4.7 Article

Interacting length scales in the reactive-infiltration instability

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 40, Issue 12, Pages 3036-3041

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1002/grl.50564

Keywords

dissolution; porous media; reactive-infiltration instabilities; wormholing

Funding

  1. US Department of Energy, Chemical Sciences, Geosciences and Biosciences Division, Office of Basic Energy Sciences [DE-FG02-98ER14853]
  2. U.S. Department of Energy (DOE) [DE-FG02-98ER14853] Funding Source: U.S. Department of Energy (DOE)

Ask authors/readers for more resources

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 1 mm to 1 km for physically reasonable flow rates and reaction rates. We obtain a closed form for the growth rate when the change in porosity is small.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available