岩体混沌动力系统演化过程的可预测尺度是非线性预测理论研究的重要内容. 在利用传统的理论和方法分析实际问题时, 常常由于观测资料不足而无法计算岩体动力系统的可预测尺度. 为了解决这一问题, 基于胞映射理论提出了一种新的岩体动力系统可预测尺度的计算模型. 该模型基于系统的非线性动力学方程和随机过程理论, 将点到点的映射转化成胞到胞的映射, 以系统演化达到极限状态概率分布前的时段作为系统的可预测尺度, 消除了初值观测误差和系统离散化对系统造成的影响, 从而可以更精确地描述系统的混沌性本质. 实例的应用也表明了这一点.
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