根据深部采矿岩体变形的离散性特征,运用元胞自动机建模方法构建深部采矿岩体的变形演化模型;利用元胞岩石的状态变化概率和元胞状态变化的影响系数,实现深部采矿岩体的动力学模拟.在演化模型的基础上,进行了模拟实验,且运用R/S分析法对结果进行分析,得到了以离散度作为岩体稳定性的标准

第六章酶 第一节概述 第二节酶的命名与分类 第三节酶分子的组成与结构 第四节酶催化作用的机制 第五节酶促反应动力学 第七节酶工程简介

一、酶技术 包括酶生物合成的调节技术、酶的分离 纯化技术、酶反应动力学研究技术、酶 的分子修饰技术、酶、细胞及原生质体 固定化技术等

where f:R\×Rn×R→ R\ and g:R\×R\×R→ R are continuous functions. Assume that f, g are continuously differentiable with respect to their first two arguments in a neigborhood of the trajectory co(t), yo(t), and that the derivative

§7-1概述 §7-2机械的运动方程式 §7-3机械运动方程式的求解 §7-4稳定运转状态下机械的周期性速度波动及其调节 §7-5机械的非周期性速度波动及其调节 §7-6考虑构件弹性时的机械动力学简介

地球内部结构划分的依据，地震波走时,波速的变化。国际合作计划，1957-1958国际地球物理年，60年代国际地壳上地幔计划，70年代地球动力学计划，80年代-今岩石圈大断面计划

with x(0)=I exist and are unique on the time interval t E [ 0, 1] for allTER\.Then discrete time system(4. 1)with f(5)=r(, i)describes the evolution of continuous time system(4.)at discrete time samples. In particular, if a is continuous then so is f Let us call a point in the closure of X locally attractive for system(4. 1)if there exists

Definition A real-valued function V: X H R defined on state space X of a system with behavior set B and state r:B×[0,∞)→ X is called a Lyapunov function if tHv(t)=v(a(t))=v(a(z(), t)) is a non-increasing function of time for every z E B according to this definition, Lyapunov

3.1.2 A general uniqueness theorem The key issue for uniqueness of solutions turns out to be the maximal slope of a=a(a) to guarantee uniqueness on time interval T=[to, t,, it is sufficient to require existence of a constant M such that

he variable t is usually referred to as the\time Note the use of an integral form in the formal definition(2.2): it assumes that the function tHa(a(t), t)is integrable on T, but does not require =a(t)to be differentiable at any particular point, which turns out to be convenient for working with discontinuous