Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed

YANG Yun; GUO Yong; WANG Fafei; SONG Jian; WU Jianfeng

doi:10.16030/j.cnki.issn.1000-3665.202312042

2025 Vol. 52, No. 1

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YANG Yun, GUO Yong, WANG Fafei, SONG Jian, WU Jianfeng. Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed[J]. Hydrogeology & Engineering Geology, 2025, 52(1): 32-41. doi: 10.16030/j.cnki.issn.1000-3665.202312042

Citation:

YANG Yun, GUO Yong, WANG Fafei, SONG Jian, WU Jianfeng. Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed[J]. Hydrogeology & Engineering Geology, 2025, 52(1): 32-41. doi: 10.16030/j.cnki.issn.1000-3665.202312042

Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed

1.
School of Earth Science and Engineering, Hohai University, Nanjing, Jiangsu　211100, China
2.
School of Earth Science and Engineering, Nanjing University, Nanjing, Jiangsu　210093, China

Received Date: 09 December 2023

Revised Date: 19 February 2024

Publish Date: 15 January 2025

Abstract

Abstract

Previous studies on surface water-groundwater (SW-GW) interactions have primarily focused on plain river networks, with limited understanding on hydrodynamic interactions in valley-type watersheds. This study focuses on the Beishan Reservoir Basin (BRB) in Jurong, specifically investigating surface runoff and shallow groundwater interactions in a valley-type watershed Jurong. A coupled SWAT-MODFLOW model was developed to evaluate the spatiotemporal variations in SW-GW interaction processes. The results show that the interaction between SW-GW varies both temporally and spatially. Temporally, the groundwater discharged into the surface water during 2016−2019, while the surface water replenished the groundwater during certain periods of wet season. Spatially, the mountainous areas in the northwest and northeast of the study area and the surrounding areas of BRB in the south of the study area are characterized by groundwater discharge into surface water. The coupling model effectively describes the surface water-groundwater (SW-GW) interaction, with groundwater contributing 8.72% to the net replenishment of rivers in the basin. The western tributaries and central tributaries of the basin receive 28.8% and 79.8% groundwater recharge in the whole basin, respectively. The eastern tributaries with negative groundwater recharge rate of 8.6% exhibit surface water discharge into groundwater. This study provides a technical support for joint scheduling and development and utilization of watershed water resources.
- valley watershed /
- surface water-groundwater /
- SWAT-MODFLOW model /
- coupling model /
- water exchange

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References

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