摘要
在数学地质中,一般计算马尔柯夫转移概率矩阵序列极限时,都是用升高矩阵乘幂的方法,所以计算量是很大的。本文用解线性方程组的方法,求出了它的极限概率矩阵,并以实例对两种方法进行比较。
In mathematical geology , the sequential limit of a Markov tramsition probability matrix is generally performed by the method of raising the matrix power, which made,the calculation is of large quantity ,In this paper,the limit probability matrix has been performed by finding the solution of linear equations and a example has been given to compare the results of two different mathods.
关键词
转移概率矩阵
马尔可夫
收敛性
transition probability matrix,nonncgativc matrix ,irreducible matrix, primitive matrix.
