含水铁流体的流变学:在强磁场中从凝胶性质转变为液体性质

IF 2.8 Q2 ENGINEERING, CHEMICAL
Stanislav Čampelj
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引用次数: 0

摘要

使用外加磁场下的流变学测量来研究含水铁磁流体的内部结构和稳定性的变化。通过使用柠檬酸作为表面活性剂将1.8wt.%的磁赤铁矿纳米颗粒分散在水中来制备铁磁流体,磁赤铁矿纳米粒子的尺寸为d=14±3nm,饱和磁化强度MS=68emu/g。在本研究中,使用振荡试验来研究磁流体在磁场B影响下的内部结构变化和稳定性。在大约50mT的磁场中,由于磁流体表现出凝胶状特征,G′变得高于损耗模量G〃。然而,在大约200mT的磁场下,铁磁流体的特性恢复为液体的特性。在这种高磁场中,铁磁流体特性的变化与从链状团聚体到能量上更有利的球状团聚体的逐渐变化有关,使用基于另一项工作中描述的模型的计算。球状团聚体对流动的阻碍程度远小于链,导致粘度降低。磁场的进一步增加导致团聚体的沉积和磁流变效应的损失。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Rheology of Aqueous Ferrofluids: Transition from a Gel-Like Character to a Liquid Character in High Magnetic Fields
Rheological measurements under an applied magnetic field were used to investigate the changes to the internal structure and stability of an aqueous ferrofluid. The ferrofluid was prepared by dispersing 1.8 wt.% of maghemite nanoparticles with a size of d = 14 ± 3 nm and a saturation magnetization MS = 68 emu/g in water using citric acid as the surfactant. In this study, oscillatory tests were used to investigate the internal structural changes and the stability of ferrofluid under the influence of the magnetic field B. In a magnetic field of approximately 50 mT, the G′ became higher than the loss modulus G″ as the ferrofluid exhibited a gel-like character. However, at a magnetic field of approximately 200 mT, the character of the ferrofluid reverted to that of a liquid. The change in the character of the ferrofluid in this high magnetic field was associated with a gradual change from chain agglomerates to the energetically more favourable globular agglomerates, using a calculation based on a model described in a separate work. The globular agglomerates impeded the flow to a much lesser degree than the chains, causing a reduction in the viscosity. Further increase of the magnetic field resulted in sedimentation of agglomerates and loss of magneto-rheological effect.
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来源期刊
ChemEngineering
ChemEngineering Engineering-Engineering (all)
CiteScore
4.00
自引率
4.00%
发文量
88
审稿时长
11 weeks
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