断裂带水力特性研究进展

史浙明; 叶海龙; 吕少杰; 齐之钰; 何冠儒

doi:10.19509/j.cnki.dzkq.tb2022

断裂带水力特性研究进展

doi: 10.19509/j.cnki.dzkq.tb2022

1.
中国地质大学(北京)水资源与环境学院, 北京 100083
2.
南昌市水文地质与优质地下水资源开发利用重点实验室, 南昌 330000

基金项目:

南昌市水文地质与优质地下水资源开发利用重点实验室资助项目 20232B22

详细信息

作者简介:
史浙明(1988—), 男, 教授, 主要从事水文地质教学与科研工作。E-mail: szm@cugb.edu.cn

中图分类号: P641
计量
- 文章访问数: 649
- PDF下载量: 113
- 被引次数: 0
出版历程
- 收稿日期: 2023-02-11
- 录用日期: 2023-05-11
- 修回日期: 2023-04-11

Advances in fault zone hydraulic properties

1.
School of Water Resources and Environment, China University of Geosciences(Beijing), Beijing 100083, China
2.
Nanchang Key Laboratory of Hydrogeology and High Quality Groundwater Resources Exploitation and Utilization, Nanchang 330000, China

摘要

摘要:
断裂带作为具有重要水文地质意义的构造现象, 往往对地下水运移产生显著影响。考虑断裂带的水文地质作用对于水资源管理和评价具有重要意义。围绕断裂带渗透性, 从断裂带渗透性结构及调查方法, 断裂带水力特性定量表征, 断裂带水力特性的动态演变特征, 断裂带地下水流模拟等方面展开论述。断裂带的渗透性是当前断裂带研究的核心, 不同的渗透性刻画方法具有不同的代表性尺度。断裂带渗透性具有复杂的时空分布特征, 对刻画断裂带的地下水运移造成较大挑战。针对不同目的, 选择合适的数值模拟方法是定量刻画断裂带地下水运移的重要途径, 也可以对其他方法进行有效的验证。如何在模拟过程中考虑断裂带水力特性在时空尺度上的复杂性是准确刻画断裂带地下水流动的前提。笔者认为建立专门的断裂带水文地质观测基地, 综合地质、水文地质、热流、地球物理及遥感数据资料, 加强多学科的交叉合作, 是进一步提升断裂带地下水研究水平的关键。
- 断裂带 /
- 地下水 /
- 破碎带 /
- 水力特性 /
- 渗透性
Abstract: Significance
As a tectonic phenomenon with important hydrogeological significance, fault zones mostly show a significant impact on groundwater migration.
Progress
It is important to include fault zones in water resource management and evaluation. This paper focuses on the permeability of the fault zone, the quantitative characterization and the evolution of the hydraulic characteristics of the fault zone, the dynamic evolution of the hydraulic characteristics of fault zones and the simulation of groundwater flow in the fault zone. The permeability of the fault zone is the key to the current study, and different permeability characterization methods have different representative scales. The permeability of the fault zone has complex spatiotemporal distribution characteristics, which challenges the description of groundwater migration in the fault zone. The selection of appropriate numerical simulation methods is an important way to quantitatively describe the groundwater movement in the fault zone and verify the suitability of the other methods. How to consider the complexity of the hydraulic characteristics of the fault zone at the spatiotemporal scale in the simulation process is the premise of accurately characterizing the groundwater flow in the fault zone.
Conclusions and Prospects
We suggest that a special hydrogeological observation base for the fault zone is the key to further improve the level of fault zone groundwater study, and data from geological, hydrogeological, heat flow, geophysical and remote sensing should be integrated, and interdisciplinary cooperation should be strengthened.
- fault zone /
- groundwater /
- damage zone /
- hydrological property /
- permeability
注释:

(所有作者声明不存在利益冲突)

HTML全文

图 1 断裂带分类示意图(据文献[1]修改)

Figure 1. Schematic diagram of fault zone classification

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图 2 断裂破碎带(a)及断裂带渗透结构(b)示意图(据文献[12]修改)

Figure 2. Schematic diagram of the fault damage zone (a) and fault zone permeability structure (b)

下载: 全尺寸图片幻灯片

图 3 断层对地下水流动影响的3种概念模式

Figure 3. Three conceptual models of fault influence on groundwater flow

下载: 全尺寸图片幻灯片

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