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Methodological considerations for studying self-weight fluidization in a sedimentation column

机译:用于研究沉积柱自身重量流化的方法论

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The objective of this research is to develop a laboratory methodology that facilitates an improved understanding of self-weight fluidization in a batch column. Observations of the fluidization pipes and of the mudline interface are made by means of a digital camera, naked eye and gamma radiation source through repeated runs for a pure kaolinite-water mixture under different initial concentrations and initial suspension heights. Analysis of the experimental results show the onset of self-weight fluidization occurs at an earlier period, during the first falling rate than the second falling rate which has been reported by others. Despite the formation and upward propagation of fluidization pipes no inflection points are observed anywhere atop the mudline interface for the kaolinite mixture. Numerical simulations made via a 1-D sedimentation model that accounts for the upward propagation of fluid further validate the observation of the authors that for the kaolinite mixture, self-weight fluidization cannot be always detected by observing the mudline interface.
机译:本研究的目的是制定一种实验室方法,便于改善批次柱中自我重量流化的理解。通过数码相机,肉眼和伽马辐射源进行流化管和泥线界面的观察,通过在不同的初始浓度和初始悬浮高度下对纯高岭石 - 水混合物的重复运行进行。实验结果的分析表明,在较早的时间内发生自身重量流化的发作,在第一次下降速率之上比其他人报告的第二个下降速率。尽管流化管的形成和向上传播,但在泥土界面的任何地方都没有观察到静脉晶岩系的任何地方。通过1-D沉积模型进行的数值模拟,其考虑流体向上传播进一步验证了对高岭石混合物的作者观察,通过观察泥线界面,不能始终检测自重流化。

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