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Nonlinear Viscoelastic Compaction in Sedimentary Basins

Geophysics 2020-01-29 v1 Analysis of PDEs

Abstract

In the mathematical modelling of sediment compaction and porous media flow, the rheological behaviour of sediments is typically modelled in terms of a nonlinear relationship between effective pressure pep_e and porosity ϕ\phi, that is pe=pe(ϕ)p_e=p_e(\phi). The compaction law is essentially a poroelastic one. However, viscous compaction due to pressure solution becomes important at larger depths and causes this relationship to become more akin to a viscous rheology. A generalised viscoelastic compaction model of Maxwell type is formulated, and different styles of nonlinear behaviour are asymptotically analysed and compared in this paper.

Keywords

Cite

@article{arxiv.1003.5373,
  title  = {Nonlinear Viscoelastic Compaction in Sedimentary Basins},
  author = {Xin-She Yang},
  journal= {arXiv preprint arXiv:1003.5373},
  year   = {2020}
}
R2 v1 2026-06-21T15:03:33.065Z