摘要
影响沙堆自组织临界性的内因是沙堆的规模和沙堆的组织结构,影响沙堆自组织临界性的外因是外界的扰动.沙堆的规模和沙堆的组织结构决定了沙堆是否能够出现自组织临界性.外界扰动的方式不同,自组织临界性出现的临界点不同;扰动强弱不同,会出现自组织临界性与非自组织临界性的分叉;外界的扰动表明怎样才能够出现自组织临界性以及自组织临界性出现的临界点,它只有通过沙堆的规模和沙堆的组织结构才能起作用.当内外因相互作用,使得系统在临界态能够维持其宏观上的稳定性的时候,自组织临界性就会出现.
Internal causes of working on selforganized criticality of sandpiles are the size and structure of sandpiles, and external cause is the outside perturbation. The size and structure of sandpiles determine sandpiles whether or not can appear selforganized criticality. Different ways of perturbation has different critical point at which selforganized criticality appears; Different intensity of perturbation causes branching between selforganized criticality and nonselforganized criticality; The perturbation shows how selforganized criticality appears and the critical point at which it appears; The perturbation works on selforganized criticality only by the size and structure of sandpiles. Selforganized criticality appears when internal and external causes act each other, and maintain macroscopic stabilization of sandpiles in the critical state.
出处
《科技通报》
北大核心
2003年第4期278-281,共4页
Bulletin of Science and Technology
基金
国家自然科学基金(50278080)
高等学校博士点专项基金(200061307)资助项目
关键词
凝聚态物理学
非线性
自组织临界性
沙粒级配
幂律分布
condensed matter physics
non-linearity
self-organized criticality
particle size distribution
power-law distribution