Geothermal Characteristics of Groundwater Seeping Division and Geothermal Hazard Prevention of Tunnel

漆继红; 许模; 王能峰; 王迪

doi:10.13409/j.cnki.jdpme.2015.03.009

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Geothermal Characteristics of Groundwater Seeping Division and Geothermal Hazard Prevention of Tunnel

更新时间：2025-12-11

- Geothermal Characteristics of Groundwater Seeping Division and Geothermal Hazard Prevention of Tunnel
- Vol. 35, Issue 3, Pages: 333-339(2015)
- 作者机构：
- 作者简介：
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- DOI：10.13409/j.cnki.jdpme.2015.03.009
  CLC： 452.11;U457.2
- Published：2015
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[1]漆继红,许模,王能峰,王迪.地下水渗流分区的地温特征及隧道热害规避应用[J].防灾减灾工程学报,2015,35(03):333-339.

漆继红, 许模, 王能峰, et al. Geothermal Characteristics of Groundwater Seeping Division and Geothermal Hazard Prevention of Tunnel[J]. 2015, 35(3): 333-339.
[1]漆继红,许模,王能峰,王迪.地下水渗流分区的地温特征及隧道热害规避应用[J].防灾减灾工程学报,2015,35(03):333-339. DOI： 10.13409/j.cnki.jdpme.2015.03.009.

漆继红, 许模, 王能峰, et al. Geothermal Characteristics of Groundwater Seeping Division and Geothermal Hazard Prevention of Tunnel[J]. 2015, 35(3): 333-339. DOI： 10.13409/j.cnki.jdpme.2015.03.009.

摘要

基于热传递微分方程讨论了水流导热影响下地温特征与深度的关系

获得地温、地温梯度与深度关系的解析表达;对渗流影响下的地温特征类型进行分析

提出了通过最小二乘法拟合地温试验数据计算渗流参量、获取渗流特征的方法及程序。并以滇西高黎贡山越岭段为研究对象

基于地温特征对其热水渗流分区进行分析。研究认为

穿越其中的拟选隧道线南北两水热活动区相互独立

黄草坝断裂阻隔了北面热水向南面渗流

判定断裂南面区域一定范围为南部热水的补给地带

越岭拟选隧道线为区内低地温通道

为合理规避隧道热害提供了依据。

Abstract

Based on the differential equation of heat conduction

this article discusses the convection influence on earth′s temperature and the relationship between geothermal characteristics and depth.It gets the analytical expression of geothermal characteristics with depth

proposes the method and procedure for using the least square method to analyze geothermal data and gets the seeping characteristics of groundwater.An engineering problem example is given

which can be explained by this relationship to choose the position of Gaoligong tunnel going through.It analyzes the geothermal characteristics and gets seeping division.It considers that the warm groundwater appears in the north part to the Huangcaoba fault

can′t flow to the south part of it.This fault cuts off warm groundwater flow

makes the north and south parts become separate area.It gets the results that the aim position of the tunnel is low geothermal area.This conclusion can give us proof to avoid the geothermal hazard of tunnel reasonably.

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references

利用井温分布估算莺-琼盆地地下流体运移速度 [J]. 张键,葛社民,许鹤华,熊亮萍,杨计海,张启明. 地质力学学报 . 2000(02)

深埋长大隧道中地下水对地温异常的影响 [J]. 王贤能,黄润秋,黄国明. 地质灾害与环境保护 . 1996(04)

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Use of Temperature Profiles and Stable Isotopes to Trace Flow Lines: Nagaoka Area, Japan [J] . Zenhom El‐saidSalem,MakotoTaniguchi,YasuaSakura. Ground Water . 2005 (1)

Estimation of groundwater velocity in localized fracture zones from well temperature profiles [J] . Shemin Ge. Journal of Volcanology and Geothermal Research . 1998 (1)

The Theory of Ground-Water Motion [J] . M. King Hubbert. The Journal of Geology . 1940 (8)

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