CAJ | 학술논문

依托大量的水文地质调查、水化学样品分析等数据,结合遥感、14C测年、水监测等多种手段对九寨沟核心景区水循环系统进行分析研究,将研究区分为日则沟、则查洼沟、树正沟、丹祖沟四个水文分系统.区内气候和降水呈周期性变化,岩石和地质构造稳定.总体上,水的转化主要通过跨流域(沟谷)补给和沟内纵向转化两个途径,并且沟内核心景观都处在青年期和壮年期,现处于相对稳定状态.
의탁대량적수문지질조사、수화학양품분석등수거,결합요감、14C측년、수감측등다충수단대구채구핵심경구수순배계통진행분석연구,장연구구분위일칙구、칙사와구、수정구、단조구사개수문분계통.구내기후화강수정주기성변화,암석화지질구조은정.총체상,수적전화주요통과과류역(구곡)보급화구내종향전화량개도경,병차구내핵심경관도처재청년기화장년기,현처우상대은정상태.
Based on data of hydrogeology survey,hydrochemistry sample analyses,combined with remote sensing,14Cdating,water monitoring and many other kinds of methods,analyses of hydrological circulating systemin the Jiuzhaigou core scenic area are conducted in this paper.The study area is divided into the Rizhegou,Zezhawagou,Shuzhenggou and Danzhugou hydrologic subsystems.Cyclical changes in climate and precipitation occur in this study area,and the rocks and geological structures arestable.Water transformation mainly occurs throughinter-basin(valley)supply and the vertical trench replenishment.The core landscape are inthe adolescence and mature stage,and itspresent situation is at a relatively steady state.