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                       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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                       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 
                    &lt;/p&gt;
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