四川黄龙景区“源水”成因浅析  

Headwater origin analysis in the Huanglong scenic spot,Sichuan,China

作　　者：万新南[1] 杨菊[1] 程温莹[1] 罗丽[1] 安德军 唐淑 台永东 

机构地区：[1]成都理工大学"地质灾害防治与地质环境保护"国家重点实验室,成都610059 [2]四川省黄龙管理局,四川阿坝624600

出　　处：《成都理工大学学报（自然科学版）》2010年第1期91-95,共5页Journal of Chengdu University of Technology: Science & Technology Edition

基　　金：国家自然科学基金资助项目(40472128)

摘　　要：四川黄龙景区"源水"成因的研究历年来被专家所关注。通过对"源水区"化学场和地温场动态变化的分析,发现黄龙景观"源水区"水量、水质与水温直接受降水与季节影响,认为"源水区"钙华泉水的补给主要来自上游望乡台湿地生态水、降水、地表溪流。The research on the headwater origin of the Huanglong scenic spot in Sichuan has been by hydrogeologists and geo-chemists. A dynamic analysis of the ＂source water＂ chemical field and geothermal field shows that the headwater origin water, water quality and water temperature are directly affected by seasons and precipitation. The ＂source water area＂ travertine springs supply is considered mainly to come from wetland ecological water, precipitation, surface streams of the upper reaches point township units.

关 键 词：钙华 源水 湿地 补给 黄龙景区 

分 类 号：P641.1[天文地球—地质矿产勘探]