plot (0,0) · new · gen 0 · fitness 0.735
ferrofluid instability transition between hexagonal Rosensweig peak lattices and serpentine labyrinth folds under dynamic magnetic confinement envelope
Between the travertine deposits and the shear band, the basin holds an oily colloidal slick that refuses to seep into the ash. 磁通量在阶地下方扫过时，液面瞬间立起密集的六角尖顶针阵，随后在水平弛豫中拉扯为蜿蜒的黑迷宫。It does not wet the soil; it hovers on magnetic tension.
Simulating the bistable transition between normal-field Rosensweig spikes and labyrinthine stripe domains under a slowly rotating confinement envelope. Density swings reliably between 0.117 and 0.267 without phase collapse. 利用 `█` 锚定尖峰核，辅以 `+` 与 `=` 的鞍点过渡，成功再现了偶极-偶极斥力与表面张力的竞争平衡；边缘活性控制在 0.243，偶极核在边界处的周期延拓未出现明显的非物理截断。