贵州省变质岩区基岩裂隙水富水分析  

Rich Water Analysis for Fissure Water in Bed Rock in Metamorphic Rock Terrains in Guizhou Province

作　　者：王汉兴[1] 郑朋[1] 

机构地区：[1]贵州省交通规划勘察设计研究院股份有限公司,贵阳550081

出　　处：《公路交通技术》2016年第3期10-14,共5页Technology of Highway and Transport

摘　　要：贵州省变质岩区具有独特的水文地质环境。近年来,随着全球气候变暖,省内岩溶区地下水水位下降、地表水干枯,对区内水文地质环境影响大,但对变质岩区影响甚微。通过对变质岩裂隙发育特征、富水性、变质岩裂隙水基本特征的分析,了解变质岩区独特的水文地质环境,其结果有助于该区域的水文地质和工程地质勘探。The metamorphic rock terrains in Guizhou Province exhibit the unique hydrogeological environment. With global climate warming in recent years,drop of the underground water level and drying of surface water in karst region within the province bring great influence on the hydrogeological environment greatly within the area,but slightly influence on the metamorphic rock area. By analyzing the growth features and watery of metamorphic rock cracks and basic features of fissure water in metamorphic rock cracks,this paper understands the unique hydrogeological environment in metamorphic rock area,and the results are helpful for hydrogeological and engineering geological exploration in the area.

关 键 词：变质岩 裂隙水 线路工程建设 

分 类 号：U412.36[交通运输工程—道路与铁道工程]