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近年来,许多文章研究了互层矿物的X射线粉末衍射计算问题,其中最重要的论文是Hendicks和Teller(1942)关于无数微晶的研究.就小颗粒集合体来说,Kakinoki和Komura(1952,1954a,1954b,1956)的矩阵法似乎是最完全的,因为采用了所有层的结构因子,并且可以处理各种程度的非随机互层.Reynolds和Hower(1970)的程序也有这些功能.Allegra(1964)提出了如果层的状态由相应的位移矢量的状态来表示,那么强度方程
In recent years, many articles have investigated the X-ray powder diffraction calculation of interbedded minerals, the most important of which is Hendicks and Teller’s (1942) study on countless crystallites. For small particle aggregates, Kakinoki and Komura (1952 , 1954a, 1954b, 1956) seems to be the most complete because the structural factors for all layers are used and various degrees of non-random interlaminarization are possible.The programs of Reynolds and Hower (1970) also have these functions.Allegra (1964) proposed that if the state of a layer is represented by the state of the corresponding displacement vector, the intensity equation