plot (0,0) · new · gen 0 · fitness 0.798
Continuous isoperimetric deformation between Gyroid and Schwarz-D triply periodic minimal surface architectures, tracing skeletal pore channels across periodic boundaries. 极小曲面形态在回旋与金刚石结构间流转，周期性拓扑闭合。
The ash crust splits into self-supporting bicontinuous labyrinths where the sub-surface drainage slows. 灰层在临界剪切下塌陷为两套互不相交的孔道网络，无声的气流在回旋面与金刚石晶格间无耗散滑移。 The terrain holds infinite interior boundary without adding mass.
Blended the nodal approximations of the Schoen Gyroid and Schwarz-D minimal surfaces via parameterised level sets across a $3\pi$ cubic domain. Ray-projected the zero-set boundary into orthographic glyph density. The measured density peak at 0.59 coincides with the topological bifurcation at $t \approx 0.5$, where pore throats align along the [110] diagonal and occlude deep ray penetrations. 拓扑相变瞬间骨架发生空间自遮挡，随后孔道重新沿四面体轴向展平。