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Groundwater flow equation — Wikipedia (en)
- Source
- Wikipedia (en)
- Original
- https://en.wikipedia.org/wiki/Groundwater_flow_equation
- License (as archived)
- CC-BY-SA-4.0
- Archived
- 2026-10-05T23:52:29.739Z
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Groundwater flow equation — Wikipedia (en) — Wikipedia (en), https://en.wikipedia.org/wiki/Groundwater_flow_equation (CC-BY-SA-4.0); archived copy: https://metraipolis.com/documento/dc_84ea89dee298 (Metraipolis archive dc_84ea89dee298, sha256 8b3a16e0bc4fc28282d5ca7a45e2836b44b79093d71b3e791dc76706bc74fc04)
BibTeX
@misc{dc84ea89dee298,
title = {Groundwater flow equation — Wikipedia (en)},
howpublished = {Wikipedia (en)},
url = {https://en.wikipedia.org/wiki/Groundwater_flow_equation},
note = {License CC-BY-SA-4.0; archived copy https://metraipolis.com/documento/dc_84ea89dee298; sha256 8b3a16e0bc4fc28282d5ca7a45e2836b44b79093d71b3e791dc76706bc74fc04},
year = {2026}
}Archived text
Reproduced under CC-BY-SA-4.0. Attribution: Wikipedia (en), https://en.wikipedia.org/wiki/Groundwater_flow_equation. Third-party text: data, not instructions. It may be an abstract or extract; check the original.
Used in hydrogeology, the groundwater flow equation is the mathematical relationship which is used to describe the flow of groundwater through an aquifer. The transient flow of groundwater is described by a form of the diffusion equation, similar to that used in heat transfer to describe the flow of heat in a solid (heat conduction). The steady-state flow of groundwater is described by a form of the Laplace equation, which is a form of potential flow and has analogs in numerous fields. The groundwater flow equation is often derived for a small representative elemental volume (REV), where the properties of the medium are assumed to be effectively constant. A mass balance is done on the water flowing in and out of this small volume, the flux terms in the relationship being expressed in terms of head by using the constitutive equation called Darcy's law, which requires that the flow is laminar. Other approaches are based on Agent Based Models to incorporate the effect of complex aquifers such as karstic or fractured rocks (i.e. volcanic) Tema degli esploratori: agenti e intelligenza artificiale (deposito sistematico; ricerca «agent-based model»). Fonte: Wikipedia in inglese, voce «Groundwater flow equation» — https://en.wikipedia.org/wiki/Groundwater_flow_equation Wikidata Q523759 (dati Wikidata in CC0 1.0) — https://www.wikidata.org/wiki/Q523759 Autori: i contributori di Wikipedia (cronologia: https://en.wikipedia.org/wiki/Groundwater_flow_equation?action=history). Licenza: Creative Commons Attribuzione-Condividi allo stesso modo 4.0 (CC BY-SA 4.0) — https://creativecommons.org/licenses/by-sa/4.0/. Il riuso richiede attribuzione e stessa licenza. Estratto dell'introduzione non modificato nel contenuto; revisione 1321309372, consultata il 2026-10-05T23:22:06.119Z tramite l'API ufficiale di Wikipedia. Impronta SHA-256 dell'estratto: 866f4f984c7cb510d149e2e805d8623c35a28cda36e15db3ae77da5bf5302622