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西江上游河水悬浮物中稀土元素的地球化学特征
Rare-earth Elements(REEs)of the Suspended Particulate Matter in the Upper Reaches of the Xijiang River

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谢雯 1   徐志方 2 *   刘丛强 1  
文摘 采用改进的BCR逐级提取法和ICP-MS测试技术,对西江上游河流悬浮物中稀土元素进行了研究.结果表明:河流悬浮物稀土元素总量的含量变化范围在188~402mg/kg之间,并主要来源于流域内岩石的风化,反映了源区的物质特征.西江上游河水悬浮物中三种非稳定态(即酸可提取态、铁锰氧化物结合态和有机物硫化物结合态)稀土元素页岩(PAAS)标准化配分模式均显示出中稀土富集的特征. 这种配分模式可能是由于流域内广布的海相沉积岩中磷酸盐矿物的风化所造成的.稳定态(即残渣态)的配分曲线较为平直,没有体现出明显的稀土分异.悬浮态稀土各赋存形态含量的顺序为:残渣态>有机物硫化物结合态、铁锰氧化物结合态>酸可提取态.中稀土元素Sm、Eu、Gd相对于轻、重稀土元素的稳定态所占比例偏低,而相对于三种非稳定态所占比例偏高,反映了其潜在的地球化学活性
其他语种文摘 The rare-earth elements(REEs)of suspended particulate matter(SPM)in the upper reaches of the Xijiang River were measured by inductively coupled plasma mass spectrometry(ICP-MS)after improving the BCR sequential extraction method. The result showed that the total REE concentrations of SPM are obviously higher than those of dissolved load, ranging from 188~402mg/kg. The PAAS-normalized REE patterns for the three unstable fractions of REEs(AEC, bound to Fe-Mn oxides, bound to organic matter)exhibit middle REEs(MREEs)enrichment, indicating the preferential weathering of phosphatic minerals. The stable fraction of REEs(residual)presents a flat PAAS-normalized REE pattern, indicating no significant fractionation of REE in residual form. The percentage of four fractions of SPM obeys the following order:residual> bound to organic matter, bound to Fe-Mn oxides>AEC.The MREEs(Sm,Eu,Gd)have relatively lower percentages in the residual fraction and higher in other three unstable fractions
来源 地球与环境 ,2010,38(4):414-420 【核心库】
关键词 西江上游 ; 稀土元素 ; 悬浮物
地址

1. 中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵州, 贵阳, 550002  

2. 中国科学院地质与地球物理研究所, 北京, 100029

语种 中文
文献类型 研究性论文
ISSN 1672-9250
学科 地质学;环境科学基础理论
基金 国家973计划 ;  国家自然科学基金
文献收藏号 CSCD:4108310

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引证文献 2

1 李景喜 热带海洋生物稀土元素生态化学特征分析研究 分析化学,2016,44(10):1539-1546
CSCD被引 1

2 赵兴媛 黔中小流域水体悬浮物与沉积物微量元素地球化学特征及物源指示 地球化学,2012,41(3):250-265
CSCD被引 5

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