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Sample text
The process involves the degradation, in arid, semi-arid and dry sub-humid areas, of fertile lands capable of sustaining vegetation and various organisms, to “dead” lands. The new deserts are not necessarily hot, dry, sandy places; instead, they are any areas where the soil has been so mistreated by humans that it is now useless for growing crops. It usually occurs near arid regions, in a transitional zone between desert and the surrounding or peripheral areas. These transition zones have very fragile, delicately balanced ecosystems that support vegetation.
2002). Transient salinity and subsoil constraints to dryland farming in Australian sodic soils: an overview. Aust J Exp Agric, 42, 351–361. UNEP (United Nations Environment Program) (2007). Environment for Development, Global Desert Outlook. asp, accessed 30 September 2007). Further reading Colley, C. C. (1983). The desert shall blossom: North African influence on the American Southwest. W Historical Q, 14, 277–290. , & Vel´azquez, E. (2006). Virtual water and water trade in Andalusia. A study by means of an input–output model.
UNEP (United Nations Environment Program) (2007). Environment for Development, Global Desert Outlook. asp, accessed 30 September 2007). Further reading Colley, C. C. (1983). The desert shall blossom: North African influence on the American Southwest. W Historical Q, 14, 277–290. , & Vel´azquez, E. (2006). Virtual water and water trade in Andalusia. A study by means of an input–output model. Universities of Groningen and Pablo de Olavide, New York, NY. Gat, J. R. (1979). Isotope hydrology of very saline surface waters, Isotopes in Lake Studies (pp.