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The Flowability of Fine Powders in Reduced Gravity Conditions

机译:细粉在降低重力条件下的流动性

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The extrapolation of Qian's semi-theoretical relationship for the transition between cohesive andnon-cohesive powder fluidization behavior into regions of low gravity is studied and a validationexperiment employing fluidization is discussed. The fluidization experiment utilized fine glassand alumina powders in a fluidized bed and was flown onboard NASA's reduced gravity aircraft.The transition region between cohesive and non-cohesive behavior is determined for the glassand alumina powders at gravity levels of 1.8g, 1.0g, 0.38g, and 0.16g. The results are comparedto Qian's model and show fair agreement. The fluidization experiment limitations are discussedand a rotating drum experiment that will reduce the experiment uncertainty, provide quantifiableresults, and is suitable for flight onboard NASA's reduced gravity aircraft is proposed. Therotating drum technique determines the characteristic frequency of the powder's center of area todetect avalanching. The concept is validated by comparing the characteristic frequency obtainedfrom analyzing a cohesive powder to the characteristic frequency obtained from analyzing aflowable powder.
机译:钱氏半理论关系的外推作用用于衔接和过渡的过渡 研究了非粘性粉末向低重力区域的流化行为并进行了验证 讨论了采用流化的实验。流化实验使用了细玻璃 和氧化铝粉末放在流化床中,然后在NASA的重力降低飞机上飞行。 确定玻璃的内聚和非内聚行为之间的过渡区域 和氧化铝粉的重力水平分别为1.8g,1.0g,0.38g和0.16g。比较结果 与钱的模范并显示出公平的协议。讨论了流化实验的局限性 和转鼓实验,可以减少实验的不确定性,提供可量化的 的结果,并建议适合在NASA的重力减轻飞机上飞行。这 转鼓技术确定粉末区域中心的特征频率 检测雪崩。通过比较获得的特征频率来验证该概念 从分析粘性粉末到分析 易流动的粉末。

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