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Related Concept Videos

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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Related Experiment Video

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

Magnetic reversals and mass extinctions.

D M Raup1

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

Nature
|March 28, 1985
PubMed
Summary

Earth's magnetic field reversals show a consistent 30 million year cycle. This geological timescale periodicity predicts future pulses of increased magnetic field activity, potentially linked to biological extinction events.

Area of Science:

  • Geophysics
  • Paleomagnetism
  • Earth Science

Background:

  • Analysis of Earth's magnetic field reversal timing has produced conflicting results regarding periodicity.
  • Some studies suggest a 10 million year periodicity, while others find random spacing.
  • Potential links between magnetic field reversals and biological extinction events warrant further investigation.

Purpose of the Study:

  • To analyze the time distribution of Earth's magnetic field reversals over the past 165 million years.
  • To identify any significant periodicities in the magnetic reversal record.
  • To assess the implications of identified periodicities for understanding Earth's dynamic processes and their potential impact.

Main Methods:

  • Time series analysis of paleomagnetic data.

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

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Last Updated: Jun 29, 2026

Magnet Assisted Composite Manufacturing: A Flexible New Technique for Achieving High Consolidation Pressure in Vacuum Bag/Lay-Up Processes
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  • Statistical examination of the Earth's magnetic reversal record spanning 165 million years.
  • Identification and characterization of periodic signals within the reversal data.
  • Main Results:

    • A stationary periodicity of 30 million years was identified in the magnetic reversal record.
    • This 30 million year cycle is superimposed on previously established non-stationarities.
    • The study predicts pulses of increased magnetic reversal activity at specific intervals (10, 40, 70 million years Before Present).

    Conclusions:

    • The Earth's magnetic field reversal process exhibits a significant 30 million year periodicity.
    • This periodicity provides a predictive framework for future reversal activity.
    • The findings contribute to understanding long-term geodynamo behavior and its potential correlation with major Earth events.