Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed
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...
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Editorial Office of Hydrogeology & Engineering Geology
2025-01-01
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Series: | Shuiwen dizhi gongcheng dizhi |
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Online Access: | https://www.swdzgcdz.com/en/article/doi/10.16030/j.cnki.issn.1000-3665.202312042 |
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author | Yun YANG Yong GUO Fafei WANG Jian SONG Jianfeng WU |
author_facet | Yun YANG Yong GUO Fafei WANG Jian SONG Jianfeng WU |
author_sort | Yun YANG |
collection | DOAJ |
description | 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. |
format | Article |
id | doaj-art-f92b607e884d46ecbe18d4bcaf00b028 |
institution | Kabale University |
issn | 1000-3665 |
language | zho |
publishDate | 2025-01-01 |
publisher | Editorial Office of Hydrogeology & Engineering Geology |
record_format | Article |
series | Shuiwen dizhi gongcheng dizhi |
spelling | doaj-art-f92b607e884d46ecbe18d4bcaf00b0282025-01-18T03:52:24ZzhoEditorial Office of Hydrogeology & Engineering GeologyShuiwen dizhi gongcheng dizhi1000-36652025-01-01521324110.16030/j.cnki.issn.1000-3665.202312042202312042Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershedYun YANG0Yong GUO1Fafei WANG2Jian SONG3Jianfeng WU4School of Earth Science and Engineering, Hohai University, Nanjing, Jiangsu 211100, ChinaSchool of Earth Science and Engineering, Hohai University, Nanjing, Jiangsu 211100, ChinaSchool of Earth Science and Engineering, Hohai University, Nanjing, Jiangsu 211100, ChinaSchool of Earth Science and Engineering, Nanjing University, Nanjing, Jiangsu 210093, ChinaSchool of Earth Science and Engineering, Nanjing University, Nanjing, Jiangsu 210093, ChinaPrevious 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.https://www.swdzgcdz.com/en/article/doi/10.16030/j.cnki.issn.1000-3665.202312042valley watershedsurface water-groundwaterswat-modflow modelcoupling modelwater exchange |
spellingShingle | Yun YANG Yong GUO Fafei WANG Jian SONG Jianfeng WU Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed Shuiwen dizhi gongcheng dizhi valley watershed surface water-groundwater swat-modflow model coupling model water exchange |
title | Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed |
title_full | Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed |
title_fullStr | Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed |
title_full_unstemmed | Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed |
title_short | Integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed |
title_sort | integrated model for estimation of the interaction between surface water and groundwater based on in valley watershed |
topic | valley watershed surface water-groundwater swat-modflow model coupling model water exchange |
url | https://www.swdzgcdz.com/en/article/doi/10.16030/j.cnki.issn.1000-3665.202312042 |
work_keys_str_mv | AT yunyang integratedmodelforestimationoftheinteractionbetweensurfacewaterandgroundwaterbasedoninvalleywatershed AT yongguo integratedmodelforestimationoftheinteractionbetweensurfacewaterandgroundwaterbasedoninvalleywatershed AT fafeiwang integratedmodelforestimationoftheinteractionbetweensurfacewaterandgroundwaterbasedoninvalleywatershed AT jiansong integratedmodelforestimationoftheinteractionbetweensurfacewaterandgroundwaterbasedoninvalleywatershed AT jianfengwu integratedmodelforestimationoftheinteractionbetweensurfacewaterandgroundwaterbasedoninvalleywatershed |