| 试论悬河补给—悬河的类型及其成因 |
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| 引用本文： | 周宏春 哈承佑. 试论悬河补给—悬河的类型及其成因[J]. 水文地质工程地质, 1993, 20(6): 20-23 |
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| 作者姓名： | 周宏春 哈承佑 |
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| 作者单位： | 地矿部环境地质研究所，地矿部环境地质研究所 北京 100081，北京 100081 |
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| 摘 要： | 文中依据我国西北干旱地区广泛发育悬河这一现象,从地表水—地下水转化和河水位—地下水位关系的角度出发,讨论了悬河的定义,划分了松散层上发育的悬河类型;从河床下非饱和带的介质组成和结构、水动力学条件和外界影响等三个方面探讨了悬河的成因。
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| 关 键 词： | 悬河 类型 形成条件 |
Types of suspended rivers and their formation concitions |
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| Zhou Hongchun et al. Types of suspended rivers and their formation concitions[J]. Hydrogeology and Engineering Geology, 1993, 20(6): 20-23 |
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| Authors: | Zhou Hongchun et al |
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| Affiliation: | Zhou Hongchun et al |
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| Abstract: | The suspended rivers which are widespread in the arid zone of northwestern China are defined from the viewpoint of the surface water/groundwater transformation and the correlation between the river water level and groundwater level. The suspended rivers in the unconsolidated media are divided into different types. The formation conditions of suspended rivers are explored in the light of the composition and structures of the media in the unsaturated zone beneath the riverbed, the hydrodynamic condition and the influence to the groundwater system from outside. |
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| Keywords: | suspended river type formation condition |
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