English

Interacting length scales in the reactive-infiltration instability

Geophysics 2013-06-24 v1 Fluid Dynamics

Abstract

The reactive-infiltration instability, which develops when a porous matrix is dissolved by a flowing fluid, contains two important length scales. Here we outline a linear stability analysis that simultaneously incorporates both scales. We show that the commonly used "thin-front" model is a limiting case of a more general theory, which also includes convection-dominated dissolution as another special case. The wavelength of the instability is bounded from below, and lies in the range 1mm to 1km for physically reasonable flow rates and reaction rates. We obtain a closed form for the growth rate when the change in porosity is small.

Keywords

Cite

@article{arxiv.1306.5034,
  title  = {Interacting length scales in the reactive-infiltration instability},
  author = {Piotr Szymczak and Anthony J. C. Ladd},
  journal= {arXiv preprint arXiv:1306.5034},
  year   = {2013}
}

Comments

to be published. in Geophys. Res. Lett

R2 v1 2026-06-22T00:37:53.830Z