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Atomic Nuclei: Nuclear Magnetic Moment00:59

Atomic Nuclei: Nuclear Magnetic Moment

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All atomic nuclei are positively charged. When they have a nonzero spin, they behave like rotating charges. As a consequence of their charge and spin, these nuclei generate a magnetic field (B). This, in turn, gives rise to a magnetic moment (μ), which is randomly oriented in the absence of an external magnetic field. When an external magnetic field (B0) is applied, the magnetic moment vectors can align with the field or against it in 2 + 1 orientations. A hydrogen nucleus, which is just a...
3.6K
Atomic Nuclei: Larmor Precession Frequency01:11

Atomic Nuclei: Larmor Precession Frequency

3.8K
The earth's gravitational field produces a 'twisting force' perpendicular to the angular momentum of a spinning mass (such as a spinning top) that causes the mass to 'wobble' around the gravitational field axis in a phenomenon called precession. Similarly, the magnetic moment (μ) of a spinning nucleus precesses due to an external magnetic field directed along the z-axis. The precession of the magnetic moment vector about the magnetic field is called Larmor precession,...
3.8K
Electric Dipoles and Dipole Moment01:30

Electric Dipoles and Dipole Moment

7.2K
Consider two charges of equal magnitude but opposite signs. If they cannot be separated by an external electric field, the system is called a permanent dipole. For example, the water molecule is a dipole, making it a good solvent.
Theoretically, studying electric dipoles leads to understanding why the resultant electric forces around us are weak. Since electric forces are strong, remnant net charges are rare. Hence, the interaction between dipoles helps us understand electrical interactions in...
7.2K
Magnetic Moment of an Electron01:23

Magnetic Moment of an Electron

3.4K
Electrons revolving around a nucleus are analogous to a circular current carrying loop. This current produces a magnetic dipole moment proportional to the electron's orbital angular momentum. Since the orbital angular momentum is quantized in terms of the reduced Planck's constant, the dipole moment is quantized in the Bohr Magneton. The value of the Bohr magneton is 9.27 x 10-24 Am2. Electrons also have an intrinsic spin angular momentum, and the associated spin magnetic moment is...
3.4K
Diamagnetism01:26

Diamagnetism

3.5K
Materials consisting of paired electrons have zero net magnetic moments. However, when these materials are placed under an external magnetic field, the moments opposite to the field are induced. Such materials are called diamagnets. Diamagnetism is the response of the diamagnets when placed in an external magnetic field.
Diamagnetism was discovered by Anton Brugmans in 1778 when he observed that bismuth gets repelled by magnetic fields, thus theorizing that diamagnets get repelled by magnets....
3.5K
Divergence and Curl of Magnetic Field01:26

Divergence and Curl of Magnetic Field

4.2K
The magnetic field due to a volume current distribution given by the Biot–Savart Law can be expressed as follows:
4.2K

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Updated: Apr 11, 2026

Magnetic Tweezers for the Measurement of Twist and Torque
11:41

Magnetic Tweezers for the Measurement of Twist and Torque

Published on: May 19, 2014

24.1K

在过去的200万年里,地磁双极强度和逆转率.

Jean-Pierre Valet1, Laure Meynadier, Yohan Guyodo

  • 1Géomagnétisme et Paléomagnétisme (UMR CNRS 7577), Institut de Physique du Globe de Paris, 4 Place Jussieu, 75252 Paris Cedex 05, France. valet@ipgp.jussieu.fr

Nature
|June 10, 2005
PubMed
概括

在200万年间地磁双极时刻的演变显示,在非反转时期,磁场更强. 这项研究为地磁场过程和地磁场行为提供了新的见解.

科学领域:

  • 地质物理学 地质物理学
  • 古磁论是古磁论的一种学说.
  • 地球科学 地球科学 地球科学

背景情况:

  • 地磁二极子时刻的演变对于理解地磁多摩过程至关重要.
  • 以前的重建仅限于过去的80万年,不包括地磁逆转.

研究的目的:

  • 为了重建地磁双极时刻在过去200万年的演变.
  • 为了研究双极时刻强度和地磁反转之间的关系.

主要方法:

  • 从全球沉积物核心堆叠相对古老强度的独立记录.
  • 校准复合曲线与来自火山岩的绝对二极极时刻.

主要成果:

  • 在过去200万年的地磁双极时刻的复合曲线被生成.
  • 在没有逆转的时期,时间平均场较强.
  • 轴性双极在逆转之前衰减60-80 kyr,然后在相反的方向上迅速重建.

结论:

  • 较强的平均二极子时刻与较少的地磁不稳定性相关,如游览和反转.
  • 地磁场的行为,包括反转,与平均磁场强度有关.
  • 这项研究扩展了我们对地力学动力学过程的理解,使我们更进一步地追溯到过去.

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