Finite element modelling of temperature gradient driven rock alteration and mineralization in porous rock masses
DOI10.1016/S0045-7825(98)00038-3zbMath0954.74076OpenAlexW2046893490MaRDI QIDQ1818460
Chongbin Zhao, Hans B. Muhlhaus, Bruce E. Hobbs
Publication date: 8 February 2001
Published in: Computer Methods in Applied Mechanics and Engineering (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1016/s0045-7825(98)00038-3
mineralizationmass balance equationsfluid-saturated porous rock massesgradient reaction criterionproduction/annihilation termsrock alteration indextemperature gradient driven rock alteration
Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Finite element methods applied to problems in solid mechanics (74S05) Soil and rock mechanics (74L10)
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Cites Work
- Effects of medium thermoelasticity on high Rayleigh number steady-state heat transfer and mineralization in deformable fluid-saturated porous media heated from below
- Analytical solutions for transient diffusion problems in infinite media
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