Reaction-infiltration instability in a compacting porous medium
Certain geological features have been interpreted as evidence of channelized magma flow in the mantle, which is a compacting porous medium. Aharonov et al. (J. Geophys. Res., vol. 100 (B10), 1995, pp. 20433–20450) developed a simple model of reactive porous flow and numerically analysed its instabil...
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Published in | Journal of fluid mechanics Vol. 852; pp. 5 - 36 |
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Format | Journal Article |
Language | English |
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Cambridge University Press
10.10.2018
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Abstract | Certain geological features have been interpreted as evidence of channelized magma flow in the mantle, which is a compacting porous medium. Aharonov et al. (J. Geophys. Res., vol. 100 (B10), 1995, pp. 20433–20450) developed a simple model of reactive porous flow and numerically analysed its instability to channels. The instability relies on magma advection against a chemical solubility gradient and the porosity-dependent permeability of the porous host rock. We extend the previous analysis by systematically mapping out the parameter space. Crucially, we augment numerical solutions with asymptotic analysis to better understand the physical controls on the instability. We derive scalings for the critical conditions of the instability and analyse the associated bifurcation structure. We also determine scalings for the wavelengths and growth rates of the channel structures that emerge. We obtain quantitative theories for and a physical understanding of, first, how advection or diffusion over the reactive time scale sets the horizontal length scale of channels and, second, the role of viscous compaction of the host rock, which also affects the vertical extent of channelized flow. These scalings allow us to derive estimates of the dimensions of emergent channels that are consistent with the geologic record. |
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AbstractList | Certain geological features have been interpreted as evidence of channelized magma flow in the mantle, which is a compacting porous medium. Aharonov et al. (J. Geophys. Res., vol. 100 (B10), 1995, pp. 20433–20450) developed a simple model of reactive porous flow and numerically analysed its instability to channels. The instability relies on magma advection against a chemical solubility gradient and the porosity-dependent permeability of the porous host rock. We extend the previous analysis by systematically mapping out the parameter space. Crucially, we augment numerical solutions with asymptotic analysis to better understand the physical controls on the instability. We derive scalings for the critical conditions of the instability and analyse the associated bifurcation structure. We also determine scalings for the wavelengths and growth rates of the channel structures that emerge. We obtain quantitative theories for and a physical understanding of, first, how advection or diffusion over the reactive time scale sets the horizontal length scale of channels and, second, the role of viscous compaction of the host rock, which also affects the vertical extent of channelized flow. These scalings allow us to derive estimates of the dimensions of emergent channels that are consistent with the geologic record. Certain geological features have been interpreted as evidence of channelized magma flow in the mantle, which is a compacting porous medium. Aharonov et al. (J. Geophys. Res., vol. 100 (B10), 1995, pp. 20433–20450) developed a simple model of reactive porous flow and numerically analysed its instability to channels. The instability relies on magma advection against a chemical solubility gradient and the porosity-dependent permeability of the porous host rock. We extend the previous analysis by systematically mapping out the parameter space. Crucially, we augment numerical solutions with asymptotic analysis to better understand the physical controls on the instability. We derive scalings for the critical conditions of the instability and analyse the associated bifurcation structure. We also determine scalings for the wavelengths and growth rates of the channel structures that emerge. We obtain quantitative theories for and a physical understanding of, first, how advection or diffusion over the reactive time scale sets the horizontal length scale of channels and, second, the role of viscous compaction of the host rock, which also affects the vertical extent of channelized flow. These scalings allow us to derive estimates of the dimensions of emergent channels that are consistent with the geologic record. |
Author | Katz, Richard F. Rees Jones, David W. |
Author_xml | – sequence: 1 givenname: David W. orcidid: 0000-0001-8698-401X surname: Rees Jones fullname: Rees Jones, David W. email: David.ReesJones@earth.ox.ac.uk organization: Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK – sequence: 2 givenname: Richard F. orcidid: 0000-0001-8746-5430 surname: Katz fullname: Katz, Richard F. organization: Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK |
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CitedBy_id | crossref_primary_10_1007_s12583_020_1301_2 crossref_primary_10_1063_5_0138998 crossref_primary_10_1016_j_chemgeo_2021_120350 crossref_primary_10_1016_j_epsl_2019_115845 crossref_primary_10_1029_2020JE006604 crossref_primary_10_1038_s41598_023_37725_6 crossref_primary_10_1029_2018JB016530 crossref_primary_10_1146_annurev_earth_032320_083704 crossref_primary_10_1029_2021GC009963 crossref_primary_10_1029_2023JB026985 crossref_primary_10_1016_j_epsl_2020_116324 crossref_primary_10_1029_2020GC008937 crossref_primary_10_1093_gji_ggab112 crossref_primary_10_1029_2018GC007880 |
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Snippet | Certain geological features have been interpreted as evidence of channelized magma flow in the mantle, which is a compacting porous medium. Aharonov... Certain geological features have been interpreted as evidence of channelized magma flow in the mantle, which is a compacting porous medium. Aharonov et al. (... Certain geological features have been interpreted as evidence of channelized magma flow in the mantle, which is a compacting porous medium. Aharonov et al. (J.... |
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SubjectTerms | Advection Bifurcations Channels Compacting Control stability Dimensions Equilibrium Flow stability Fluid mechanics Growth rate Infiltration Instability JFM Papers Lava Magma Mapping Mathematical models Numerical analysis Organic chemistry Permeability Porosity Porous media Rocks Stability analysis Wavelengths |
Title | Reaction-infiltration instability in a compacting porous medium |
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