On a shallow water model for the simulation of turbidity currents

On a shallow water model for the simulation of turbidity currents. Morales de Luna, T., Castro Díaz, M. J., Parés Madroñal, C., & Fernández Nieto, E. D. Communications in Computational Physics, 6(4):848–882, 2009.

Paper doi abstract bibtex

We present a model for hyperpycnal plumes or turbidity currents that takes into account the interaction between the turbidity current and the bottom, considering deposition and erosion effects as well as solid transport of particles at the bed load due to the current. Water entrainment from the ambient water in which the turbidity current plunges is also considered. Motion of ambient water is neglected and the rigid lid assumption is considered. The model is obtained as a depth-average system of equations under the shallow water hypothesis describing the balance of fluid mass, sediment mass and mean flow. The character of the system is analyzed and numerical simulations are carried out using finite volume schemes and path-conservative Roe schemes.

@Article{moralesdeluna2009shallow,
  Title                    = {On a shallow water model for the simulation of turbidity currents},
  Author                   = {Morales de Luna, Tom\'{a}s and Castro D\'{i}az, Manuel J. and Par\'{e}s Madro\~{n}al, Carlos and Fern\'{a}ndez Nieto, Enrique D.},
  Journal                  = {Communications in Computational Physics},
  Year                     = {2009},
  Number                   = {4},
  Pages                    = {848--882},
  Volume                   = {6},

  Abstract                 = {We present a model for hyperpycnal plumes or turbidity currents that takes into account the interaction between the turbidity current and the bottom, considering deposition and erosion effects as well as solid transport of particles at the bed load due to the current. Water entrainment from the ambient water in which the turbidity current plunges is also considered. Motion of ambient water is neglected and the rigid lid assumption is considered. The model is obtained as a depth-average system of equations under the shallow water hypothesis describing the balance of fluid mass, sediment mass and mean flow. The character of the system is analyzed and numerical simulations are carried out using finite volume schemes and path-conservative Roe schemes.},
  Category                 = {PHYSICS, MATHEMATICAL},
  Comment                  = {�ndice de impacto: 2.077, Revista dentro del 25%: S�, Posici�n: 8, Fuente de impacto: WOS (JCR), Num. revistas en cat.: 47, Categor�a: PHYSICS, MATHEMATICAL},
  Doi                      = {10.4208/cicp.2009.v6.p848},
  File                     = {:moralesdeluna09shallow.pdf:PDF},
  Impactfactor             = {2.077},
  Keywords                 = {Turbidity currents, hyperbolic systems, finite volume methods, path-conservative schemes, numerical modeling},
  Position                 = {8},
  Revincat                 = {47},
  Url                      = {http://www.global-sci.com/cgi-bin/fulltext/6/848/full}
}

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