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STRUCTURE-RELATED ANOMALOUS DIFFUSION IN ZEOLITES

机译:沸石结构相关的异常扩散

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For anomalous diffusion the dependence of the mean square displacement < r~2(t) > on the diffusion time t usually differs from the linear dependence expected for the normal (i.e. Fickian) diffusion < r~2(t) > = 2dDt. (1) Eq.1 is known as the Einstein's equation with D and d denoting the self-diffusion coefficient and the dimensionality of the diffusion space, respectively. Proportionality between the mean square displacement and the diffusion time in Eq.1 may be easily rationalised when describing the diffusion as a random walk. In this case it is assumed that during a certain elementary time interval τ each particle makes a diffusion step of length l in arbitrary direction. Assuming further that the particle displacements during different elementary time intervals (i≠j) are uncorrelated we obtain < r~2(t = nτ) > = < ∑ from i=1 to n of r_i r_i > + < ∑ from i≠j=1 to n of r_i r_j > = n (l)~2 ∝ t, (2) where r_i is the displacement vector in the i-th interval of time. Under the conditions of anomalous diffusion, displacements in different time intervals are usually correlated, so that the second sum in Eq.2 does not vanish as in the case of normal diffusion and, consequently, the mean square displacement cannot be expected to increase proportionally to the diffusion time t.
机译:对于异常扩散,平均方位位移在扩散时间t的依赖性通常与正常(即fickian)扩散 = 2ddt的线性依赖性不同。 (1)EQ.1被称为EINSTEIN的与D和D表示分别的自扩散系数和扩散空间的维度。当将扩散描述为随机行走时,可以容易地合理地在均方位移与EQ.1中的扩散时间之间的比例。在这种情况下,假设在某个基本时间间隔τ期间每个粒子使得长度L的扩散步骤以任意的方向。假设在不同基本时间间隔(I≠j)期间的粒子位移是不相关的,我们从i≠j的r_i r_i> + <σ的i = 1到n获得 = <σ. = 1到n的R_I r_j> = n(l)〜2αt,(2)在第i个时间间隔内的r_i是位移向量。在异常扩散的条件下,不同时间间隔的位移通常是相关的,因此在EQ.2中的第二和在正常扩散的情况下不会消失,因此,通常不能预期平均方形位移到扩散时间t。

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