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関連する概念動画

Atomic Nuclei: Nuclear Relaxation Processes01:23

Atomic Nuclei: Nuclear Relaxation Processes

In the absence of an external magnetic field, nuclear spin states are degenerate and randomly oriented. When a magnetic field is applied, the spins begin to precess and orient themselves along (lower energy) or against (higher energy) the direction of the field. At equilibrium, a slight excess population of spins exists in the lower energy state. Because the direction of the magnetic field is fixed as the z-axis,  the precessing magnetic moments are randomly oriented around the z-axis. This...
Magnetic Fields01:27

Magnetic Fields

A moving charge or a current creates a magnetic field in the surrounding space, in addition to its electric field. The magnetic field exerts a force on any other moving charge or current that is present in the field. Like an electric field, the magnetic field is also a vector field. At any position, the direction of the magnetic field is defined as the direction in which the north pole of a compass needle points.
A magnetic field is defined by the force that a charged particle experiences...
Magnetic Flux01:18

Magnetic Flux

The magnetic flux measures the number of magnetic field lines passing through a given surface area. The SI unit for magnetic flux is the weber (Wb). Magnetic flux is a scalar quantity. It depends on three factors: the strength of the magnetic field B, the area through which the field lines pass, and the relative orientation of the field with the surface area.
Suppose a surface is divided into elements of area dA. For each element, the component of the magnetic field that is normal to the...
Ferromagnetism01:31

Ferromagnetism

Materials like iron, nickel, and cobalt consist of magnetic domains, within which the magnetic dipoles are arranged parallel to each other. The magnetic dipoles are rigidly aligned in the same direction within a domain by quantum mechanical coupling among the atoms. This coupling is so strong that even thermal agitation at room temperature cannot break it. The result is that each domain has a net dipole moment. However, some materials have weaker coupling, and are ferromagnetic at lower...
Magnetic Force01:18

Magnetic Force

In addition to the electric forces between electric charges, moving electric charges exert magnetic forces on each other. A magnetic field is created by a moving charge or a group of moving charges known as the electric current. A magnetic force is experienced by a second current or moving charge in response to this magnetic field. Fundamentally, interactions between moving electrons in the atoms of two bodies produce magnetic forces between them.
The magnetic force acting on a moving charge...
Magnetic Damping01:17

Magnetic Damping

Eddy currents can produce significant drag on motion, called magnetic damping. For instance, when a metallic pendulum bob swings between the poles of a strong magnet, significant drag acts on the bob as it enters and leaves the field, quickly damping the motion.
If, however, the bob is a slotted metal plate, the magnet produces a much smaller effect. When a slotted metal plate enters the field, an emf is induced by the change in flux; however, it is less effective because the slots limit the...

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関連する実験動画

Updated: Jun 29, 2026

Magnet Assisted Composite Manufacturing: A Flexible New Technique for Achieving High Consolidation Pressure in Vacuum Bag/Lay-Up Processes
09:41

Magnet Assisted Composite Manufacturing: A Flexible New Technique for Achieving High Consolidation Pressure in Vacuum Bag/Lay-Up Processes

Published on: May 17, 2018

磁気逆転と大量絶滅が起こる

D M Raup1

  • 1Department of the Geophysical Sciences, University of Chicago, Illinois 60637, USA.

Nature
|March 28, 1985
PubMed
まとめ

地球の磁場逆転は,3000万年の周期を一貫して示しています. この地質学的時間スケールの周期性により,将来の磁場活動の増加のパルスが予測され,生物学的絶滅イベントと潜在的に関連しています.

科学分野:

  • 地質物理学 地質物理学とは地質物理学です.
  • パレオマグネティズム (古磁気学) とは
  • 地球科学 地球科学 地球科学

背景:

  • 地球の磁場逆転のタイミングの分析は,周期性に関して矛盾する結果を生み出しました.
  • 一部の研究では1000万年の周期性を示唆しているが,他の研究ではランダムな間隔が認められている.
  • 磁場逆転と生物学的絶滅の出来事の間の潜在的な関連は,さらなる調査を正当化します.

研究 の 目的:

  • 過去1.65億年にわたる地球の磁場逆転の時間分布を分析するために.
  • 磁気逆転記録における有意な周期性を特定するために.
  • 地球のダイナミックなプロセスとその潜在的な影響を理解するために,特定された周期性の影響を評価する.

主な方法:

  • 古代磁気データのタイムシリーズ分析.
  • 地球の磁気逆転記録の統計的調査は,165百万年をカバーしています.
  • 逆転データ内の周期信号の識別と特徴付け.

主要な成果:

  • 磁気逆転記録では,3000万年の静止周期が確認されました.
  • この3000万年周期は,以前に確立された非静止値と重なり合っている.

さらに関連する動画

A 100 KW Class Applied-field Magnetoplasmadynamic Thruster
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A 100 KW Class Applied-field Magnetoplasmadynamic Thruster

Published on: December 22, 2018

A Magnetic Separation-Assisted High-Speed Homogenization Method for Large-Scale Production of Endosome-Derived Vesicles
05:36

A Magnetic Separation-Assisted High-Speed Homogenization Method for Large-Scale Production of Endosome-Derived Vesicles

Published on: January 26, 2024

関連する実験動画

Last Updated: Jun 29, 2026

Magnet Assisted Composite Manufacturing: A Flexible New Technique for Achieving High Consolidation Pressure in Vacuum Bag/Lay-Up Processes
09:41

Magnet Assisted Composite Manufacturing: A Flexible New Technique for Achieving High Consolidation Pressure in Vacuum Bag/Lay-Up Processes

Published on: May 17, 2018

A 100 KW Class Applied-field Magnetoplasmadynamic Thruster
11:47

A 100 KW Class Applied-field Magnetoplasmadynamic Thruster

Published on: December 22, 2018

A Magnetic Separation-Assisted High-Speed Homogenization Method for Large-Scale Production of Endosome-Derived Vesicles
05:36

A Magnetic Separation-Assisted High-Speed Homogenization Method for Large-Scale Production of Endosome-Derived Vesicles

Published on: January 26, 2024

  • この研究は,特定の間隔で (10,40,7000万年前) 磁気逆転活動の増幅のパルスを予測しています.
  • 結論:

    • 地球の磁場逆転プロセスは,3,000万年の周期性を有する.
    • この周期性は,将来の逆転活動の予測の枠組みを提供します.
    • この発見は,長期のジオダイナモの行動とその地球上の主要な出来事との潜在的な相関を理解するのに寄与しています.