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A discussion on the geochemical features and origin of selenium-rich soil on the northern slope of the Tianshan Mountains from Urumqi to Shawan County |
WEI Zhen-Shan1,2, TU Qi-Jun3,4, TANG Shu-Hong1, WANG Hua-Bing1, ZHAO Xue-Jiao1, BAI Jin-Qi1 |
1. No.1 Hydrology & Engineering Geology Department, Xinjiang Bureau of Geology and Mineral Resources, Urumqi 830091, China;
2. School of Geology and Mining Engineering, Xinjiang University, Urumqi 830047, China;
3. Xinjiang Institute of Geological Survey, Urumqi 830000, China;
4. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China |
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Abstract Based on the multi-purpose regional geochemical survey, the authors discovered a large area of selenium-rich soils on the north slope of the Tianshan Mountains in Xinjiang from Urumqi to Shawan County. The selenium content is relatively high, and a variety of fertile elements are rich. The study shows that the selenium is mostly distributed in the surface soil and exhibits the positive correlation with the organic content. It is indicated that the selenium originates in parent soil materials while the enrichment state of selenium depends on the supergene geochemical circumstance of local fluvio-lacustrine deposits.
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Received: 08 January 2016
Published: 10 October 2016
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