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Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below - MaRDI portal

Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below (Q2457900)

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Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below
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    Double diffusion-driven convective instability of three-dimensional fluid-saturated geological fault zones heated from below (English)
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    23 October 2007
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    double diffusion
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    convective instability
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    critical Rayleigh number
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    geological fault zone
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    analytical solution
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