http://www.cnr.it/ontology/cnr/individuo/prodotto/ID263767
Relevance of solutions to the Navier-Stokes equations for explaining groundwater flow in fractured karst aquifers (Articolo in rivista)
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- Label
- Relevance of solutions to the Navier-Stokes equations for explaining groundwater flow in fractured karst aquifers (Articolo in rivista) (literal)
- Anno
- 2013-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1002/wrcr.20279 (literal)
- Alternative label
Masciopinto C., Palmiotta D. (2013)
Relevance of solutions to the Navier-Stokes equations for explaining groundwater flow in fractured karst aquifers
in Water resources research; AGU, American geophysical union, Washington, DC (Stati Uniti d'America)
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- Masciopinto C., Palmiotta D. (literal)
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- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- CNR, Istituto di Ricerca Sulle Acque (literal)
- Titolo
- Relevance of solutions to the Navier-Stokes equations for explaining groundwater flow in fractured karst aquifers (literal)
- Abstract
- We examine the use of numeric flow solutions of the Navier-Stokes (N-S) equations to
improve flow modeling in fractured karst aquifers. The N-S equations were discretized with
both the meshed finite difference method (FDM) and the meshless smoothed particle
hydrodynamics method. The results using the FDM model were successfully compared with
those taken from the literature. The N-S equations were solved numerically for two
practical problems in karst aquifers: (a) the horizontal displacement of the saltwater/
freshwater sharp interface in fissures due to groundwater overexploitation and (b) the
pressure and velocity profiles in fissures in the vicinity of an injection well. In the first
problem, the numeric N-S solution suggests an exponential time advancement of the
freshwater/saltwater interface in fissures. In the second problem, the unsteady water
velocity and pressure profiles were determined in fissures having variable apertures in the
vicinity of an injection well. The N-S simulation results agreed well with the data collected
during the test, thereby removing any uncertainty in the estimation of the aquifer
transmissivity. (literal)
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