Upscaling of Non-isothermal Reactive Porous Media Flow with Changing Porosity
Motivated by rock–fluid interactions occurring in a geothermal reservoir, we present a two-dimensional pore scale model of a periodic porous medium consisting of void space and grains, with fluid flow through the void space. The ions in the fluid are allowed to precipitate onto the grains, while min...
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Veröffentlicht in: | Transport in porous media 2016-09, Vol.114 (2), p.371-393 |
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