国外均匀电磁场中球形地球电磁的较先进的理论模型

S. Bjelić, N. Marković
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引用次数: 0

摘要

前言/目的:本文描述了一种基于双分量假设的更先进的地球电磁场理论模型。一种已定义的数学模型,显示磁化强度为M的导电球在外来磁场中的旋转,以及由于地球绕地轴旋转而可能产生的磁场分量根据所建立的模型,以地球行星的参考值为参照,计算了太阳系中其他行星的成分值,并将计算结果制成表格。方法:采用形式化的物理方法和数学分析方法相结合的方法来确定本文标题所强调的问题的解决方案,以建立一个新的、更先进的数学模型。为此,使用了类比的方法,涉及到应用类似的结构形式和系统来研究电磁过程和行星旋转。采用类比法有两个相互关联的原因。第一个是,表征任何自然系统功能的所有值都可能发生变化,第二个是,应用的解决方案并不能确定每个特定情况下结构功能的条件。结果:表2中所列的原始解析公式和数值形式的解,参考了行星特别是地球自转的影响,将用于研究太阳发出的电磁场对行星的影响,特别是对地球的保护作用。表2给出的结果尤其重要。结束语:本文以目前科学发展水平可以理解的方式讨论了地球电磁场的出现和影响。科学上的科学发现以及地球和天体物理学的测量结果表明,太阳是通过行星际空间延伸的电磁场的一个可能来源,地球磁场的组成部分只是对该来源影响的一种反应。在系统理论中,地球上的自然现象和过程可以用一个包含地球状态参数变化的模型来定义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A more advanced theoretical model of the sphere earth's EM in a foreign homogeneous EM field
Introduction/purpose: The paper describes a more advanced theoretical model of the Earth's EM field based on two-component hypotheses. A defined mathematical model that shows the rotation of the magnetically conducting sphere of Tthe magnetization M in a foreign magnetic field and the components of the magnetic field that may arise due to the rotation of the Earth around its axis. According to the established model, in relation to the reference values of the planet Earth, the values of the components of the other planets in the solar system were calculated and the results were tabulated. Methods: The solution to the problem highlighted in the title of the paper was determined using the combined, for that purpose, formalized methods of physics and mathematical analysis, in order to develop a new, more advanced mathematical model. For this purpose, the method of analogy was used, related to the application of similar structural forms and systems for researching electromagnetic processes and planetary rotation. The method of analogy was applied for two interrelated reasons. The first one is that all values that characterize the function of any natural system are subject to change, and the second one is that the applied solutions do not determine the conditions of the structure's function in each specific case. Results: The solutions in the form of original analytical formulas and numerical values arranged in Table 2, referring to the influence of the rotation of the planets and especially the Earth, will be applied to research the effects of the EM field emitted by the Sun towards the planets, especially the role that the process plays in protecting the planet Earth. The results given in Table 2 are particularly important. Conclusion: The paper discusses the appearance and effect of the Earth's EM field in a way that is understandable at the current level of scientific development. Scientific findings in science and measurements in geoand astrophysics indicate the Sun as a possible source of the EM field that extends through interplanetary space and the component of the Earth's magnetic field is only a response to the influence of that source. Natural phenomena and processes on the Earth can be defined in system theory by a model that contains changes in the parameters of the state of the planet.
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