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Sources of river water radiogenic strontium: examples from the Achaean granite dominated catchments of Swaziland

机译:河水放射性锶的来源:以斯亚兹兰阿契亚人花岗岩为主的流域的例子

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This study of the geochemistry of rivers draining the Archaean granite-gneissic terrains of Swaziland reports the first anomalous Sr-Sr-87/Sr-86 data for a river system outside the Himalayas. Both major cation and calcium mass balance approaches suggest that the source of the radiogenic high strontium load of Swaziland rivers is predominantly, or exclusively, silicate weathering. However, a compilation of bedrock compositional data for river catchments in Swaziland demonstrates that the uncertainties associated with these mass balance approaches are large and presently underestimated in global chemical weathering studies. Consideration of the strontium mass balance, based on silicate Na/Sr end member values, demonstrates the potential magnitude of the error involved. Importantly, a compilation of both the Na/Sr and Sr content of silicate rocks in Swaziland demonstrates that the general relationship between (Na/Sr)(sil) and Sr content is poor and that high silicate versus carbonate X/Sr end member values cannot be assumed to imply relatively lower Sr weathering yields from silicate rocks.
机译:这项对斯威士兰古生花岗岩-片麻岩地形排水的河流的地球化学研究报告了喜马拉雅山以外河流系统的第一个Sr-Sr-87 / Sr-86异常数据。阳离子和钙质量平衡的主要方法都表明,斯威士兰河的放射性高锶负载源主要或完全是硅酸盐风化。但是,对斯威士兰河流域的基岩成分数据的汇编表明,与这些质量平衡方法相关的不确定性很大,目前在全球化学风化研究中被低估了。基于硅酸盐Na / Sr末端元素值的锶质量平衡的考虑表明了所涉及误差的潜在幅度。重要的是,对斯威士兰硅酸盐岩的Na / Sr和Sr含量的汇编表明,(Na / Sr)(sil)和Sr含量之间的一般关系很差,并且高硅酸盐与碳酸盐X / Sr端值不能假定这意味着硅酸盐岩石的Sr风化率相对较低。

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