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赤铁矿椭圆体干燥沉积物中的裂缝:磁转矩和水动力转矩的相互作用。

Cracks in dried deposits of hematite ellipsoids: Interplay between magnetic and hydrodynamic torques.

机构信息

Soft Materials Laboratory, Department of Physics, Indian Institute of Technology Madras, Chennai 600036, India; Polymer Engineering and Colloid Science Laboratory, Chemical Engineering Department, Indian Institute of Technology Madras, Chennai 600036, India.

Polymer Engineering and Colloid Science Laboratory, Chemical Engineering Department, Indian Institute of Technology Madras, Chennai 600036, India.

出版信息

J Colloid Interface Sci. 2018 Jan 15;510:172-180. doi: 10.1016/j.jcis.2017.09.022. Epub 2017 Sep 12.

Abstract

The orientation and morphology of cracks in coffee-ring like particulate deposit obtained by drying sessile drops containing anisotropic magnetic particles strongly depends on the magnitude of the applied magnetic field and its direction. This opens up the possibility of tuning the micro-structure of cracks via suitable manipulation of magnetic and hydrodynamic torques on the particles which has potential applications in nano-fabrication and field driven self-assembly. We report a systematic study of magnetic field driven self-assembly of hematite ellipsoids in sessile drops dried on solid substrates and resulting crack patterns. The experiments are carried out over a wide range of applied magnetic field strength (|B→|) varying from 0 to 400G and ellipsoids of two different aspect ratios. Dried coffee-ring deposits of ellipsoids in absence of the external applied magnetic field and at low field strength, |B→|≤20G exhibit circular cracks. However, at |B→|⩾30G, the cracks are observed to be linear and perpendicular to the direction of the applied magnetic field. Random cracks are observed in the intermediate field range of 20G<|B→|<30G. Thus our experiments reveal that there exists a critical magnetic field at which the orientation of cracks change from circular to linear. The knowledge of the critical field is exploited to measure the hydrodynamic torque experienced by nano-ellipsoids and fluid velocities during evaporation, which are challenging to measure experimentally.

摘要

通过干燥含有各向异性磁性粒子的悬滴获得的类咖啡环颗粒沉积物中的裂缝的方向和形态强烈依赖于所施加磁场的大小及其方向。这开辟了通过对粒子施加适当的磁和流体动力扭矩来调整裂缝的微结构的可能性,这在纳米制造和场驱动自组装中有潜在的应用。我们报告了在固体基底上干燥的悬滴中,通过磁场驱动赤铁矿椭圆体的自组装以及由此产生的裂缝模式的系统研究。实验在宽范围的外加磁场强度(|B→|)下进行,范围从 0 到 400G,以及两个不同纵横比的椭圆体。在不存在外加磁场的情况下以及在低场强(|B→|≤20G)下,干燥的椭圆体类咖啡环沉积物显示出圆形裂缝。然而,在|B→|≥30G 时,观察到裂缝是线性的并且垂直于施加磁场的方向。在 20G<|B→|<30G 的中间场范围内观察到随机裂缝。因此,我们的实验表明,存在一个临界磁场,在该磁场下,裂缝的方向从圆形变为线性。临界场的知识被利用来测量在蒸发过程中纳米椭圆体经历的流体动力扭矩和流体速度,这在实验上很难测量。

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