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岩溶地下河管道流和管道结构及参数的定量示踪——以桂林寨底地下河为例

陈余道 程亚平 王恒 蒋亚萍 黄月群

水文地质工程地质2013,Vol.40Issue(5):11-15,5.
水文地质工程地质2013,Vol.40Issue(5):11-15,5.

岩溶地下河管道流和管道结构及参数的定量示踪——以桂林寨底地下河为例

Quantitative tracing study of hydraulic and geometric parameters of a karst underground river: exemplified by the Zhaidi underground river in Guilin

陈余道 1程亚平 1王恒 1蒋亚萍 1黄月群1

作者信息

  • 1. 桂林理工大学广西矿冶与环境科学实验中心,广西桂林541004
  • 折叠

摘要

Abstract

Quantitative tracing studies are the most reliable diagnostic techniques for estimating basic hydraulic and geometric parameters of karst conduits for hydrogeological generalization and numerical model.As an example,a tracer test was performed in the Zhaidi underground river in Guilin of China,in which uranine and rhodamine B were used as co-tracers and were monitored via the automatic detection technology with high precision,high density and multiple indicators.Based on breakthrough curves (BTCs),some parameters including mean residence time,average transfer velocity,dispersion coefficient,conduit volume,conduit surface area and flow cross-sectional area were determined.Moreover,the difference in adsorption between uranine and rhodamine B exist.The BTC of uranine can provide more reliable results owing to little adsorption.However,rhodamine B with strong adsorption need cautions when data are interpreted.

关键词

岩溶地下河/定量示踪研究/管道流/管道结构/参数估测

Key words

karst underground river/ quantitative tracing study / conduit flow / conduit structure/ parameter estimation

分类

天文与地球科学

引用本文复制引用

陈余道,程亚平,王恒,蒋亚萍,黄月群..岩溶地下河管道流和管道结构及参数的定量示踪——以桂林寨底地下河为例[J].水文地质工程地质,2013,40(5):11-15,5.

基金项目

国家自然科学基金(41172229) (41172229)

国家科技支撑项目(2012BAC16B02) (2012BAC16B02)

水文地质工程地质

OA北大核心CSCDCSTPCD

1000-3665

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