Reference : Comparative analysis between analytical approximations and numerical solutions descri...
Scientific journals : Article
Engineering, computing & technology : Geological, petroleum & mining engineering
http://hdl.handle.net/2268/3414
Comparative analysis between analytical approximations and numerical solutions describing recession flow in unconfined hillslope aquifers
English
Rocha, David [Katholieke Universiteit Leuven - KUL > Geologie-Geografie > Hydrogeologie en Ingenieursgeologie > >]
Feyen, Jan [Katholieke Universiteit Leuven - KUL > Department of Land Management and Economics > Division Soil and Water > >]
Dassargues, Alain mailto [Université de Liège - ULg > Département Argenco : Secteur GEO3 > Hydrogéologie & Géologie de l'environnement >]
2007
Hydrogeology Journal
Springer Science & Business Media B.V.
15
6
1077-1091
Yes (verified by ORBi)
International
1431-2174
New York
NY
[en] groundwater flow ; analytical approximations ; numerical solutions ; numerical modeling ; Boussinesq equation
[en] Recession flow of aquifers from a hillslope can be described by the non-linear Boussinesq equation. Under strong assumptions and for specific conceptual formulations, different authors derived analytical approximations or linearized versions to this partial differential equation. A comparative analysis between some analytical approximations of the Boussinesq equation and the numerical solution of the recession flow of an unconfined homogeneous aquifer (horizontal, inclined and concave aquifer floor) was carried out. The objective was to define the range where the analytical solutions approximate the numerical solution. The latter was considered in this study as the reference method, because it requires fewer assumptions. From the considered analytical approximations, exponential decay relationships were found to be mainly valid for fine domain materials when horizontal, mild slopes (less than 2%) and concave aquifer floors were considered, but failed to reproduce coarse aquifer numerical model outflows, in contrast to the quadratic decay relationship, which better reproduce outflows in such domains. On the basis of the comparative analysis, it has been found that recession flows obtained with the considered analytical approximations yield similar values only for certain ranges of aquifer properties and geometries.
Aquapôle - AQUAPOLE
Researchers ; Professionals
http://hdl.handle.net/2268/3414
10.1007/s10040-007-0170-4
http://www.springerlink.com/content/45745h4711g05450/
We acknowledge Springer. The original publication is available at www.springerlink.com

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