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Induced Electric Dipoles01:28

Induced Electric Dipoles

4.0K
A permanent electric dipole orients itself along an external electric field. This rotation can be quantified by defining the potential energy because the external torque does work in rotating it. Then, the potential energy is minimum at the parallel configuration and maximum at the antiparallel configuration. While the former is a stable equilibrium, the latter is an unstable equilibrium.
Since the absolute value of potential energy holds no physical meaning, its zero value can be chosen as per...
4.0K
Magnetic Fields01:27

Magnetic Fields

6.0K
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...
6.0K
Potential Due to a Polarized Object01:29

Potential Due to a Polarized Object

946
A neutral atom consists of a positively charged nucleus surrounded by a negatively charged electron cloud. When placed in an external electric field, the external electric force pulls the electrons and nucleus apart, opposite to the intrinsic attraction between the nucleus and the electrons. The opposing forces balance each other with a slight shift between the center of masses of the nucleus and the electron cloud, resulting in a polarized atom. On the other hand, a few molecules, like water,...
946
Potential Due to a Magnetized Object01:24

Potential Due to a Magnetized Object

924
Magnetic dipoles in magnetic materials are aligned when placed under an external magnetic field. For paramagnets and ferromagnets, dipole alignment occurs in the direction of the magnetic field. However, the dipoles align opposite to the field in the case of diamagnets. This state of magnetic polarization due to the external field is called magnetization. Magnetization is defined as the dipole moment per unit volume. It plays a similar role to polarization in electrostatics.
The vector...
924
Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

1.9K
An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
1.9K
Magnetic Declination01:19

Magnetic Declination

789
Magnetic declination is the angle between true north, which aligns with the Earth's rotational axis, and magnetic north, which follows the direction of the Earth's magnetic field. This discrepancy exists because the magnetic poles do not coincide with the geographic poles. The value of magnetic declination depends on the observer's location on Earth and is subject to changes over time due to the dynamic nature of the Earth's magnetic field.The declination is called eastern when magnetic north...
789

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Related Experiment Video

Updated: May 2, 2026

Dissolution Dynamic Nuclear Polarization Instrumentation for Real-time Enzymatic Reaction Rate Measurements by NMR
10:54

Dissolution Dynamic Nuclear Polarization Instrumentation for Real-time Enzymatic Reaction Rate Measurements by NMR

Published on: February 23, 2016

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Polarity transition records and the geomagnetic dynamo.

K A Hoffman

    Science (New York, N.Y.)
    |June 17, 1977
    PubMed
    Summary

    The Parker-Levy model accurately predicts virtual geomagnetic pole paths during reversals, aligning with observational data. Some discrepancies suggest complex core convection not fully captured by the model.

    Area of Science:

    • Geophysics
    • Earth Science
    • Paleomagnetism

    Background:

    • Geomagnetic field reversals are complex phenomena.
    • The Parker-Levy model offers a theoretical framework for understanding these reversals.
    • Detailed records of transitional virtual geomagnetic pole (VGP) paths are crucial for validating models.

    Purpose of the Study:

    • To compare the Parker-Levy model's predictions of VGP transitional paths with available observational data.
    • To assess the model's accuracy in predicting VGP paths and transitional field intensity.
    • To identify potential reasons for discrepancies between model predictions and real-world data.

    Main Methods:

    • The study involves comparing theoretical predictions from the Parker-Levy model with empirical data from detailed transitional VGP path records.

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  • Analysis focuses on whether VGP paths pass through the observation site or its antipode.
  • Transitional field intensity predictions are also compared with reported records.
  • Main Results:

    • The Parker-Levy model's predictions for meridional VGP transitional paths show some agreement with the most detailed available records.
    • The model's predictions align with observations regarding whether paths pass through the site or its antipode, depending on location and transition sense.
    • Predicted variations in transitional field intensity are also compatible with several reported transition records.

    Conclusions:

    • The Parker-Levy approach provides a valuable framework for understanding geomagnetic field reversals.
    • Discrepancies between the model and data may arise from unconsidered complexities in core convection.
    • Further research into core dynamics is needed to refine geomagnetic reversal models.