ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
赣南小流域水体中稀土元素的地球化学特征
  
关键词:water in southern Jiangxi Province  REE  dissolution form  distribution  fractionation
基金项目:国家自然科学基金项目(编号:40473051,40232002)
作者单位E-mail
罗建美 石家庄经济学院资源学院,河北石家庄050031 luojm3003@126.com 
季宏兵 首都师范大学资源环境与旅游学院首都圈生态环境过程重点实验室,北京100037  
霍永伟 河北省国土资源利用规划院,河北石家庄050051  
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摘要:
Geochemical Characteristics of Rare Earth Elements in the Water Body of the Ganjiang River, Southern Jiangxi
      Concentrations of dissolved rare earth elements(DREE) were measured in the upper reaches of the Ganjiang River in southern Jiangxi Province.The authors analyzed the distribution and fractionation of DREE in the water,and discussed the origins of the rare earth elements(REE) signatures.The results show that Ce has negative anomalies in the valley of southern Jiangxi,suggesting less mobilization of Ce in the weathering profile.The water controlled by natural weathering has no obvious REE fractionation except for Ce and Eu.The positive Eu anomalies in this area are mainly determined by the preferential dissolution of Eu-enriched minerals.The DREE in the water affected by the evaporable salt deposit are lowly fractionated in comparison with those in the natural settings.The heavy REE(HREE)-enriched negative Eu anomalistic patterns in the water body affected by rare earth deposit have inherited characteristics of the weathering crust.Middle REE(MREE)-enriched negative Eu anomalistic patterns in the mainstream water are probably related to anthropogenic factors.
LUO Jian-mei,JI Hong-bin,HUO Yong-wei.2007.Geochemical Characteristics of Rare Earth Elements in the Water Body of the Ganjiang River, Southern Jiangxi[J].Acta Geoscientica Sinica,28(5):438-445.
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