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Rheological properties of magnetite suspensions

机译:磁铁矿悬浮液的流变特性

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Rheological properties of aqueous suspensions ofmagnetite, varying in particle size distribution and solids contenthave been studied.Three models, the Bingham, the Herschel - Bulkley, and theCasson were found to describe the experimental flow curves quitewell. The Casson model turned out to be very effective indescribing the flow curves in a broad range of magnetite particlesizes (from d_(63.2) = 30 #mu#m resembling commercialmagnetite down to a micronized magnetite with d_(63.2) = 2.7##mum), and over the solid content range from 5 percent to 25percent by volume.The two rheological parameters obtained from the experimentaldata using the Casson model, the Casson yield stress and theCasson viscosity were evaluated, and it was concluded that whilethe Casson viscosity was nearly constant over the magnetitemedium density range of 1.3 to 1.7 (5 percent to 20 percent byvolume), the Casson yield stress varied in a predictable way withmagnetite particle size and solids content.
机译:研究了磁铁矿水悬浮液的流变性质,其粒径分布和固体含量各不相同。找到了三种模型,即宾厄姆,赫歇尔-布克利和卡森,可以很好地描述实验流动曲线。事实证明,Casson模型非常有效地描述了各种磁铁矿颗粒尺寸中的流动曲线(从d_(63.2)= 30#mu#m类似于商业磁铁矿,一直到微粉化磁铁矿,d_(63.2)= 2.7 ## mum)。固含量范围为5%至25%(体积)。使用Casson模型从实验数据中获得了两个流变参数,即Casson屈服应力和Casson粘度,得出结论,尽管当磁铁矿的密度范围为1.3至1.7(按体积计5%至20%)时,卡森屈服应力随磁铁矿颗粒尺寸和固体含量的变化而以可预测的方式变化。

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