ISSN:
1440-1703
Keywords:
Arid highland soils
;
CaCO3
;
Humidity index
;
Nutrients
;
Tibet
Source:
Springer Online Journal Archives 1860-2000
Topics:
Biology
Notes:
Abstract A variety of soil studies were carried out along a 920-km transect running SE to NW from near the border with northern Nepal, through the Western Tibet Highlands (soils sampled at six locations at an elevation of about 4200 m), to the Takla Makan Desert. This transect, which parallels the China-India border, covers a range of aridities. Annual precipitation decreased exponentially (from 169 mm to ca. 50 mm) north-westwards along the transect. The humidity index also decreased exponentially to the desert zone in the Western Tibet Highlands, and decreased further in the Takla Makan Desert because of the high temperature in the latter area. Vegetation changed fromCaragana thorn-bush steppe, throughArtemisia sparse steppe, to desert. Soil properties were studied in relation to the humidity index. Organic C, total N, cation exchange capacity, and very low C/N ratio values (a maximum of 12.8) of soils decreased with the decrease in humidity index. In contrast, carbonate, pH (KCl), and sulfate increased exponentially. Available P and ammonia content were inversely related to the abundance of carbonate, whereas nitrate increased where carbonate was abundant. Illite was the most abundant of the clay minerals, followed in order by kaolinite and montmorillonite.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/BF02347154
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