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It follows from the previous equation that, for each of the Cartesian components, e.g. <math>x</math>:
It follows from the previous equation that, for each of the Cartesian components, e.g. <math>x</math>:
:<math>D = \lim_{t \rightarrow \infty} \frac{1}{2t} \langle \vert x_i(t) - x_i(0) \vert^2\rangle  </math>,
:<math>D = \lim_{t \rightarrow \infty} \frac{1}{2} \langle \vert x_i(t) \cdot x_i(0) \vert^2\rangle  </math>,
for every particle <math>i</math>. Therefore, an average over all particles can be employed in
for every particle <math>i</math>. Therefore, an average over all particles can be employed in
order to improve statistics. The same applies to time averaging: in equilibrium the average
order to improve statistics. The same applies to time averaging: in equilibrium the average
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so several time segments from the same simulation may be averaged for a given interval [2].
so several time segments from the same simulation may be averaged for a given interval [2].
Adding all components, the following also applies:
Adding all components, the following also applies:
:<math>D = \lim_{t \rightarrow \infty} \frac{1}{6t } \langle \vert \mathbf{r}_i(t) - \mathbf{r}_i(0) \vert^2\rangle  </math>
:<math>D = \lim_{t \rightarrow \infty} \frac{1}{6} \langle \vert \mathbf{r}_i(t) \cdot \mathbf{r}_i(0) \vert^2\rangle  </math>
 


==Green-Kubo relation==
==Green-Kubo relation==
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