相关实验视频
Updated: Jul 9, 2026

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Extraction of the EPP Component from the Surface EMG
Published on: December 16, 2009
地磁冲击的起源 地磁冲击的起源
Jeremy Bloxham1, Stephen Zatman, Mathieu Dumberry
1Department of Earth and Planetary Sciences, Harvard University, Cambridge, Massachusetts 02138, USA. Jeremy_Bloxham@harvard.edu
Nature
|November 8, 2002
概括
地磁冲击是地球磁场的突然变化. 我们的研究解释了这些事件,利用地球核心内的稳定和时间变化的流体流动的组合,与扭曲振荡相一致.
科学领域:
- 地质物理学 地质物理学
- 地球科学 地球科学 地球科学
- 地磁主义 地磁主义
背景情况:
- 地磁冲击是地球磁场长期加速的突然变化.
- 这些事件定期发生,表明磁场的世俗变化的重组.
- 地磁冲击的内部起源和核心表面流体流动力学已知,但其物理原因尚不清楚.
研究的目的:
- 为了阐明地磁冲击的物理起源.
- 为了解释地球磁场的突然变化,世俗加速.
- 为了将地磁冲击与地球核心内的流体动力学联系起来.
主要方法:
- 对地磁性世俗变化数据的分析.
- 在地球核心表面的流体流动的建模.
- 球体波分析以确定现象的内部起源.
主要成果:
- 地磁冲动可以通过核心表面稳定和时间变化的 toroidal 区域流的组合来解释.
- 这种流动是轴对称和赤道对称的.
- 拟议的流动模型与地球核心的扭曲振荡是一致的.
结论:
- 地磁冲击的物理起源与地球核心内的扭曲振荡有关.
- 这些发现支持了核心流量和动力发电机模型的理论预期和观察.
- 这项研究为地磁冲击提供了一个新的动态解释.
相关概念视频
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An individual magnetic pole cannot be isolated. No matter how small, every piece of a magnet contains a north pole and a south...
An individual magnetic pole cannot be isolated. No matter how small, every piece of a magnet contains a north pole and a south...
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The representation of magnetic fields by magnetic field lines is very useful in visualizing the strength and direction of the magnetic field. Each of the magnetic field lines forms a closed loop. The field lines emerge from the north pole (N), loop around to the south pole (S), and continue through the bar magnet back to the north pole.
Magnetic field lines follow several hard-and-fast rules:
Magnetic field lines follow several hard-and-fast rules:
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...
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...
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Consider two parallel straight wires carrying a current of 10 A and 20 A in the same direction and separated by a distance of 20 cm. Calculate the magnetic field at a point "P2", midway between the wires. Also, evaluate the magnetic field when the direction of the current is reversed in the second wire.
Potential Due to a Magnetized Object
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...
The vector...
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...

