Impact of topographic fluctuation of riverbed on surface water-groundwater-wetland water interaction

Spatial variation of riverbed topography caused by the difference of dynamic conditions of surface water affects spatial distribution of pressure at water-sediment interface, which has an important influence on the interaction between surface water and groundwater and the interaction between groundw...

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Main Authors: Lijuan ZHANG, Peipeng WU, Shengyan ZHANG, Yang ZHANG
Format: Article
Language:zho
Published: Editorial Office of Hydrogeology & Engineering Geology 2024-01-01
Series:Shuiwen dizhi gongcheng dizhi
Subjects:
Online Access:https://www.swdzgcdz.com/en/article/doi/10.16030/j.cnki.issn.1000-3665.202303004
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author Lijuan ZHANG
Peipeng WU
Shengyan ZHANG
Yang ZHANG
author_facet Lijuan ZHANG
Peipeng WU
Shengyan ZHANG
Yang ZHANG
author_sort Lijuan ZHANG
collection DOAJ
description Spatial variation of riverbed topography caused by the difference of dynamic conditions of surface water affects spatial distribution of pressure at water-sediment interface, which has an important influence on the interaction between surface water and groundwater and the interaction between groundwater and wetland water. To reveal the influence mechanism of riverbed undulations on surface water-ground water interaction, This study established a groundwater flow numerical simulation model and analyzed the influence mechanism of riverbed topography on surface water-groundwater-wetland interaction process based on the characteristics of riverbed topographic undulations of a profile at Liuyuankou, Kaifeng, the lower reaches of the Yellow River. The results show that: (1) compared with flat riverbed, the variable riverbed topography leads to an increasing exchange fluxes between surface water and between groundwater and wetland water; (2) The spatial fluctuation of riverbed topography forms different levels of groundwater flow systems at the bottom of the riverbed, and changes the groundwater flow path and the travel time. Compared with the flat bed topography, the variation of the topography of river bed complicates the groundwater flow path in the underlying aquifer. Retention areas are developed in different positions in the aquifer near the bed interface. Moreover, the greater topography degree of the river bed, the older the groundwater age in the aquifer beneath the wetland bed and aquifer near the wetland. This study can provide theoretical basis for promoting the coordinated protection of surface water, groundwater and wetland water in the suspended reach of the lower Yellow River.
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spelling doaj.art-86a7c555436b40b58ab145d18d043fe22024-01-21T13:37:34ZzhoEditorial Office of Hydrogeology & Engineering GeologyShuiwen dizhi gongcheng dizhi1000-36652024-01-01511222910.16030/j.cnki.issn.1000-3665.202303004202303004Impact of topographic fluctuation of riverbed on surface water-groundwater-wetland water interactionLijuan ZHANG0Peipeng WU1Shengyan ZHANG2Yang ZHANG3Ecological Environment Geo-Service Center of Henan Geological Bureau, Zhengzhou, Henan 450053, ChinaCollege of New Energy and Environment, Jilin University, Changchun, Jilin 130021, ChinaEcological Environment Geo-Service Center of Henan Geological Bureau, Zhengzhou, Henan 450053, ChinaEcological Environment Geo-Service Center of Henan Geological Bureau, Zhengzhou, Henan 450053, ChinaSpatial variation of riverbed topography caused by the difference of dynamic conditions of surface water affects spatial distribution of pressure at water-sediment interface, which has an important influence on the interaction between surface water and groundwater and the interaction between groundwater and wetland water. To reveal the influence mechanism of riverbed undulations on surface water-ground water interaction, This study established a groundwater flow numerical simulation model and analyzed the influence mechanism of riverbed topography on surface water-groundwater-wetland interaction process based on the characteristics of riverbed topographic undulations of a profile at Liuyuankou, Kaifeng, the lower reaches of the Yellow River. The results show that: (1) compared with flat riverbed, the variable riverbed topography leads to an increasing exchange fluxes between surface water and between groundwater and wetland water; (2) The spatial fluctuation of riverbed topography forms different levels of groundwater flow systems at the bottom of the riverbed, and changes the groundwater flow path and the travel time. Compared with the flat bed topography, the variation of the topography of river bed complicates the groundwater flow path in the underlying aquifer. Retention areas are developed in different positions in the aquifer near the bed interface. Moreover, the greater topography degree of the river bed, the older the groundwater age in the aquifer beneath the wetland bed and aquifer near the wetland. This study can provide theoretical basis for promoting the coordinated protection of surface water, groundwater and wetland water in the suspended reach of the lower Yellow River.https://www.swdzgcdz.com/en/article/doi/10.16030/j.cnki.issn.1000-3665.202303004riverbed topographysurface watergroundwaterwetlands waterinteraction
spellingShingle Lijuan ZHANG
Peipeng WU
Shengyan ZHANG
Yang ZHANG
Impact of topographic fluctuation of riverbed on surface water-groundwater-wetland water interaction
Shuiwen dizhi gongcheng dizhi
riverbed topography
surface water
groundwater
wetlands water
interaction
title Impact of topographic fluctuation of riverbed on surface water-groundwater-wetland water interaction
title_full Impact of topographic fluctuation of riverbed on surface water-groundwater-wetland water interaction
title_fullStr Impact of topographic fluctuation of riverbed on surface water-groundwater-wetland water interaction
title_full_unstemmed Impact of topographic fluctuation of riverbed on surface water-groundwater-wetland water interaction
title_short Impact of topographic fluctuation of riverbed on surface water-groundwater-wetland water interaction
title_sort impact of topographic fluctuation of riverbed on surface water groundwater wetland water interaction
topic riverbed topography
surface water
groundwater
wetlands water
interaction
url https://www.swdzgcdz.com/en/article/doi/10.16030/j.cnki.issn.1000-3665.202303004
work_keys_str_mv AT lijuanzhang impactoftopographicfluctuationofriverbedonsurfacewatergroundwaterwetlandwaterinteraction
AT peipengwu impactoftopographicfluctuationofriverbedonsurfacewatergroundwaterwetlandwaterinteraction
AT shengyanzhang impactoftopographicfluctuationofriverbedonsurfacewatergroundwaterwetlandwaterinteraction
AT yangzhang impactoftopographicfluctuationofriverbedonsurfacewatergroundwaterwetlandwaterinteraction