Littérature scientifique sur le sujet « SW-GW interaction »

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Articles de revues sur le sujet "SW-GW interaction"

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Akhtar, Naseem, Muhammad I. Syakir, Mardiana Idayu Ahmad, et al. "Upscaling of Surface Water and Groundwater Interactions in Hyporheic Zone from Local to Regional Scale." Water 14, no. 4 (2022): 647. http://dx.doi.org/10.3390/w14040647.

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The groundwater (GW) and surface water (SW) interaction (SW-GW) through the hyporheic zone is a significant component in sustainable water resource management. The complexities in SW-GW interactions increase from a local to a regional scale and are affected by variation in hydraulic, hydrologic, and hydrogeologic (3H) processes. Controlling factors and their upscaling of these processes to assess SW-GW interaction have not been addressed sufficiently in previous studies. Additionally, it is unclear what the effective factors are at different scales during the upscaling. Therefore, the present
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Cai, Zizhao, Wenke Wang, Ming Zhao, Zhitong Ma, Chuan Lu, and Ying Li. "Interaction between Surface Water and Groundwater in Yinchuan Plain." Water 12, no. 9 (2020): 2635. http://dx.doi.org/10.3390/w12092635.

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The interaction of surface water (SW) and groundwater (GW) is becoming more and more complex under the effects of climate change and human activity. It is of great significance to fully understand the characteristics of regional SW–GW circulation to reveal the water circulation system and the effect of its evolution mechanism to improve the rational allocation of water resources, especially in arid and semi-arid areas. In this paper, Yinchuan Plain is selected as the study area, where the SW–GW interaction is intensive. Three typical profiles are selected to build two-dimensional hydrogeologic
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Banerjee, Dolon, and Sayantan Ganguly. "A Review on the Research Advances in Groundwater–Surface Water Interaction with an Overview of the Phenomenon." Water 15, no. 8 (2023): 1552. http://dx.doi.org/10.3390/w15081552.

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Groundwater and surface water, though thought to be different entities in the past, are connected throughout the different landforms of the world. Despite being studied for quite some time, the interaction between groundwater and surface water (GW–SW) has received attention recently because of the heavy exploitation of both of these resources. This interaction is responsible for a phenomenon like contaminant transport, and understanding it helps to estimate the effects of climate change, land use on chemical behavior, and the nature of water. Hence, knowledge of GW–SW interactions is required
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Wang, Huimin, Yufei Jiao, Bill X. Hu, Fulin Li, and Dan Li. "Study on Interaction between Surface Water and Groundwater in Typical Reach of Xiaoqing River Based on WEP-L Model." Water 15, no. 3 (2023): 492. http://dx.doi.org/10.3390/w15030492.

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Surface water and groundwater (SW-GW) are an inseparable whole, having a tightly coupled hydraulic relationship and frequent inter-transformation. As such, the quantitative calculation of water exchange between SW-GW is a difficult challenge. To address this issue, we propose the use of a physically based and distributed hydrological model, called WEP-L, in order to analyze the effects of the SW-GW interaction and its spatiotemporal variation characteristics in the Xiaoqing River basin. We demonstrate that the SW-GW interaction is significantly affected by season. The simulated annual average
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Jin, Jing, Tiejun Liu, Mingxin Wang, Zilong Liao, and Jing Zhang. "Hydrochemical and Isotopic Explanations of the Interaction between Surface Water and Groundwater in a Typical-Desertified Steppe of Northern China." Sustainability 15, no. 14 (2023): 11034. http://dx.doi.org/10.3390/su151411034.

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The Tabu catchment, a typical-desertified steppe in China, was selected as the study area to qualitatively analyze the interaction between surface water (SW) and groundwater (GW), and an integration of hydrochemical analysis and isotopic techniques was applied. The results show that the ion contents in SW and GW increased from upstream to downstream, and the hydrochemical evolutions were both controlled by rock weathering and influenced by evaporation. The δD–δ18O lines of SW and GW were δD = 5.14δ18O − 24.68 and δD = 6.89δ18O − 5.81, respectively. Along the I–I′ profile, the contents of most
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Zhang, Lu, Yunfeng Dai, Jin Lin, et al. "Evaluating Spatiotemporal Variations of Groundwater–Surface Water Interaction Using an Integrated Hydrological Model in Huashan Basin, China." Sustainability 14, no. 21 (2022): 14325. http://dx.doi.org/10.3390/su142114325.

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Quantifying the spatiotemporal variations of basin-scale surface water (SW)–groundwater (GW) interactions is vital for the conjunctive management of water resources in the basin. In this study, an integrated hydrological model (SWAT-MODFLOW) is used to simulate the SW–GW system in the Huashan Basin. The numerical model was calibrated and validated using the streamflow observations of the watershed outlet and the groundwater levels of the long-term monitoring wells from 2016 to 2020 in the study area. The model results show that the SWAT–MODFLOW can achieve a better fit for the streamflow disch
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Soleimani, Shima, Omid Bozorg-Haddad, Arezoo Boroomandnia, and Hugo A. Loáiciga. "A review of conjunctive GW-SW management by simulation–optimization tools." Journal of Water Supply: Research and Technology-Aqua 70, no. 3 (2021): 239–56. http://dx.doi.org/10.2166/aqua.2021.106.

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Abstract The conjunctive use of groundwater and surface water (GW-SW) resources has grown worldwide. Optimal conjunctive water use can be planned by coupling hydrologic models for the simulation of water systems with optimization techniques for improving management strategies. The coupling of simulation and optimization methods constitutes an effective approach to determine sustainable management strategies for the conjunctive use of these water resources; yet, there are challenges that must be addressed. This paper reviews (1) hydrologic models applied for the simulation of GW-SW interaction
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Zhang, Jia, Aidi Huo, Zhixin Zhao, et al. "Impact of Mountain Reservoir Construction on Groundwater Level in Downstream Loess Areas in Guanzhong Basin, China." Water 14, no. 9 (2022): 1470. http://dx.doi.org/10.3390/w14091470.

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An accurate understanding of the relationship between reservoir construction and the dynamic change of groundwater level in downstream areas is of great significance for rational development and utilization of water resources. At present, the research on the interaction between surface water (SW) and groundwater (GW) mainly focuses on the interaction between river and GW. There are few studies on the impact of the reservoir construction on GW level in downstream loess irrigation area. Rainfall, evaporation and climate temperature have a great impact on W level, but the impact of reservoir cons
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Azzirgue, El Mustapha, El Khalil Cherif, Hamza El El Azhari, et al. "Interactions Evaluation between the Jouamaa Hakama Groundwater and Ouljat Echatt River in the North of Morocco, Using Hydrochemical Modeling, Multivariate Statistics and GIS." Water 15, no. 9 (2023): 1752. http://dx.doi.org/10.3390/w15091752.

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The processed discharges from Tangier Automotive City’s (TAC) Chrafate Wastewater Treatment Plant (WWTP) contaminate the Jouamaa Hakama groundwater and the Ouljat Echatt river. We aimed to study the unknown interactions between surface water (SW) and groundwater (GW). A total of nine Jouamaa Hakama GW samples and eleven Ouljat Echatt SW samples were taken and analyzed in 2021 and 2022 to determine 16 physical and chemical parameters (pH, temperature (T), electrical conductivity (EC), dissolved oxygen (DO), total hardness (TH), turbidity (TURB), and total dissolved solids (TDS), cations: Na+, K
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Sangeetha, K., Balaji Narasimhan, and R. Srinivasan. "A Coupled SWAT-AEM Modelling Framework for a Comprehensive Hydrologic Assessment." Water 14, no. 17 (2022): 2753. http://dx.doi.org/10.3390/w14172753.

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This study attempts to integrate a Surface Water (SW) model Soil and Water Assessment Tool (SWAT) with an existing steady-state, single layer, unconfined heterogeneous aquifer Analytic Element Method (AEM) based Ground Water (GW) model, named Bluebird AEM engine, for a comprehensive assessment of SW and GW resources and its management. The main reason for integrating SWAT with the GW model is that the SWAT model does not simulate the distribution and dynamics of GW levels and recharge rates. To overcome this issue, often the SWAT model is coupled with the numerical GW model (either using MODFL
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Thèses sur le sujet "SW-GW interaction"

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PERICO, ROBERTA. "GROUNDWATER-SURFACE WATER INTERACTION IN ALPINE CATCHMENT." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2022. http://hdl.handle.net/10281/374727.

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L'evidenza riconosciuta del riscaldamento globale richiede una valutazione del ciclo dell'acqua presente e futuro in Europa e nel mondo. Recentemente, è stata documentata l'evidenza di un regime idrologico modificato nelle Alpi sotto il cambiamento climatico. Tuttavia, secondo il quinto rapporto di valutazione dell'IPCC, è ancora necessario approfondire la nostra comprensione dell'impatto del cambiamento climatico e dell'uso del suolo sullo stoccaggio delle acque sotterranee nei bacini idrografici alpini. Una delle maggiori limitazioni all'analisi dell'interazione tra acque superficiali e sott
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Nzama, Stanley Mvuselelo. "Spatial and temporal assessment of groundwater-surface water interaction, Schoonspruit river catchment, North West, South Africa." Diss., 2016. http://hdl.handle.net/10500/22083.

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The study presents the spatio-temporal assessment of groundwater-surface water (GW-SW) interaction aspects in the Schoonspruit River catchment, North West of South Africa. The research study aimed at improving understanding of groundwater and surface water interaction through assessing its location and time when such interaction occurs. GW-SW interaction sites were identified using principal aquifer type characterization methods. The occurrence of the interaction was established using hydrochemistry methods and the effectiveness of the existing monitoring methods were evaluated in their consid
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Chapitres de livres sur le sujet "SW-GW interaction"

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Jafari, Tina, Saman Javadi, and Anthony S. Kiem. "Integrated Simulation of Surfacewater-Groundwater (SW-GW) Interactions Using SWAT-MODFLOW (Case study: Shiraz Basin, Iran)." In Riverine Systems. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-87067-6_7.

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Akhtar, Naseem, Muhammad Izzuddin Syakir, Mohd Talha Anees, Abdul Qadir, and Mohamad Shaiful Yusuff. "Characteristics and Assessment of Groundwater." In Groundwater [Working Title]. IntechOpen, 2020. http://dx.doi.org/10.5772/intechopen.93800.

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Groundwater system is very vital to humanity and the ecosystem. Aquifers are determined based on the absence or presence of water table positioning, that is, confined, unconfined, leaky aquifers and fractured aquifers. The objective of this chapter is to discuss the characteristic and assessment of groundwater within the scope of vertical distribution of GW, types of the aquifer system, types of SW-GW interface, and SW-GW interaction at both local and regional scales. The properties of the aquifer depend on the physical characteristics of the materials (porosity, permeability, specific yield,
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Actes de conférences sur le sujet "SW-GW interaction"

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Blanc, Théo, Philip Brunner, Rolf Kipfer, Matthias Brennwald, and Morgan Peel. "Gases as artificial tracers to study SW-GW interactions." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.19920.

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