Abstract
Western Rajasthan (part of Indian arid zone) is located between the 24° 0′ to 30° 05′ N latitudes and 70° 0′ to 75° 42′ E longitudes, to the west of Aravalli mountains, extending up to the Thar desert of Pakistan. It covers nearly 233 100 sq km area of Rajasthan State. Like other hot deserts of the world, a considerable part of the Rajasthan desert is comprised of saline unproductive land, in the form of saline lakes, salt depressions, swamps and saline lands covered by desert wind blown sand. Such salt basins are the main characteristic feature of the hot deserts, where évapotranspiration exceeds rainfall.
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Sen, D.N., Rajpurohit, K.S., Wissing, F.W. (1982). Survey and adaptive biology of halophytes in western Rajasthan, India. In: Sen, D.N., Rajpurohit, K.S. (eds) Contributions to the ecology of halophytes. Tasks for vegetation science, vol 2. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-8037-2_5
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DOI: https://doi.org/10.1007/978-94-009-8037-2_5
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