基于地下水位微动态反演含水层水文地质参数研究进展

张卉; 王广才; 史浙明; 周鹏鹏

doi:10.19509/j.cnki.dzkq.tb20230029

基于地下水位微动态反演含水层水文地质参数研究进展

doi: 10.19509/j.cnki.dzkq.tb20230029

张卉^{1, 2,},
王广才^2, ,,
史浙明²,
周鹏鹏²

1.
太原理工大学, 太原 030024
2.
中国地质大学(北京), 北京 100083

基金项目:

国家自然科学基金重点项目 42030705

山西省基础研究计划(自由探索类)青年项目 202203021222114

详细信息

作者简介:
张卉(1993—), 女, 讲师, 主要从事地震地下水研究工作。E-mail: zhanghui03@tyut.edu.cn

通讯作者:
王广才(1962—), 男, 教授, 主要从事水文地质方面的教学与科研工作。E-mail: wanggc@cugb.edu.cn

中图分类号: P641
计量
- 文章访问数: 792
- PDF下载量: 63
- 被引次数: 0
出版历程
- 收稿日期: 2023-01-17
- 录用日期: 2023-03-10
- 修回日期: 2023-03-08

Advances in estimation of aquifer hydrogeological parameters based on microfluctuations of groundwater level

1.
Taiyuan University of Technology, Taiyuan 030024, China
2.
China University of Geosciences(Beijing), Beijing 100083, China

摘要

摘要:
研究水文地质参数随时间变化的特征及机理有利于深入了解地下水系统特性。地下水位微动态对于天然周期性荷载固体潮及气压加载作用的响应则提供了一种经济有效的含水层水文地质参数计算方法。系统梳理了地下水对于固体潮响应、气压响应以及综合固体潮及气压响应求解参数的理论模型，介绍了井-含水层系统受地震及采矿活动影响过程中水文地质参数随时间变化的情况。气压响应方法也可用于含水层脆弱性的评估。分析认为，研究地下水位微动态有利于在时间及空间尺度上了解地壳运动及人类活动对含水层系统的影响。最后提出了该领域未来研究方向主要包括：井孔皮肤效应及储积效应的应用、结合多种确定基础地质参数的方法提高水文地质参数计算精度、探索地下水超采及地面沉降等其他人类活动对区域尺度含水层系统的影响。
- 地下水位 /
- 微动态 /
- 固体潮 /
- 气压 /
- 水文地质参数
Abstract: Objective
In order to understand groundwater systems, it is useful to study the changing characteristics and mechanisms of hydrogeological parameters with time. Responses of groundwater level microfluctuations to natural periodic loadings, such as earth tides and barometric pressure, serve as low-cost and effective investigation technique to calculate aquifer hydrogeological parameters.
Methods
In this paper, we systematically reviewed theoretical methods of hydrogeological parameters estimation based on groundwater level response to earth tides, barometric pressure, and their combination. We presented earthquake-related and mining-related parameters change with time in well-aquifer system. The barometric pressure response method also applies to the assessment of aquifer vulnerability.
Results
We conclude that studying the microfluctuation of groundwater level may provide insight into the interaction among hydrogeological processes, tectonic activities, and artificial influences in the shallow crust at spatial and temporal scales.
Conclusion
This paper also proposes three scientific problems to be solved in the future: the application of skin and wellbore storage effects, the improvement of computation accuracy of hydrogeological parameters by combining multiple methods for determining basic geological parameters, and the investigation of other artificial influences such as groundwater overdraft and subsidence to regional aquifer systems.
- groundwater level /
- microfluctuation /
- earth tides /
- barometric pressure /
- hydrogeological parameter
注释:

(所有作者声明不存在利益冲突)

HTML全文

图 1 井孔水位微动态固体潮和气压响应概念模型图(a)，实测大气压数据时间序列(b)，对应实测大气压数据频率域(c)，实测非承压条件下潜水井水位时间序列(d), 对应潜水井水位频率域(e), 理论固体潮计算结果时间序列(f), 对应固体潮频率域(g), 实测承压条件下承压井水位时间序列(h), 对应承压井水位频率域(i), 频率域中上标AT、ET分别代表气压、固体潮主导分波，S₁、K₁、S₂、M₂为与其相关的日波及半日波，φ₁和φ₂代表相同频率的固体潮及气压谐波加载作用下引起的地下水位相位响应(改自文献[26])

Figure 1. Conceptual overview of the groundwater system response to earth tides and barometric pressure(a), and time series of measured barometric pressure(b), barometric pressure in frequency domain(c), water level measured in unconfined aquifer(d), amplitude spectrum of water level measured in unconfined aquifer (e), computed theoretical earth tides in time domain(f), theoretical earth tides in frequency domain(g), time series of measured confined water level(h), confined water level in frequency domain(i)

下载: 全尺寸图片幻灯片

图 2 实验室及野外观测到的渗透率与动态应变幅值变化关系图总结(引自文献[54])

黑色填充框表示频率≥10 Hz的室内实验; 白色框为实验室动态应力变化测试结果; 灰色线框为野外天然情况下观测结果

Figure 2. Summary of the permeability changes documented in the laboratory and field as a function of dynamic strain

下载: 全尺寸图片幻灯片

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