil erosion. Land degradation due to wind erosion is common in semi-arid and dry climates. Sandy soils and uncovered lands are prone to wind erosion. Land degradation tends to be common in areas where the topography is hilly and where there is no adequate cover. Unsuitable land use also causes land degradation. Soils in waterlogged alluvial plains or interior basins with restricted outward drainage of groundwater tend to be saline and such lands are less productive and degraded unless crops such as rice which can stand water logged conditions are cultivated. In many countries, steep slopes and mountain lands are cultivated by landless poor people who have limited resources to implement practices to control land degradation. Population growth; a lack of alternative avenues of livelihood, and inequity all contribute to land degradation.

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Notes

  1. 1.

    Inorganic fraction contains particles of different sizes. The smallest are clay particles having diameters of less than 0.002 mm. The next smallest are silt particles and have diameters between 0.002 mm and 0.05 mm. The largest are sand particles with diameters varying from 0.05 to 2 mm in diameter. For details on soils and its properties readers are referred to Nature and Properties of soils by Raymond R. Weil and Nyle C. Brady. ISBN: 978-0133254488.

  2. 2.

    Soil is made up of primary particles—sand, silt and clay. These particles are bound together into aggregates by the action of microorganisms mainly fungi. These aggregates vary in size that range from less than 0.25 mm in diameter to greater than 0.25 mm in diameter. Aggregates have different shapes such as granular, blocky, etc. Aggregates allow a soil to have pores spaces for air and water.

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Correspondence to Stanley Weeraratna .

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Weeraratna, S. (2022). Factors Causing Land Degradation. In: Understanding Land Degradation. SpringerBriefs in Geography. Springer, Cham. https://doi.org/10.1007/978-3-031-12138-8_2

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