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相关概念视频

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...
Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

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...
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 Fields01:28

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 Susceptibility and Permeability01:31

Magnetic Susceptibility and Permeability

In linear magnetic materials, like paramagnets and diamagnets, magnetization is proportional to the magnetic field intensity. The constant of proportionality, a dimensionless number, is called magnetic susceptibility. The value of the susceptibility depends on the type of material.
When diamagnetic materials are placed under an external magnetic field, the moments opposite to the field are induced. Hence, the susceptibility for diamagnets has a minimal negative value of 10-5–10-6. Since...
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...

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相关实验视频

Updated: Jul 12, 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: November 30, 2015

地磁逆转在棕色的正常极性时代.

J D Smith, J H Foster

    Science (New York, N.Y.)
    |February 7, 1969
    PubMed
    概括

    研究人员在深海沉积物核心中发现了一段短暂的反向磁极性的时期,称为布莱克事件. 这一重要的古磁性发现为地球的地质历史提供了新的标记.

    科学领域:

    • 古磁力学是一种古磁学.
    • 海洋地质 海洋地质学
    • 地质时间学 (Geochronology)

    背景情况:

    • 地球的磁场在历史上多次逆转极性.
    • 深海沉积物核心提供了关于过去环境和地磁条件的宝贵档案.

    研究的目的:

    • 为了研究深海沉积物核心的磁性层级.
    • 为了识别和描述逆极性的短时间间隔.

    主要方法:

    • 在七个深海沉积物核心中分析磁性层级学.
    • 磁逆转区与古生物学界限的相关性.

    主要成果:

    • 在上布鲁尼斯时代发现了一个短的反向极性间隔.
    • 把这个间隔命名为"布莱克事件".
    • 估计布莱克事件的边界在108,000至114,000年前 (+/- 10%).

    结论:

    • 布莱克事件代表了一个明显的地磁探险或逆转.
    • 这一事件在海洋沉积物中充当了一种有价值的年代层学标记.
    • 这些发现增强了我们对地球古磁场行为的理解.

    相关实验视频

    Last Updated: Jul 12, 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: November 30, 2015