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An atomic orbital represents the three-dimensional regions in an atom where an electron has the highest probability to reside. The radial distribution function indicates the total probability of finding an electron within the thin shell at a distance r from the nucleus. The atomic orbitals have distinct shapes which are determined by l, the angular momentum quantum number. The orbitals are often drawn with a boundary surface, enclosing densest regions of the cloud.
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Atoms — and the protons, neutrons, and electrons that compose them — are extremely small. For example, a carbon atom weighs less than 2 × 10−23 g. When describing the properties of tiny objects such as atoms, we use appropriately small units of measure, such as the atomic mass unit (amu). The amu was originally defined based on hydrogen, the lightest element, then later in terms of oxygen. Since 1961, it has been defined with regard to the most abundant isotope of carbon, atoms of which...
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In an atom, the negatively charged electrons are attracted to the positively charged nucleus. In a multielectron atom, electron-electron repulsions are also observed. The attractive and repulsive forces are dependent on the distance between the particles, as well as the sign and magnitude of the charges on the individual particles. When the charges on the particles are opposite, they attract each other. If both particles have the same charge, they repel each other.
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The earliest recorded discussion of the basic structure of matter comes from ancient Greek philosophers. Leucippus and Democritus argued that all matter was composed of small, finite particles that they called atomos, meaning “indivisible.” Later, Aristotle and others came to the conclusion that matter consisted of various combinations of the four “elements” — fire, earth, air, and water — and could be infinitely divided. Interestingly, these philosophers...
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原子钟的性能使得在厘米以下的地质测量

W F McGrew1,2, X Zhang1,3, R J Fasano1,2

  • 1National Institute of Standards and Technology, Boulder, CO, USA.

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概括
此摘要是机器生成的。

新的光学原子钟实现了前所未有的精度,超越了目前在测量时间上的重力效应的能力. 这一突破使得先进的地理测量和基础物理研究成为可能.

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科学领域:

  • 原子物理
  • 测量学
  • 地质学

背景情况:

  • 原子钟通过计算频率标准的振荡来测量时间.
  • 光学原子钟提供了卓越的精度,达到低于10−17的分数性能.
  • 相对论规定时间的流逝是相对的,受速度,加速度和重力的影响.

研究的目的:

  • 为了证明光学时钟测量超过当前的能力, 解释地球的引力时空扭曲.
  • 为光学时钟建立系统不确定性,测量不稳定性和可重复性的新基准.

主要方法:

  • 使用两个独立的光学晶格时钟.
  • 进行局部时钟测量以评估性能基准.
  • 进行十次盲目的频率比较以进行可重复性分析.

主要成果:

  • 达到1.4 × 10−18的系统不确定性 (用时钟频率单位).
  • 报告的测量不稳定性为3.2 × 10−19.
  • 经证明的可重复性与频率差异为 [-7 ± 5] ± 8] × 10−19.

结论:

  • 展示的光学时钟在测量时空的引力扭曲方面超越了当前的能力.
  • 它们对地势的敏感性使得先进的地质测量能够达到厘米级的分辨率.
  • 这些时钟可以用于探索地质现象,测试广义相对论,寻找暗物质.