Effect of Surface Water Level Fluctuations on the Performance of Near-Bank Managed Aquifer Recharge from Injection Wells

Managed aquifer recharge operations are often conducted in near-bank areas to regulate water resources or reduce seawater intrusion. Yet little is known about the influence of surface water level fluctuations at different temporal scales on MAR performance. A generalized conceptual model was develop...

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Autores principales: Peipeng Wu, Jean-Christophe Comte, Lijuan Zhang, Shuhong Wang, Bin Chang
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Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/78465ef174214b40b382d976df07a1c3
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spelling oai:doaj.org-article:78465ef174214b40b382d976df07a1c32021-11-11T19:54:30ZEffect of Surface Water Level Fluctuations on the Performance of Near-Bank Managed Aquifer Recharge from Injection Wells10.3390/w132130132073-4441https://doaj.org/article/78465ef174214b40b382d976df07a1c32021-10-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/3013https://doaj.org/toc/2073-4441Managed aquifer recharge operations are often conducted in near-bank areas to regulate water resources or reduce seawater intrusion. Yet little is known about the influence of surface water level fluctuations at different temporal scales on MAR performance. A generalized conceptual model was developed based on an investigation site in Western China as a basis to simulate the response surface water level fluctuations on the water table, artificially recharged water lens (formed by the artificially recharged water), groundwater flow paths and average travel times (which is an important control on how quickly contaminants are flushed out of aquifers), and the discharge of the artificially recharged aquifer during the surface water level fluctuation. The results showed a fluctuating groundwater table in the artificially recharged near-bank aquifer under the influence of surface water level fluctuations. The peak values of the increment of the groundwater table induced by artificial recharge decreased with the increase of the period and amplitude of surface water level fluctuation, but the trough values of the increment of water table increases with that. The penetration depth of surface water into the aquifer with a fluctuating surface water level leads to a decreasing increment of the groundwater table which follows a power law. The fluctuating surface water level leads to dynamic changes of artificially recharged water lens morphology and a thinner artificially recharged water lens. A mixing zone of recharged water and ambient water could be found in the artificially recharged near-bank area, which is expected to lead to modifications in the geochemical conditions in the artificially recharged near-bank aquifer. A longer period of surface water level fluctuation leads to a longer average travel time, but the larger penetration depth of surface water and amplitude lead to a shorter average travel time. The peak discharge of the near-bank aquifer was found to decrease with the period of surface water level fluctuation, but it increases with penetration depth and amplitude. This study is important in providing insights into the performance of near-bank managed aquifer recharge with respect to surface water level fluctuation.Peipeng WuJean-Christophe ComteLijuan ZhangShuhong WangBin ChangMDPI AGarticlemanaged aquifer rechargenear-bank: surface water level fluctuationsgroundwater flowHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 3013, p 3013 (2021)
institution DOAJ
collection DOAJ
language EN
topic managed aquifer recharge
near-bank: surface water level fluctuations
groundwater flow
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle managed aquifer recharge
near-bank: surface water level fluctuations
groundwater flow
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Peipeng Wu
Jean-Christophe Comte
Lijuan Zhang
Shuhong Wang
Bin Chang
Effect of Surface Water Level Fluctuations on the Performance of Near-Bank Managed Aquifer Recharge from Injection Wells
description Managed aquifer recharge operations are often conducted in near-bank areas to regulate water resources or reduce seawater intrusion. Yet little is known about the influence of surface water level fluctuations at different temporal scales on MAR performance. A generalized conceptual model was developed based on an investigation site in Western China as a basis to simulate the response surface water level fluctuations on the water table, artificially recharged water lens (formed by the artificially recharged water), groundwater flow paths and average travel times (which is an important control on how quickly contaminants are flushed out of aquifers), and the discharge of the artificially recharged aquifer during the surface water level fluctuation. The results showed a fluctuating groundwater table in the artificially recharged near-bank aquifer under the influence of surface water level fluctuations. The peak values of the increment of the groundwater table induced by artificial recharge decreased with the increase of the period and amplitude of surface water level fluctuation, but the trough values of the increment of water table increases with that. The penetration depth of surface water into the aquifer with a fluctuating surface water level leads to a decreasing increment of the groundwater table which follows a power law. The fluctuating surface water level leads to dynamic changes of artificially recharged water lens morphology and a thinner artificially recharged water lens. A mixing zone of recharged water and ambient water could be found in the artificially recharged near-bank area, which is expected to lead to modifications in the geochemical conditions in the artificially recharged near-bank aquifer. A longer period of surface water level fluctuation leads to a longer average travel time, but the larger penetration depth of surface water and amplitude lead to a shorter average travel time. The peak discharge of the near-bank aquifer was found to decrease with the period of surface water level fluctuation, but it increases with penetration depth and amplitude. This study is important in providing insights into the performance of near-bank managed aquifer recharge with respect to surface water level fluctuation.
format article
author Peipeng Wu
Jean-Christophe Comte
Lijuan Zhang
Shuhong Wang
Bin Chang
author_facet Peipeng Wu
Jean-Christophe Comte
Lijuan Zhang
Shuhong Wang
Bin Chang
author_sort Peipeng Wu
title Effect of Surface Water Level Fluctuations on the Performance of Near-Bank Managed Aquifer Recharge from Injection Wells
title_short Effect of Surface Water Level Fluctuations on the Performance of Near-Bank Managed Aquifer Recharge from Injection Wells
title_full Effect of Surface Water Level Fluctuations on the Performance of Near-Bank Managed Aquifer Recharge from Injection Wells
title_fullStr Effect of Surface Water Level Fluctuations on the Performance of Near-Bank Managed Aquifer Recharge from Injection Wells
title_full_unstemmed Effect of Surface Water Level Fluctuations on the Performance of Near-Bank Managed Aquifer Recharge from Injection Wells
title_sort effect of surface water level fluctuations on the performance of near-bank managed aquifer recharge from injection wells
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/78465ef174214b40b382d976df07a1c3
work_keys_str_mv AT peipengwu effectofsurfacewaterlevelfluctuationsontheperformanceofnearbankmanagedaquiferrechargefrominjectionwells
AT jeanchristophecomte effectofsurfacewaterlevelfluctuationsontheperformanceofnearbankmanagedaquiferrechargefrominjectionwells
AT lijuanzhang effectofsurfacewaterlevelfluctuationsontheperformanceofnearbankmanagedaquiferrechargefrominjectionwells
AT shuhongwang effectofsurfacewaterlevelfluctuationsontheperformanceofnearbankmanagedaquiferrechargefrominjectionwells
AT binchang effectofsurfacewaterlevelfluctuationsontheperformanceofnearbankmanagedaquiferrechargefrominjectionwells
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