Rare Earth Element Patterns in the Karst Terrains of Guizhou Province, China: Implication for Water/Particle Interaction | |
Han, Guilin1; Xu, Zhifang2; Tang, Yang1,3; Zhang, Guoping1 | |
刊名 | AQUATIC GEOCHEMISTRY
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2009-12-01 | |
卷号 | 15期号:4页码:457-484 |
关键词 | Karst Rare earth elements (REE) Water chemistry Water/particle interaction Y/Ho ratio |
ISSN号 | 1380-6165 |
DOI | 10.1007/s10498-009-9061-8 |
文献子类 | Article |
英文摘要 | The authors determine the concentrations of dissolved (< 0.22 mu m) rare earth elements (REE) and suspended particulate matter (SPM) of typical karst rivers in Guizhou Province, China during the high-flow period. The concentrations of acid-soluble REE extracted from SPM using diluted hydrochloric acid are also obtained to investigate water/particle interaction in the river water. The dissolved REE contents in the river water are extremely low in the rivers of the study. The dissolved REE distribution patterns normalized by the Post Archean Australia Shale (PAAS) in the karst rivers are not flat, show slight enrichment of heavy REE to light REE, and also have significant negative Ce and Eu anomalies. The acid-soluble REE appears to have similar distribution patterns as characterized by MREE enrichment and slight LREE depletion, with unremarkable Ce and Eu anomalies. The PAAS-normalized REE distribution patterns of SPM are flat with negative Eu anomalies. The contents and distribution patterns of REE in the SPM are closely related to the lithological character of the source rocks. The SPM contains almost all the REE produced in the process of surficial weathering. This demonstrates that particle-hosted REE are the most important form of REE occurrence. REE fractionation, which takes place during weathering and transport, leads to an obvious HREE enrichment in the dissolved loads relative to the SPM. Y/Ho ratio can be used to shed light on REE behaviors during water/particle interaction. |
WOS关键词 | PLASMA-MASS-SPECTROMETRY ; RIVER WATERS ; COLLOIDAL PARTICLES ; IONIC-STRENGTH ; FRESH-WATERS ; 1 ATM ; SEAWATER ; YTTRIUM ; CARBONATE ; FRACTIONATION |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | SPRINGER |
WOS记录号 | WOS:000271720200001 |
资助机构 | Chinese Academy of Sciences(KZCX2-YW-306) ; Chinese Academy of Sciences(KZCX2-YW-306) ; Chinese National Natural Science Foundation(40673010 ; Chinese National Natural Science Foundation(40673010 ; 40721002) ; 40721002) ; Chinese Academy of Sciences(KZCX2-YW-306) ; Chinese Academy of Sciences(KZCX2-YW-306) ; Chinese National Natural Science Foundation(40673010 ; Chinese National Natural Science Foundation(40673010 ; 40721002) ; 40721002) ; Chinese Academy of Sciences(KZCX2-YW-306) ; Chinese Academy of Sciences(KZCX2-YW-306) ; Chinese National Natural Science Foundation(40673010 ; Chinese National Natural Science Foundation(40673010 ; 40721002) ; 40721002) ; Chinese Academy of Sciences(KZCX2-YW-306) ; Chinese Academy of Sciences(KZCX2-YW-306) ; Chinese National Natural Science Foundation(40673010 ; Chinese National Natural Science Foundation(40673010 ; 40721002) ; 40721002) |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/70304] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Han, Guilin |
作者单位 | 1.Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550002, Guizhou, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 3.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China |
推荐引用方式 GB/T 7714 | Han, Guilin,Xu, Zhifang,Tang, Yang,et al. Rare Earth Element Patterns in the Karst Terrains of Guizhou Province, China: Implication for Water/Particle Interaction[J]. AQUATIC GEOCHEMISTRY,2009,15(4):457-484. |
APA | Han, Guilin,Xu, Zhifang,Tang, Yang,&Zhang, Guoping.(2009).Rare Earth Element Patterns in the Karst Terrains of Guizhou Province, China: Implication for Water/Particle Interaction.AQUATIC GEOCHEMISTRY,15(4),457-484. |
MLA | Han, Guilin,et al."Rare Earth Element Patterns in the Karst Terrains of Guizhou Province, China: Implication for Water/Particle Interaction".AQUATIC GEOCHEMISTRY 15.4(2009):457-484. |
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