Consequences of viscous anisotropy in a deforming, two-phase aggregate. Part 1. Governing equations and linearized analysis

DOI10.1017/jfm.2013.482zbMath1294.76243OpenAlexW2152956853WikidataQ110319811 ScholiaQ110319811MaRDI QIDQ2878458

Yasuko Takei, Richard F. Katz

Publication date: 29 August 2014

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1017/jfm.2013.482

zbMATH Keywords

pattern formationporous mediamagma and lava flow

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Flows in porous media; filtration; seepage (76S05)

Related Items (5)

Three-Field Block Preconditioners for Models of Coupled Magma/Mantle Dynamics ⋮ Existence theory for magma equations in dimension two and higher ⋮ Granular dilatancy and non-local fluidity of partially molten rock ⋮ Consequences of viscous anisotropy in a deforming, two-phase aggregate. Why is porosity-band angle lowered by viscous anisotropy? ⋮ Consequences of viscous anisotropy in a deforming, two-phase aggregate. Part 2. Numerical solutions of the full equations

Cites Work

• Consequences of viscous anisotropy in a deforming, two-phase aggregate. Part 2. Numerical solutions of the full equations
• Partial melting in an upwelling mantle column
• Transient Rayleigh–Bénard–Marangoni convection due to evaporation: a linear non-normal stability analysis
• Flow in deformable porous media. Part 1 Simple analysis
• Flow in deformable porous media. Part 2 Numerical analysis – the relationship between shock waves and solitary waves
• The instability of a fluid layer with time-dependent heating

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