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Preliminary Planck constant measurements via UME oscillating magnet Kibble balance

机译:通过UME振荡磁体岩布平衡初步普通普通测量

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The UME Kibble balance project was initiated in the second half of 2014. During this period we have studied the theoretical aspects of Kibble balances, in which an oscillating magnet generates AC Faraday's voltage in a stationary coil, and constructed a trial version to implement this idea. The remarkable feature of this approach is that it can establish the link between the Planck constant and a macroscopic mass by one single experiment in the most natural way. Weak dependences on variations of environmental and experimental conditions, small size, and other useful features offered by this novel approach reduce the complexity of the experimental set-up. This paper describes the principles of the oscillating magnet Kibble balance and gives details of the preliminary Planck constant measurements. The value of the Planck constant determined with our apparatus is h/h(90) = 1.000 004, with a relative standard uncertainty of 6 ppm.
机译:Ume Kibble Balance项目在2014年下半年开始。在此期间,我们研究了Kibble余额的理论方面,其中振荡磁铁在静止线圈中产生了AC Faraday的电压,并构建了实现这个想法的试用版 。 这种方法的显着特征是,在最自然的方式中,它可以通过一项实验在普朗克常数和宏观质量之间建立链路。 对环境和实验条件的变化,小尺寸和其他新颖方法提供的其他有用特征的弱依赖性降低了实验设置的复杂性。 本文介绍了振荡磁体岩石平衡的原理,并提供了初步普通常量测量的细节。 用我们的装置确定的普朗克常数的值是H / H(90)= 1.000 004,具有6 ppm的相对标准不确定性。

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