Forchheimer flow to a well-considering time-dependent critical radius

Previous studies on the non-Darcian flow into a pumping well assumed that critical radius (<i>R</i><sub>CD</sub>) was a constant or infinity, where <i>R</i><sub>CD</sub> represents the location of the interface between the non-Darcian flow region and D...

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Main Authors: Q. Wang, H. Zhan, Z. Tang
Format: Article
Language:English
Published: Copernicus Publications 2014-06-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/18/2437/2014/hess-18-2437-2014.pdf
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spelling doaj-7ee2315ebeb34bca9b5d0abc60a418e72020-11-24T22:44:20ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382014-06-011862437244810.5194/hess-18-2437-2014Forchheimer flow to a well-considering time-dependent critical radiusQ. Wang0H. Zhan1Z. Tang2School of Environmental Studies, China University of Geosciences, Wuhan, Hubei, 430074, PR ChinaSchool of Environmental Studies, China University of Geosciences, Wuhan, Hubei, 430074, PR ChinaSchool of Environmental Studies, China University of Geosciences, Wuhan, Hubei, 430074, PR ChinaPrevious studies on the non-Darcian flow into a pumping well assumed that critical radius (<i>R</i><sub>CD</sub>) was a constant or infinity, where <i>R</i><sub>CD</sub> represents the location of the interface between the non-Darcian flow region and Darcian flow region. In this study, a two-region model considering time-dependent <i>R</i><sub>CD</sub> was established, where the non-Darcian flow was described by the Forchheimer equation. A new iteration method was proposed to estimate <i>R</i><sub>CD</sub> based on the finite-difference method. The results showed that <i>R</i><sub>CD</sub> increased with time until reaching the quasi steady-state flow, and the asymptotic value of <i>R</i><sub>CD</sub> only depended on the critical specific discharge beyond which flow became non-Darcian. A larger inertial force would reduce the change rate of <i>R</i><sub>CD</sub> with time, and resulted in a smaller <i>R</i><sub>CD</sub> at a specific time during the transient flow. The difference between the new solution and previous solutions were obvious in the early pumping stage. The new solution agreed very well with the solution of the previous two-region model with a constant <i>R</i><sub>CD</sub> under quasi steady flow. It agreed with the solution of the fully Darcian flow model in the Darcian flow region.http://www.hydrol-earth-syst-sci.net/18/2437/2014/hess-18-2437-2014.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Q. Wang
H. Zhan
Z. Tang
spellingShingle Q. Wang
H. Zhan
Z. Tang
Forchheimer flow to a well-considering time-dependent critical radius
Hydrology and Earth System Sciences
author_facet Q. Wang
H. Zhan
Z. Tang
author_sort Q. Wang
title Forchheimer flow to a well-considering time-dependent critical radius
title_short Forchheimer flow to a well-considering time-dependent critical radius
title_full Forchheimer flow to a well-considering time-dependent critical radius
title_fullStr Forchheimer flow to a well-considering time-dependent critical radius
title_full_unstemmed Forchheimer flow to a well-considering time-dependent critical radius
title_sort forchheimer flow to a well-considering time-dependent critical radius
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2014-06-01
description Previous studies on the non-Darcian flow into a pumping well assumed that critical radius (<i>R</i><sub>CD</sub>) was a constant or infinity, where <i>R</i><sub>CD</sub> represents the location of the interface between the non-Darcian flow region and Darcian flow region. In this study, a two-region model considering time-dependent <i>R</i><sub>CD</sub> was established, where the non-Darcian flow was described by the Forchheimer equation. A new iteration method was proposed to estimate <i>R</i><sub>CD</sub> based on the finite-difference method. The results showed that <i>R</i><sub>CD</sub> increased with time until reaching the quasi steady-state flow, and the asymptotic value of <i>R</i><sub>CD</sub> only depended on the critical specific discharge beyond which flow became non-Darcian. A larger inertial force would reduce the change rate of <i>R</i><sub>CD</sub> with time, and resulted in a smaller <i>R</i><sub>CD</sub> at a specific time during the transient flow. The difference between the new solution and previous solutions were obvious in the early pumping stage. The new solution agreed very well with the solution of the previous two-region model with a constant <i>R</i><sub>CD</sub> under quasi steady flow. It agreed with the solution of the fully Darcian flow model in the Darcian flow region.
url http://www.hydrol-earth-syst-sci.net/18/2437/2014/hess-18-2437-2014.pdf
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