回顾引入“地球物理电动力学”术语的基本原理

V. Aksenov
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引用次数: 0

摘要

背景。本文为引入“地球物理电动力学”这一术语提供了论据。为了证明引入一个新术语“地球物理电动力学”的合理性。证实的方法。研究了麦克斯韦方程组的适用极限。此外,还介绍了一些概念,特别是电动力学的新范式,地球物理电动力学的新方程,新电动力学与麦克斯韦电动力学的区别,环向和极向电磁场的来源,麦克斯韦方程中的环向电流,非功率电磁场,非功率电磁场中的量子效应,地核中的环向场,新范式下的数学成就,关于地球电磁场源的再现,以及用地球物理电动力学结果解释经典电动力学中的效应。收到了对上述理由的回应。引入“地球物理电动力学”这一术语的物理和数学理由,在地球的自然电磁场和标准麦克斯韦电动力学中许多众所周知的经典效应中都得到了证实。一种电动力学与另一种电动力学之间微小但基本的差异,将减少从麦克斯韦方程的角度无法解释的效应的数量,这些效应在地球上的理论和实验中都遇到过。
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Review of rationales for the introduction of the “Geophysical electrodynamics” term
Background. The article provides arguments for the introduction of the “geophysical electrodynamics” term.Aim. To justify the introduction of a new term “geophysical electrodynamics”.Methods of substantiation. The limits of the applicability of Maxwell’s equations are studied. Additionally, some concepts are introduced, in particular, about a new paradigm in electrodynamics, about new equations in geophysical electrodynamics, about the differences between new electrodynamics and Maxwell’s electrodynamics, about the sources of toroidal and poloidal electromagnetic fields, about toroidal currents in Maxwell’s equations, about non-power electromagnetic fields, about the quantum effect in non-power electromagnetic fields, toroidal fields in the core of the Earth, mathematical achievements in the new paradigm, about the reproduction of sources of the electromagnetic field of the Earth, and effects in classical electrodynamics explained by geophysical electrodynamics.Results. Responses to the above justifications were received.Conclusion. Physical and mathematical justifications for the introduction of the term “geophysical electrodynamics” find confirmation both in the natural electromagnetic field of the Earth, and in a number of long-known classical effects in the standard Maxwell’s electrodynamics. Small but fundamental differences of one electrodynamics from another will reduce the number of effects unexplained from the standpoint of Maxwell’s equations, encountered in both theory and experiments on Earth.
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审稿时长
8 weeks
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