岩溶地下水分散流场示踪探测原理及其在水库渗漏研究中的应用  

PRINCIPLE OF TRACING AND DETECTING KARST GKOUNDWATER DISPERSIVE FLOW FIELD AND APPLICATION IN RESERVIOR LEAKAGE STUDY

作　　者：张祯武 邹成杰[1] 

机构地区：[1]贵州省水利电力学校,电力部贵阳勘测设计研究院

出　　处：《中国岩溶》1995年第3期251-260,共10页Carsologica Sinica

摘　　要：溶隙流一般称为分散流；岩溶管道流一般称为管流。本文仅研究分散流场的示踪探测问题。为此，导出了各类分散流场示踪数学模型，建立了各类分散流场与示踪曲线的对应关系，并以猫跳河四级水电站某些部位岩溶分散流场作为示踪探测的应用实例，取得了良好的效果。Solutional fissure flow is generally called dispersive flow and karst conduit flow. Thepropose of the paper is to study karst groundwater dispersive flow field with traces. Mathe-matic models for dispersive flow field tracing are derived and relation between different typesof dispersive flow fields and their tracing curves is set up.The application in the Maotiao Riv-er Hydroelectric Power Station of Fourth Cassade is of success.

关 键 词：岩溶地下水 分散流场 示踪探测 水库 渗漏 

分 类 号：TV697.32[水利工程—水利水电工程] P641.134[天文地球—地质矿产勘探]