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华蓥山隧道隧址区水文地球化学特征及涌水来源识别

林云 娄亚南 武亚遵 秦成 潘磊

水资源与水工程学报2017,Vol.28Issue(5):43-48,6.
水资源与水工程学报2017,Vol.28Issue(5):43-48,6.DOI:10.11705/j.issn.1672-643X.2017.05.07

华蓥山隧道隧址区水文地球化学特征及涌水来源识别

Hydrogeochemical characteristics and identification of water source in Huayingshan Tunnel District

林云 1娄亚南 2武亚遵 1秦成 1潘磊3

作者信息

  • 1. 河南理工大学资源环境学院,河南焦作454000
  • 2. 中原经济区煤层(页岩)气河南省协同创新中心,河南焦作454000
  • 3. 中煤科工集团重庆研究院有限公司,重庆400016
  • 折叠

摘要

Abstract

In order to predict the potential water inrush problem produced during the construction of Huayingshan tunnel, the research analyzed the hydrogeochemical characteristics of the surface water, groundwater and inrush water of Huayingshan tunnel, and identified the inrush water resource based on the field investigations and hydrochemical analysis of water samples.The result shows that,in Huayings-han tunnel area the main hydrochemical types of regional water are HCO 3-Ca and HCO3· SO4-Ca. The water quality is in alkalescency,and the hydrochemical origin of water is rock weathering.There is close relationship between shallow groundwater and surface water.Precipitation is main supply sources of all kinds of water.Replenishment elevation of study area is 315~1467m.In the southeast region the tun-nel inrush water mainly comes from sandstone aquifers of upper Triassic Xujiahe formation(T3xj)and middle Jurassic Xintiangou formation(J2x),and the northwest comes from limestone karst aquifer of lower Triassic Jialingjiang formation(J1x).

关键词

稳定同位素/水化学特征/涌水来源/含水层/华蓥山隧道

Key words

stable isotope/hydrochemistry/water inrush sources/aquifers/Huayingshan tunnel

分类

交通工程

引用本文复制引用

林云,娄亚南,武亚遵,秦成,潘磊..华蓥山隧道隧址区水文地球化学特征及涌水来源识别[J].水资源与水工程学报,2017,28(5):43-48,6.

基金项目

国家自然科学基金项目(41502224、41602265) (41502224、41602265)

河南省高校科技创新团队支持计划(15IRTSTHN027) (15IRTSTHN027)

河南省创新型科技人才队伍建设工程(CXTD2016053) (CXTD2016053)

水资源与水工程学报

OACSCDCSTPCD

1672-643X

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