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1)  Feigenbaum's Renormalization Group Equation
Feigenbaum重正化群方程
2)  renormalization group equation
重正化群方程
1.
An effective numerical solution of renormalization group equations;
重正化群方程的一种有效数值解法
2.
The description of the critical theory,the definition of the renormalization group of the critical theory,the derivation and the sense of the renormalization group equation as well as the functional equation of the group are discussed.
讨论临界现象的描述、临界理论的重正化群的定义、重正化群方程的导出和意义以及群的泛函方程等,给出 了重正化群在临界理论中的一些应用。
3)  renormalization group equations
重正化群方程
1.
The renormalization group equations for a period-tripling bifurcation in trimodal maps are discussed,and the numerical solutions of their universal functions and scaling factors are obtained.
讨论了三峰映射三倍周期分岔的重正化群方程,并求出其普适函数和标度因子的数值解。
2.
The renormalization group equations for a periodtripling bifurcation in bimodal maps are discussed, and universal functions and scaling factors are solved.
讨论了双峰映射三倍周期分岔的重正化群方程,并求解出其普适函数和标度因子。
4)  Feigenbaum functional equation
Feigenbaum方程
1.
A study is made on the property of a class of simple and accurate solutions to Feigenbaum functional equation, which is piecewisely and fractionally linear function.
研究Feigenbaum方程的一类简单的精确解的性质 ,它为分段分式线性函数 。
5)  Feigenbaum function equation
Feigenbaum函数方程
6)  renormalization group method
重正化群方法
1.
By using the so called renormalization group method,we give a uniformly valid asymptotic expansions of the boundary value problems under consideration.
利用重正化群方法,构造了该边值问题解的一致有效渐近展开式。
2.
The present paper presents an uniformly valid asymptotic expansion for a class of singular perturbation boundary value problems via the renormalization group method.
用重正化群方法,对一类非线性奇异摄动问题构造了一致有效的渐近展式。
3.
The study using the renormalization group method shows that there is a self-organized criticality characterized by the critical cracking probability of the micro-cells in the process of the progressive cracking of the inner micro-cells of rock.
用重正化群方法研究发现 :岩石内部微元累进破坏过程中存在一个可用微元临界破坏概率来表征的自组织临界状态 ;在该临界状态以前 ,微元的破裂是随机、独立和短程相关的 ,岩石蠕变为稳定蠕变 ;在该临界状态以后 ,微元的破裂便是相互协同和长程相关的 ,并且原来随机、无序分布的破裂微元会逐渐向某一吸引域集中而形成宏观贯通的破裂面 ,岩石蠕变为不稳定蠕变 ;与该临界破坏概率相对应的应力值是岩石的长期强度 ,它约为岩石峰值强度的 80 %。
补充资料:正化
【正化】
 (术语)以正道化众生也。无量寿经上曰:“宣流正化。”
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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