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Laboratory layered latte

机译:实验室分层拿铁

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Inducing thermal gradients in fluid systems with initial, well-defined density gradients results in the formation of distinct layered patterns, such as those observed in the ocean due to double-diffusive convection. In contrast, layered composite fluids are sometimes observed in confined systems of rather chaotic initial states, for example, lattes formed by pouring espresso into a glass of warm milk. Here, we report controlled experiments injecting a fluid into a miscible phase and show that, above a critical injection velocity, layering emerges over a time scale of minutes. We identify critical conditions to produce the layering, and relate the results quantitatively to double-diffusive convection. Based on this understanding, we show how to employ this single-step process to produce layered structures in soft materials, where the local elastic properties vary step-wise along the length of the material.
机译:在具有明确定义的初始密度梯度的流体系统中引起热梯度会导致形成明显的分层模式,例如由于双扩散对流而在海洋中观察到的分层模式。相反,有时会在初始状态相当混乱的密闭系统中观察到分层复合流体,例如,通过将浓缩咖啡倒入一杯温牛奶中而形成的拿铁咖啡。在这里,我们报告了将流体注入可混溶相的受控实验,结果表明,在临界注入速度以上,分层会在几分钟的时间内出现。我们确定了产生分层的关键条件,并将结果定量地与双扩散对流联系起来。基于这种理解,我们展示了如何使用此单步过程在柔软的材料中生成分层结构,其中局部弹性特性沿材料的长度逐步变化。

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