| 汾河泥沙变化研究 |
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| 引用本文： | 梁述杰,贾小军. 汾河泥沙变化研究[J]. 山西水利科技, 2004, 0(1): 47-49 |
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| 作者姓名： | 梁述杰 贾小军 |
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| 作者单位： | 山西省水文水资源勘测局 |
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| 摘 要： | 分析汾河流域实测泥沙资料，认为汾河水流的泥沙含量是比较大的，统计证明汾河流域水量和沙量同步减少，而且沙量的减少远远大于水量的减少。原因是降水量减少、水库拦沙、水土保持措施、河道淤积等多方面影响因素共同作用所致。
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| 关 键 词： | 汾河流域 泥沙 径流量 含沙量 降水量 水土保持 |
| 文章编号： | 1006-8139(2004)01-47-03 |
| 修稿时间： | 2003-09-11 |
Research on The Sediment Change of Fen River |
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| Liang Shujie Jia Xiaojun. Research on The Sediment Change of Fen River[J]. Shanxi Hydrotechnics, 2004, 0(1): 47-49 |
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| Authors: | Liang Shujie Jia Xiaojun |
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| Affiliation: | Liang Shujie Jia Xiaojun |
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| Abstract: | After analyzing the practical sediment data of Fen River,a conclusion that the sediment content in the water of Fen River is high has been drawn. The statistics proves that the sediment and water in Fen river basin decreases in the same degree, and the sediment decreases much more than that of water. The reasons that lead to these phenomena are the decrease of precipitation amount, water and soil conservation etc. |
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| Keywords: | sediment characteristic runoff amount sediment content precipitation amount water and soil conservation |
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