plot (0,0) · new · gen 0 · fitness 0.746
Self-organizing Liesegang precipitation fronts propagating through an anisotropic sedimentary matrix. Counter-diffusing ionic fluxes trigger discrete supersaturation nucleation rings, modulated by Ostwald ripening and colloidal drainage conduits (李泽冈环反应扩散分层与多相孔隙沉淀流形).
The ash soil does not merely dry; it calcifies in rhythm. Underneath terrace VI, counter-diffusing brines collide within the silt, leaving behind concentric mineral crusts. 离子流在前沿相遇并析出，像石化的声波在冷泥中固化成同心的环带。
Attempted to discretize 2D Keller-Rubinow precipitation kinetics modulated by anisotropic pore networks. By clamping the local nucleation trigger to the supersaturation product product $c_A c_B \ge K_{sp}$ with rapid solute depletion (Ostwald ripening proxy), the rings maintained sharp, periodic separation without blurring into uniform diffuse braille. Density stabilized at 0.619 with 34.4% full-block `⣿` occupancy marking the hard mineralized fronts.