[1]李瑾,夏克勤,张强.重庆走马岭隧道岩溶及岩溶水发育特征[J].水土保持研究,2005,12(06):36-38.
　LI Jin,XIA Ke-qin,ZHANG Qiang.The Characteristic and Impact of Karst in Zoumaling Tunnel[J].Research of Soil and Water Conservation,2005,12(06):36-38.
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重庆走马岭隧道岩溶及岩溶水发育特征

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 12 期数: 2005年06期 页码: 36-38 栏目: 出版日期: 1900-01-01
Title:
The Characteristic and Impact of Karst in Zoumaling Tunnel
作者:
李瑾, 夏克勤, 张强
成都理工大学环境与土木工程学院, 四川, 成都, 610059
Author(s):
LI Jin, XIA Ke-qin, ZHANG Qiang
College of Environment and Civil Engineering, Chengdu University of Technology, Chengdu, 610059, China
关键词:
岩溶; 岩溶水; 发育特征; 发育深度; 方斗山背斜
Keywords:
karst; karst water; developing characteristic; developing depth; Fangdoushan anticline
分类号:
P588.18
摘要:
走马岭隧道通过方斗山背斜可溶岩地区,岩溶发育强烈.在分析隧址区地质环境的基础上,详细论述隧址区岩溶发育分布规律和特征,岩溶水补、径、排条件及化学特征,为隧道安全施工提供科学依据并提出建议.
Abstract:
Zoumaling tunnel passes through the Fangdoushan anticline where the karst development is strong.Based on the brief geologic condition in this area,the authors particularly discuss the developing characteristic and karst water’s recharge,runoff and outflow and chemical features.It offers the scientific basis and rational suggestion in safety tunnel construction.

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备注/Memo

收稿日期:2004-12-1。
作者简介:李瑾(1981- ),女,环境工程专业硕士研究生,主要从事环境地质及水文地质方面的研究.

更新日期/Last Update: 1900-01-01