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Behaviours of REE and Other Trace Elements During Pedological Weathering-Evidence from Chemical Leaching of Loess and Palaeosol from the Luochuan Section in Central China
引用本文:Chen Jun,Wan Hongtao,Department of Earth Sciences,Nanjing University,Nanjing,Jiangsuand Lu HuayuKey Lab. of Loess and Quaternary Geology,Chinese Academy of Sciences,Xi an,Shaanxi Liu Xinzhu. Behaviours of REE and Other Trace Elements During Pedological Weathering-Evidence from Chemical Leaching of Loess and Palaeosol from the Luochuan Section in Central China[J]. 《地质学报》英文版, 1996, 70(3): 290-302. DOI: 10.1111/j.1755-6724.1996.mp9003006.x
作者姓名:Chen Jun  Wan Hongtao  Department of Earth Sciences  Nanjing University  Nanjing  Jiangsuand Lu HuayuKey Lab. of Loess and Quaternary Geology  Chinese Academy of Sciences  Xi an  Shaanxi Liu Xinzhu
作者单位:Chen Jun,Wan Hongtao,Department of Earth Sciences,Nanjing University,Nanjing,Jiangsuand Lu HuayuKey Lab. of Loess and Quaternary Geology,Chinese Academy of Sciences,Xi an,Shaanxi Liu Xinzhu
摘    要:The chemical leaching method is used for a systematic analysis of distribution characteristics of acid-soluble and acid-insoluble REE and other trace elements from the Luochuan loess deposits. The study shows that the acid-insoluble phase in loess and palaeosol is a stable component of old aeolian dusts and is characteristic of the provenance; the acid-soluble phase is the unstable component in the weathering pedogenic process and reflects rock-forming features after accumulation of aeolian dusts. The acid-insoluble REE and acid-soluble Sr and Pb can be used as geochemical indicators respectively to trace the provenance characteristics and the weathering pedogenic process.


Behaviours of REE and Other Trace Elements During Pedological Weathering-Evidence from Chemical Leaching of Loess and Palaeosol from the Luochuan Section in Central China
Chen Jun,Wan Hongtao. Behaviours of REE and Other Trace Elements During Pedological Weathering-Evidence from Chemical Leaching of Loess and Palaeosol from the Luochuan Section in Central China[J]. Acta Geologica Sinica (English Edition), 1996, 70(3): 290-302. DOI: 10.1111/j.1755-6724.1996.mp9003006.x
Authors:Chen Jun  Wan Hongtao
Affiliation:Chen Jun,Wan Hongtao,Department of Earth Sciences,Nanjing University,Nanjing,Jiangsuand Lu HuayuKey Lab. of Loess and Quaternary Geology,Chinese Academy of Sciences,Xi an,Shaanxi Liu Xinzhu
Abstract:The chemical leaching method is used for a systematic analysis of distribution characteristics of acid-soluble and acid-insoluble REE and other trace elements from the Luochuan loess deposits. The study shows that the acid-insoluble phase in loess and palaeosol is a stable component of old aeolian dusts and is characteristic of the provenance; the acid-soluble phase is the unstable component in the weathering pedogenic process and reflects rock-forming features after accumulation of aeolian dusts. The acid-insoluble REE and acid-soluble Sr and Pb can be used as geochemical indicators respectively to trace the provenance characteristics and the weathering pedogenic process.
Keywords:chemical leaching   loess and palaeosol   REE geochemistry   provenance characteristics   weathering pedogenesis
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