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Spontaneous stratification in granular mixtures

机译:颗粒状混合物的自发分层

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Granular materials segregate according to grain size when exposed to periodic perturbations such as vibrations. Moreover, mixtures of grains of different sizes can also spontaneously segregate in the absence of external perturbations: when such a mixture is simply poured onto a pile, the large grains are more likely to be found near the base, while the small grains are more likely to be near the top. Here we report another size-separation effect, which arises when we pour a granular mixture between two vertical plates: the mixture spontaneously stratifies into alternating layers of small and large grains whenever the large grains have larger angle of repose than the small grains. We find only spontaneous segregation, without stratification, when the large grains have smaller angle of repose than the small grains. The stratification is related to the occurrence of avalanches: during each avalanche, the grains separate into a pair of static layers, with the small grains forming a sublayer underneath the layer of large grains.
机译:当暴露于周期性扰动(例如振动)时,颗粒材料会根据晶粒大小分离。此外,在没有外部干扰的情况下,不同大小的谷物混合物也可以自发分离:将这种混合物简单地倒在堆上时,大颗粒更可能在底部附近找到,而小颗粒则更有可能靠近顶部。在这里,我们报告了另一种尺寸分离效果,该效果是在将颗粒状混合物倒入两个垂直板之间时产生的:只要大颗粒的休止角大于小颗粒的静止角,混合物就会自发分层为大颗粒和小颗粒的交替层。当大颗粒的休止角小于小颗粒的休止角时,我们发现只有自发偏析而没有分层。分层与雪崩的发生有关:在每次雪崩期间,晶粒分离为一对静态层,小晶粒在大晶粒层下方形成子层。

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