| 九寨沟地下径流系统 |
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| 引用本文： | 杨俊义,张慧利.九寨沟地下径流系统[J].四川地质学报,2012,32(1):80-82,93. |
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| 作者姓名： | 杨俊义 张慧利 |
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| 作者单位： | 1. 成都理工大学,成都610059;四川省地矿局区域地质调查队,成都610213
2. 四川省地矿局区域地质调查队,成都,610213 |
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| 基金项目： | 四川省“十五”重大科技攻关项目（川发改地区函[2004]161号） |
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| 摘 要： | 九寨沟景观钙华呈相对集中的带状分布,地表径流多处流量呈现异常,运用水均衡原理,论证了九寨沟次级含水单元间的补、排关系,用则查哇沟、丹祖沟次级含水单元通过渗漏补给日则沟,保证了九寨沟核心景观的稳定,长海对九寨沟径流系统具有重要调节作用。
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| 关 键 词： | 水均衡原理 地下径流 九寨沟 |
Groundwater Runoff System in the Jiuzhai Valley |
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| YANG Jun-yi
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ZHANG Hui-li.Groundwater Runoff System in the Jiuzhai Valley[J].Acta Geologica Sichuan,2012,32(1):80-82,93. |
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| Authors: | YANG Jun-yi ZHANG Hui-li |
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| Institution: | YANG Jun-yi ZHANG Hui-li(Chengdu University of Technology, Chengdu 610059; Regional Geological Surveying Team, BGEEMRSP, Chengdu 610213 ) |
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| Abstract: | Abnormal surface runotl and relative centrallzeQ olsnaouuon of travertine landscape in the Jiuzhai Valley result from the specific geological conditions. This paper deals with recharge-discharge regime relation of groundwater between the various secondary groundwater units. The Long Sea ensures the stability of core landscape in the Jiuzhai Valley. |
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| Keywords: | principle of water balance groundwater runoff system Jiuzhai Valley |
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