Abstract

Principally new model of the magnetic field of the Hot Earth is proposed. Unlike the commonly accepted approach which considers that the Earth’s temperature doesn’t increase because heat released under selfgravitation is removed through radiation our model assumes that early substance of the Earth heated up to 30 000 K was a superheated and overcompressed vapour. Cooling the Earth substance was condensing. The system was expanding adiabatically that governed the character of the Earth enlargement. This scheme origins from the phase transition (PT) of condensation-evaporation under the benefit of condensation. PT provides the heat, geodynamics of expansion and the Earth’s magnetic field (EMF). The high temperature of the substance causes its thermoionization, whereas PT operation relating to mass transfer initiates charges separation and generation of the double electric layer (DEL). A diurnal rotation of DEL induces a weak initial EMF which enhances then at the expense of the Hall dynamo (Hall current) inside PT area. The benefit of evaporation causes the Earth compression and reversal of the EMF polarity. The approach we develop provides an insight into features of the magnetic field of the planets and satellites at the Sun system.

Highlights

  • At the conference “The inner core – 2000” in Moscow the leading Russian magnitilogist Prof

  • In contrast to the commonly used kinematic dynamo as a scheme of the Earth’s magnetic field (EMF) generation, the new model is based on the author's model of hot expanding Earth, using the features of this idea

  • The main advantage of both the hot Earth model and the EMF generation model is that the hot Earth provides an obvious energy source, it is the phase transition (PT) "condensation-evaporation"

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Summary

Introduction

At the conference “The inner core – 2000” in Moscow the leading Russian magnitilogist Prof. Assuming that all mantle matter condensed and crystallized, and the substance of the outer core condensed [3] we estimate the value of energy EU released by the Earth during its evolution (t = 4.5 billion years) by means of a phase transition.

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