水中双层表面活性剂稳定的磁性流体的粘度反常现象

A. V. Lebedev
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摘要

目的:研究水基磁性流体粘度的温度依赖性。测量基于钴铁氧体颗粒的磁性流体的动态粘度,该磁性流体通过双层表面活性剂稳定在水中。月桂酸(第一层)和月桂酸与十二烷基硫酸钠的混合物(第二层)被用作稳定剂。使用配备同轴圆筒系统的 Brookfield DV-II+Pro 旋转粘度计进行测量。粘度计的测量系统使用 KRIO-VT-12-1 恒温器进行恒温。在 0-90C° 温度范围内,测量了基于不同浓度钴铁氧体颗粒的三种磁性流体样品的动态粘度随温度变化的情况。所获得的粘度随温度变化的关系与已知理论预测和实验观察到的煤油基磁性流体的随温度变化的关系截然不同。根据众所周知的理论模型,磁性流体的粘度与基础介质的粘度之比是颗粒浓度的某种普遍函数。不同的模型提供了不同类型的这一特征。但从中可以清楚地看出,粘度比不应取决于温度。对于基于煤油的磁性流体,实验证明其相对粘度会随着温度的升高而降低。然而,根据所获得的结果,水基磁性流体的相对粘度并不会随着温度的升高而降低,反而会显著增加。也就是说,与水的粘度相比,水基磁性流体的粘度随温度升高而降低的速度更慢。观察到的相关性完全违背了已知的煤油基磁性流体的理论和实验模式。获得的结果可能有助于进一步发展通过双层表面活性剂稳定颗粒的胶体水溶液理论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Viscosity Anomalies of Magnetic Fluid Stabilized by a Double Layer of Surfactant in Water
Purpose to study the temperature dependence of the viscosity of a water-based magnetic fluid.Method. Consists of measuring the dynamic viscosity of a magnetic fluid based on cobalt ferrite particles stabilized in water by a double layer of surfactant. Lauric acid (first layer) and a mixture of lauric acid and sodium dodecyl sulfate (second layer) were used as a stabilizer. Measurements were performed using a Brookfield DV-II+Pro rotational viscometer equipped with a coaxial cylinder system. The measuring system of the viscometer was thermostated using a KRIO-VT-12-1 thermostat.Results. The temperature dependences of dynamic viscosity were measured for three samples of magnetic fluid based on cobalt ferrite particles of various concentrations in the temperature range 0–90C°. The obtained temperature dependences of viscosity are radically different from the temperature dependences both predicted by known theories and experimentally observed for kerosene-based magnetic fluids. According to well-known theoretical models, the ratio of the viscosity of the magnetic fluid to the viscosity of the base medium is a certain universal function of particle concentration. Different models offer different types of this feature. But it clearly follows from them that the viscosity ratio should not depend on temperature. For magnetic fluids based on kerosene, it has been experimentally established that its relative viscosity decreases with increasing temperature. However, according to the results obtained, the relative viscosity of a water-based magnetic fluid does not decrease with increasing temperature, but increases significantly. That is, the viscosity of a water-based magnetic fluid decreases more slowly with increasing temperature than the viscosity of water.Conclusion. The observed dependencies completely contradict the known patterns, both theoretical and experimentally established for kerosene-based magnetic fluids. The results obtained may be useful for the further development of the theory of aqueous colloidal solutions with particle stabilization by a double layer of surfactants.
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