黄龙钙华景观形成及演化趋势研究  

A study of the formation and evolution trend of the Huanglong travertine landscape

作　　者：姜泽凡 刘艳梅[2] 胥良[1] 

机构地区：[1]四川省地质环境监测总站,成都610081 [2]西南民族大学化学与环境保护工程学院,成都610041

出　　处：《水文地质工程地质》2008年第1期107-111,116,共6页Hydrogeology & Engineering Geology

基　　金：四川省发展和改革委员会([2004]161号)资助

摘　　要：黄龙景区因拥有钙华源泉、彩池、滩流、瀑布等景观而享誉世界,其钙华景观的稳定性也为世人所关注。文章通过对与钙华景观形成密切相关的地质环境,特别是水循环系统动态变化及区域钙华景观成长演化历史的研究,认为黄龙钙华景观现状稳定性较好,但正处于缓慢的、反复的衰退过程,只要采取适当的措施可以延缓其衰退。The Huanglong scenic spot is world-famous, which includes travertine source spring, colored ponds, sinter flow beaches and waterfalls, etc. The stability of the travertine landscape attracts more and more attention. An investigation of geo-environment related to the formation of the travertine landscape, especially the dynamic changes in water circulation system and the development of the landscape was carried out. The results indicate that the Huangl reoccurring ong travertine landscape is stable at present, but it is in its gradual decline stage and this decline is a procedure. The decline could be controlled if propert protection measures are taken.

关 键 词：黄龙 钙华景观 演化趋势 衰退 

分 类 号：P642.251[天文地球—工程地质学]