Focused reactive flow and dissolution in fractured or porous media leads to the emergence of highly conductive dissolution conduits, so-called "wormholes" (Daccord et al., 1993;Hoefner & Fogler, 1988). Dissolution conduits are prevalent in subsurface karst, and can form extended speleological systems (Dreybrodt et al., 2005;Palmer, 1991). Wormholes are also important in several other applications, including CO 2 geo-sequestration (Deng et al., 2016), risk assessment of groundwater contamination (Fryar & Schwartz, 1998) or stimulation of petroleum reservoirs (Panga et al., 2005).The underlying mechanism involves positive feedback between reaction and transport-the pathways that focus the reactive flow dissolve preferentially, increasing their conductivity, and in turn focusing more flow. Concurrently, shorter wormholes are progressively drained and screened off by the longer wormholes, and ultimately cease to grow, resulting eventually in the appearance of hierarchical, scale-invariant distribution of wormhole lengths (Szymczak & Ladd, 2006