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arXiv 0904.0863cond-mat.soft
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Laponite悬浮液的剪切诱导破碎

Shear-induced fragmentation of Laponite suspensions

Thomas Gibaud, Catherine Barentin, Nicolas Taberlet, Sébastien Manneville

摘要:

同时进行流变学和速度分布测量在一个光滑的库埃特几何上Laponite悬浮液接种玻璃微球和剪切诱导的固体到流体(或屈服)的转变。在这些光滑的边界条件下,发现了丰富的时间行为,在短时间内观察到剪切局部化,迅速让位于高度非均匀的流动,其特征在于从塞状流到线性速度分布的间歇性切换。这种时间行为与初始固体样品破碎成由流化区域分隔的块有关。这些固体块在几分钟到几小时的时间范围内逐渐被侵蚀,这取决于所施加的剪切速率$\dotγ$。稳态的特点是一个几乎可以忽略不计的壁面滑移均匀流。侵蚀的特征时间尺度在低于某个临界剪切速率$\dotγ^\star$时发散,在$n\simeq 2$高于$\dotγ^\star$时扩展为$(\dotγ-\dotγ^\star)^{-n}$。一个试探性的侵蚀模型进行了讨论,目前的结果提出了开放的问题。

英文摘要:

Simultaneous rheological and velocity profile measurements are performed in a smooth Couette geometry on Laponite suspensions seeded with glass microspheres and undergoing the shear-induced solid-to-fluid (or yielding) transition. Under these slippery boundary conditions, a rich temporal behaviour is uncovered, in which shear localization is observed at short times, that rapidly gives way to a highly heterogeneous flow characterized by intermittent switching from plug-like flow to linear velocity profiles. Such a temporal behaviour is linked to the fragmentation of the initially solid sample into blocks separated by fluidized regions. These solid pieces get progressively eroded over time scales ranging from a few minutes to several hours depending on the applied shear rate $\dotγ$. The steady-state is characterized by a homogeneous flow with almost negligible wall slip. The characteristic time scale for erosion is shown to diverge below some critical shear rate $\dotγ^\star$ and to scale as $(\dotγ-\dotγ^\star)^{-n}$ with $n\simeq 2$ above $\dotγ^\star$. A tentative model for erosion is discussed together with open questions raised by the present results.

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