SpringerImages - Solute contours in a 3D adaptive simulation of double-diffusive convection in a porous medium. A plume of warm, low concentration fluid is convected upward, and a solute boundary layer develops near the bottom of the domain. The adaptivity is driven by a physics-independent indicator as discussed in Sect. , which in this case is related to inter-element jumps in the solutal flux

Solute contours in a 3D adaptive simulation of double-diffusive convection in a porous medium. A plume of warm, low concentration fluid is convected upward, and a solute boundary layer develops near the bottom of the domain. The adaptivity is driven by a physics-independent indicator as discussed in Sect. , which in this case is related to inter-element jumps in the solutal flux

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Fig 10

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Different models for flow in porous media, including the Elder problem and the double-diffusive natural convection problem shown in Fig. 10 , have been studied, as have biological simulations of e.

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