Groundwater flow in a fissurised porous stratum (Articolo in rivista)

Type
Label
  • Groundwater flow in a fissurised porous stratum (Articolo in rivista) (literal)
Anno
  • 2010-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.3934/nhm.2010.5.765 (literal)
Alternative label
  • Bertsch M.; Nitsch C. (2010)
    Groundwater flow in a fissurised porous stratum
    in Networks and heterogeneous media
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Bertsch M.; Nitsch C. (literal)
Pagina inizio
  • 765 (literal)
Pagina fine
  • 782 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 5 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 18 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 4 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Bertsch: IAC-CNR and Univ. Roma Tor Vergata; Nitsch: Univ. di Napoli Federico II (literal)
Titolo
  • Groundwater flow in a fissurised porous stratum (literal)
Abstract
  • Barenblatt e. a. introduced a fluid model for groundwater flow in fissurised porous media. The system consists of two diffusion equations for the groundwater levels in, respectively, the porous bulk and the system of cracks. The equations are coupled by a fluid exchange term. Numerical evidence suggests that the penetration depth of the fluid increases dramatically due to the presence of cracks and that the smallness of certain parameter values play a key role in this phenomenon. In the present paper we give precise estimates for the penetration depth in terms of the smallness of some of the parameters. (literal)
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