| 格尔木冲洪积扇地下水锶物质流通量分析 |
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| 引用本文： | 王东胜,任福弘.格尔木冲洪积扇地下水锶物质流通量分析[J].地球科学,1995,20(4):469-473. |
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| 作者姓名： | 王东胜 任福弘 |
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| 作者单位： | 地矿部水文地质工程地质研究所 |
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| 摘 要： | 在分析格尔木含锶矿水田供锶环境和水迁移条件的基础上，将形成含锶矿水田的地质空间分为两个区：山区淋溶迁移区和平原迁移聚集区，运用物质流通量分析的观点，对锶的迁移聚集进行了系统分析，山区为锶矿水的形成提供了物质环境，平原区为锶矿水提供了贮存环境。
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| 关 键 词： | 地下水 物质流通量 格尔木 冲洪积扇 |
MASS FLUX ANALYSIS OF STRONTIUM IN THE ALLUVIAL AQUIFER OF GEERMU |
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| Wang Dongsheng.MASS FLUX ANALYSIS OF STRONTIUM IN THE ALLUVIAL AQUIFER OF GEERMU[J].Earth Science-Journal of China University of Geosciences,1995,20(4):469-473. |
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| Authors: | Wang Dongsheng |
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| Abstract: | The alluvial aquifer of Geermu is rich in strontium.Based on the analysis of origin and transportation of strontium in Geermu region,two subdivisions,namely the dissolution-transportation area in the Kunlun mountain and transportation-accumulation area in the Geermu alluvium are classified.Mass flux theory is applied for analysing the transportation and accumulation of strontium in the subdivisions.The result indicates that strontium which comes from the mountain area is accumulated in the Geermu alluvial aquifer. |
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| Keywords: | origin of strontium transportation and accumulation groundwater mass flux Geermu |
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