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Magnetism01:30

Magnetism

Magnets are commonly found in everyday objects, such as toys, hangers, elevators, doorbells, and computer devices. Experimentation on these magnets shows that all magnets have two poles: one is labeled north (N) and the other south (S). Magnetic poles repel if they are alike and attract if unlike. Moreover, both poles of a magnet attract unmagnetized pieces of iron.
An individual magnetic pole cannot be isolated. No matter how small, every piece of a magnet contains a north pole and a south...
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...
Induced Electric Fields: Applications01:27

Induced Electric Fields: Applications

An important distinction exists between the electric field induced by a changing magnetic field and the electrostatic field produced by a fixed charge distribution. Specifically, the induced electric field is nonconservative because it does not work in moving a charge over a closed path. In contrast, the electrostatic field is conservative and does no net work over a closed path. Hence, electric potential can be associated with the electrostatic field but not the induced field. The following...
Magnetic Field due to Moving Charges01:23

Magnetic Field due to Moving Charges

A stationary charge creates and interacts with the electric field, while a moving charge creates a magnetic field.
Consider a point charge moving with a constant velocity. Like the electric field, the magnetic field at any point is directly proportional to the magnitude of the charge and inversely proportional to the square of the distance between the source point and the field point. However, unlike the electric field, the magnetic field is always perpendicular to the plane containing the line...
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...
Magnetic Declination01:19

Magnetic Declination

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...

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Updated: Jun 24, 2026

Geomagnetic Field (Gmf) and Plant Evolution: Investigating the Effects of Gmf Reversal on Arabidopsis thaliana Development and Gene Expression
11:04

Geomagnetic Field (Gmf) and Plant Evolution: Investigating the Effects of Gmf Reversal on Arabidopsis thaliana Development and Gene Expression

Published on: December 1, 2015

太平洋地磁気圏の世俗的な変動

R R Doell, A Cox

    Science (New York, N.Y.)
    |January 22, 1971
    PubMed
    まとめ
    この要約は機械生成です。

    地磁気的世俗的な変動記録は,過去070万年にわたって太平洋中部でより弱い非二極場を明らかにしています. これは,下層マントルの不均一性が,この領域の下の地球の磁場生成に影響することを示唆しています.

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    関連する実験動画

    Last Updated: Jun 24, 2026

    Geomagnetic Field (Gmf) and Plant Evolution: Investigating the Effects of Gmf Reversal on Arabidopsis thaliana Development and Gene Expression
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    Enhancement of the Initial Growth Rate of Agricultural Plants by Using Static Magnetic Fields
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    科学分野:

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

    背景:

    • 地球の磁場は,その強度と方向の長期的な変化である,世俗的な変動を示しています.
    • 地磁場の非二極成分は,地球の核内の複雑な流体運動から発生すると考えられている.
    • 以前の研究では,地磁場における地域的な変動が示唆されているが,その根本的な原因については議論が続いている.

    研究 の 目的:

    • 多様な古磁気および直接観測データを用いて,長期間の地磁気世俗的変動を調査する.
    • 太平洋中部地域が地質的な時間スケールにおける地磁場行動においてユニークな特徴を示すかどうかを判断する.
    • 下層マントルの構造と非二極地磁場の抑制の間の潜在的なリンクを特定する.

    主な方法:

    • 地磁気世俗的変動の直接観測所による測定の分析.
    • ハワイの溶岩流の古磁気分析は,正確な年代 (0-200年) を示しています.
    • ハワイの溶岩流の古磁気分析は,年代がより正確ではない (200-10,000年).
    • 地磁気角分散を評価するために,過去070万年のラバ流からの世界的な古磁気データの調査.

    主要な成果:

    • すべての分析された磁気記録は,一貫して,他の地域と比較して太平洋中部における地球の磁場の非二極成分が減少していることを示しています.
    • この観測パターンは,過去070万年にわたって持続し,現代のフィールドの特徴を反映しています.
    • データは,地球のコアと下層マントルの間のカップリングを示し,中央太平洋の下の非二極フィールドの生成を抑制しています.

    結論:

    • 太平洋中部地域では,下部マントルの不均一性による非二極地磁場が抑制されている可能性が高い.
    • 観測されたパターンは,地磁場を生成するプロセスに地球深層の構造が有意な影響を与えていることを示唆しています.
    • 主な原因として,コアマントルの境界地形と下部マントルの性質の横向的な変動を区別するためにさらなる研究が必要です.