Effects of topography and vegetation on distribution of rare earth elements in calcareous soils

Springer Science and Business Media LLC - Tập 36 - Trang 469-473 - 2017
Zhaoliang Song1, Yuntao Wu1, Xiaomin Yang1, Zijuan Xu1, Linan Liu1, Xiaodong Zhang1, Qian Hao1, Shaobo Sun2, Guilin Han3, Congqiang Liu1,4
1Institute of the Surface-Earth System Science Research, Tianjin University, Tianjin, China
2State Key Laboratory of Resources and Environment Information System, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
3School of Water Resources and Environment, China University of Geosciences (Beijing), Beijing, China
4State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China

Tóm tắt

This study investigated the impact of topography and vegetation on distribution of rare earth elements (REEs) in calcareous soils using methods of single extraction and mass balance calculation. The purposes of the study were to set a basis for further research on the biogeochemical REE cycle and to provide references for soil–water conservation and REE-containing fertilizer amendments. The results show a generally flat Post-Archean Average Australian Shale—normalized REE pattern for the studied calcareous soils. REE enrichment varied widely. The proportion of acid-soluble phases of heavy REEs was higher than that of light REEs. From top to bottom of the studied hills, dominant REE sources transitioned from limestone in-situ weathering to input from REE-containing phases (e.g., clay minerals, amorphous iron, REE-containing fluids). Our results indicate that the REE content of calcareous soils is mainly controlled by slope aspect, while the enrichment degree of REEs is related to geomorphological position and vegetation type. Furthermore, the proportion of acid-soluble phases of REEs is mainly controlled by geomorphological position.

Tài liệu tham khảo

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