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arXiv 1404.0318cond-mat.soft
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弱润湿颗粒材料的流变学--实验数据与数值数据的比较

Rheology of weakly wetted granular materials - a comparison of experimental and numerical data

Ruediger Schwarze, Anton Gladkyy, Fabian Uhlig, Stefan Luding

摘要:

剪切单元模拟和弱润湿颗粒(几个体积百分比的液体粘合剂)的实验进行了比较,目的是了解他们的流动流变学。应用实例是由砂和液体粘结材料制成的射芯金属铸造用型芯。实验是用库埃特式旋转粘度计进行的。弱润湿颗粒材料由石英砂和少量牛顿液体组成。为了比较,干砂的实验也进行了修改配置的粘度计。数值模型涉及球形,单分散颗粒与接触力和一个简单的液桥模型的两个颗粒之间的个别毛细桥。不同的液体含量和性质导致不同的流动流变学时,测量剪切应力-应变关系。在弱润湿颗粒材料的实验中,对于所有剪切速率,表观剪切粘度$η_g$与惯性数$I$成反比。相反,在干燥的情况下,在$I$中观察到中等剪切速率下的中间结垢制度成反比二次。在模拟中,这两个缩放制度被发现为干和湿颗粒材料以及。

英文摘要:

Shear cell simulations and experiments of weakly wetted particles (a few volume percent liquid binders) are compared, with the goal to understand their flow rheology. Application examples are cores for metal casting by core shooting made of sand and liquid binding materials. The experiments are carried out with a Couette-like rotating viscometer. The weakly wetted granular materials are made of quartz sand and small amounts of Newtonian liquids. For comparison, experiments on dry sand are also performed with a modified configuration of the viscometer. The numerical model involves spherical, monodisperse particles with contact forces and a simple liquid bridge model for individual capillary bridges between two particles. Different liquid content and properties lead to different flow rheology when measuring the shear stress-strain relations. In the experiments of the weakly wetted granular material, the apparent shear viscosity $η_g$ scales inversely proportional to the inertial number $I$, for all shear rates. On the contrary, in the dry case, an intermediate scaling regime inversely quadratic in $I$ is observed for moderate shear rates. In the simulations, both scaling regimes are found for dry and wet granular material as well.

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