黄龙自然风景区地表水流量减少原因初探  

Study on Cause of Surface Water Flow Reduction at Huanglong Scenic Spot

作　　者：张金流[1,2] 唐淑 

机构地区：[1]合肥学院,合肥230601 [2]安徽省环境污染防治与生态修复协同创新中心,合肥230601 [3]黄龙国家级自然风景区管理局,松潘623300

出　　处：《世界科技研究与发展》2015年第6期688-691,共4页World Sci-Tech R&D

基　　金：国家自然科学基金(41172232);安徽高校省级自然科学研究重点项目(KJ2014A214);重点学科项目(2014XK01);学科带头人培养对象项目(2014dtr02);合肥学院人才基金(13RC04)资助

摘　　要：近年来黄龙风景区出现了许多干涸的钙华池,说明相较以前,黄龙风景区地表水流量已明显减少。本文通过对当地大气降水量年际间变化及景区上游地表雪融水、黄龙泉(源泉)及下游龙眼泉(二次转化泉)三者流量间变化趋势进行分析,确定地表水垂直下渗量增加是导致黄龙风景区地表水流量减少的真正原因。文章最后分析了导致地表水垂直下渗量增加的可能原因。Some travertine pools drying up in Huanglong scenic spot in recent years, this show that surface water flow has been significantly reduced compared to that in previous. The annual variation of precipitation and the flow change trend of the upstream snowmelt water, Huanglong spring （source spring） water and Longyan spring （secondary transferred spring） water are analyzed. The result show that surface water vertical infiltration increase is the real reason that lead to surface wa- ter flow reduction in recent years at Huanglong scenic spot. Finally, possible cause that lead to surface water vertical infiltra- tion increased are analyzed.

关 键 词：地表水 流量减少 下渗增加 黄龙风景区 

分 类 号：P333[天文地球—水文科学]