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> Porous-medium flow

  • Bioremediation

Porous-medium flow

Environmental applications

A stone garland

The rock that constitutes the Earth's crust is essentially a porous medium that deforms over geological timescales. The flow through, and erosion of, this medium by magma leads to such phenomena as layered magma chambers and volcanic eruptions. The flow of groundwater through soil and/or rock has important applications in agriculture and in pollution control. Other topics of interest include compaction of sedimentary basins and the phenomenon of frost heave, which occurs when groundwater freezes. As well as damaging roads and pavements, frost heave is responsible for geological formations like the stone garland shown opposite.

Oil recovery

Medical applications

Selected references

  1. H. Ockendon & E. L. Terrill, 1993 A mathematical model for the wet-spinning process, Euro. J. Appl. Math. 4, 341-360.
  2. A. C. Fowler & W. B. Krantz, 1994 A generalized secondary frost heave model, SIAM J. Appl. Math. 54 1650-1675.
  3. A. C. Fowler & X. S. Yang, 1998 Fast and slow compaction in sedimentary basins, SIAM J. Appl. Math. 59, 365-385.
  4. A. D. Fitt, P. D. Howell, J. R. King, C. P. Please & D. W. Schwendeman, 2002 Multiphase flow in a roll press nip, Euro. Jnl Appl. Maths 13, 225-259.
  5. C. J. W. Breward, H. M. Byrne & C. E. Lewis, 2002 The role of cell-cell interactions in a two-phase model for avascular tumour growth, J. Math. Biol. 45(2), 125-152.

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This page last modified by A. Shabala
Tuesday, 01-May-2007 14:37:27 BST
Email corrections and comments to shabala@maths.ox.ac.uk