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。
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.
出处
《四川地质学报》
2012年第1期80-82,93,共4页
Acta Geologica Sichuan
基金
四川省"十五"重大科技攻关项目(川发改地区函[2004]161号)
关键词
水均衡原理
地下径流
九寨沟
principle of water balance
groundwater runoff system
Jiuzhai Valley
