Jun Zhang; Rong-zhe Hou; Kun Yu; Jia-qiu Dong; Li-he Yin

doi:10.26599/JGSE.2024.9280010

doi: 10.26599/JGSE.2024.9280010

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出版历程
- 收稿日期: 2023-10-13
- 录用日期: 2024-04-12
- 网络出版日期: 2024-06-10
- 刊出日期: 2024-06-30

Impact of water table on hierarchically nested groundwater flow system

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Key Laboratory of Groundwater and Ecology in Arid and Semi-arid Areas, Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China

More Information

Corresponding author: zjun@mail.cgs.gov.cn

摘要

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Abstract: Water table configuration gives rise to hierarchically nested groundwater flow systems. However, there remains a lack of comprehensive understanding regarding the controlling factors of water table and its impact on flow systems. Moreover, it remains challenging to identify characteristics of water table space variation through limited groundwater observations at the regional scale. Based on two ideal two-dimensional cross-section analytical models, this study presents a simplified approach to preliminarily assess the nonlinear interactions between water table variation and three driving factors: Topography, geology and climate. Two criteria, C1 and C2, are utilized to address issues at different scales ranging from basin to local: (i) the influence of various factors on water table configuration; and (ii) the influence of water table on groundwater flow pattern. Then, the Ordos Plateau is taken as an example to explore the role of the water table in nested groundwater systems using the provided approach and criterion. The application of this approach in the Ordos Plateau demonstrates its appropriateness as a practical method for preliminarily determining the characteristics of water table configuration and its impact on flow systems. The study explores the mechanism influencing spatial variation in the water table and improves understanding of the interaction between topography, geology, and climate on groundwater flow patterns.
- Water table configuration /
- Groundwater flow pattern /
- Analytical models /
- Top boundary conditions /
- Ordos Plateau

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Figure 1. (a) Groundwater mounding due to recharge may interact with the topography; (b) topography-controlled water table; (c) recharge-controlled water table (Haitjema and Mitchell-Bruker, 2005).

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Figure 2. (a) CSF in an unconfined aquifer between two water bodies; (b) LFS in RFS, which IFS represents the intermediate flow system.

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Figure 3. Map of the Ordos Plateau showing average annual precipitation, potential evapotranspiration, endorheic region and groundwater divide

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Figure 4. The contours map of water table elevation and water table depth of 2006 to 2008

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