基于波动增长的磁碟发电机模型解释地磁场反转。

S. Kondo
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引用次数: 1

摘要

基于涨落增长的观点,对地磁场倒转进行了分析和讨论,重点讨论了三盘发电机模型,主要讨论了互感对动态行为的影响。如果互感很大,这意味着相邻磁盘及其相关电路之间的相互作用很强,那么发现电流的非常轻微的波动在短暂的孵育时间后会大大增强。相反,当互感较小时,经过较长孵育时间后,波动增长非常缓慢。因此,相互作用的程度与孵育时间的长短有关:相互作用越强,孵育时间越短。磁碟发电机与地磁场倒转模式的相似性表明,在过去25 Ma期间,轻微的波动大大增强,而在白垩纪超时期间,波动增长非常缓慢,这表明互感依赖于时间。因此,包含互感时间依赖性的磁盘发电机计算可以定性地解释地磁场反转模式。从数学的角度出发,发现调频对时变互感的数值解优于对时变互感的数值解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Interpretation of Geomagnetic Field Reversal on the Basis of Fluctuation Growth by Using Disk Dynamo Model.
Based on the viewpoint of fluctuation growth, we analyze and discuss the geomagnetic field reversal, focusing on a three-disk dynamo model, mainly on the effect of mutual inductance on dynamic behaviors. If mutual inductance is large, which means strong interaction between neighboring disks and their associated circuits, then a very slight fluctuation of electric current is found to be greatly enhanced after a short incubation time. On the contrary, after a long incubation time, fluctuation growth is very slow when mutual inductance is small. Therefore the degree of interaction is related to the length of incubation time: the stronger the interaction, the shorter incubation time. The analogy between the disk dynamos and the geomagnetic field reversal patterns implies slight fluctuations are greatly enhanced during the period for the past 25 Ma, whereas fluctuation growth is very slow during the period of the Cretaceous Superchron, implying that mutual inductance is dependent on time. Hence, disk dynamo calculations including time dependence of mutual inductance are found to explain geomagnetic field reversal pattern qualitatively. From the mathematical viewpoint, numerical solutions for time dependent mutual inductance is found to be obtained by frequency modulation (FM) over those for time independent mutual inductance.
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