Groundwater flow equation, overview, derivation, and solution

Darcy’s law is the basic law of flow, and it produces a partial differential equation is similar to the heat transfer equation when coupled with an equation of continuity that explains the conservation of fluid mass during flow through a porous media. This article, titled the groundwater flow equati...

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Autores principales:	El Mezouary Lhoussaine, El Mansouri Bouabid
Formato:	article
Lenguaje:	EN FR
Publicado:	EDP Sciences 2021
Materias:	Environmental sciences GE1-350
Acceso en línea:	https://doaj.org/article/491b7595d0564552812681ed0b960091
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spelling	oai:doaj.org-article:491b7595d0564552812681ed0b9600912021-11-08T15:19:09ZGroundwater flow equation, overview, derivation, and solution2267-124210.1051/e3sconf/202131404007https://doaj.org/article/491b7595d0564552812681ed0b9600912021-01-01T00:00:00Zhttps://www.e3s-conferences.org/articles/e3sconf/pdf/2021/90/e3sconf_wmad2021_04007.pdfhttps://doaj.org/toc/2267-1242Darcy’s law is the basic law of flow, and it produces a partial differential equation is similar to the heat transfer equation when coupled with an equation of continuity that explains the conservation of fluid mass during flow through a porous media. This article, titled the groundwater flow equation, covers the derivation of the groundwater flow equations in both the steady and transient states. We look at some of the most common approaches and methods for developing analytical or numerical solutions. The flaws and limits of these solutions in reproducing the behavior of water flow on the aquifer are also discussed in the article.El Mezouary LhoussaineEl Mansouri BouabidEDP SciencesarticleEnvironmental sciencesGE1-350ENFRE3S Web of Conferences, Vol 314, p 04007 (2021)
institution	DOAJ
collection	DOAJ
language	EN FR
topic	Environmental sciences GE1-350
spellingShingle	Environmental sciences GE1-350 El Mezouary Lhoussaine El Mansouri Bouabid Groundwater flow equation, overview, derivation, and solution
description	Darcy’s law is the basic law of flow, and it produces a partial differential equation is similar to the heat transfer equation when coupled with an equation of continuity that explains the conservation of fluid mass during flow through a porous media. This article, titled the groundwater flow equation, covers the derivation of the groundwater flow equations in both the steady and transient states. We look at some of the most common approaches and methods for developing analytical or numerical solutions. The flaws and limits of these solutions in reproducing the behavior of water flow on the aquifer are also discussed in the article.
format	article
author	El Mezouary Lhoussaine El Mansouri Bouabid
author_facet	El Mezouary Lhoussaine El Mansouri Bouabid
author_sort	El Mezouary Lhoussaine
title	Groundwater flow equation, overview, derivation, and solution
title_short	Groundwater flow equation, overview, derivation, and solution
title_full	Groundwater flow equation, overview, derivation, and solution
title_fullStr	Groundwater flow equation, overview, derivation, and solution
title_full_unstemmed	Groundwater flow equation, overview, derivation, and solution
title_sort	groundwater flow equation, overview, derivation, and solution
publisher	EDP Sciences
publishDate	2021
url	https://doaj.org/article/491b7595d0564552812681ed0b960091
work_keys_str_mv	AT elmezouarylhoussaine groundwaterflowequationoverviewderivationandsolution AT elmansouribouabid groundwaterflowequationoverviewderivationandsolution
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Groundwater flow equation, overview, derivation, and solution

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