在地球,原子内粒子在地球磁场的作用下呈流状分布在两极。
As on Earth, the particles are channelled to the poles by the planet's magnetic field.
在地球上,从坚固的内磁芯的热量通过与炽热的外磁芯核的对流而形成流体动力,引起了电荷,进而由电荷产生了全球的电磁场。
On Earth, heat from the solid inner core drives complex fluid dynamics through convection in the planet's molten outer core, causing an electrical charge which generates a global magnetic field.
地球磁场的演化历史对研究地核与地幔边界的动力学和地核内的磁流体力学过程提供了重要的信息。
The history of the Earth's magnetic field provides basic information on the dynamics of core mantle boundary and core convection.
地球磁场的演化历史对研究地核与地幔边界的动力学和地核内的磁流体力学过程提供了重要的信息。
The history of the Earth's magnetic field provides basic information on the dynamics of core mantle boundary and core convection.
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