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Book Boris V. Vasiliev Astrophysics

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Astrophysics

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Chapter 12<br />

The Theory of Earth<br />

12.1 The introduction<br />

Seismic measurements show that as the depth grows, the density of the Earth’s matter<br />

increases at first more or less monotonically. However, on the core-mantle interface<br />

it rises abruptly. There exist a series of Earth models [23],[24] for the description of<br />

the density growth, for the explanation of the reason of the separation of the Earth<br />

matter into the core and the mantle and the determination of the density jump on their<br />

interface. Quite separately there exist models for the explanation of the origin of the<br />

terrestrial magnetism. Among these models, there is one based on the hydrodynamic<br />

hypothesis. It was developed in the 1940’s-1950’s. At present it is generally adopted.<br />

All these models try to decide the basic problem - to obtain the answer: why the main<br />

magnetic field of the Earth near the poles is of the order of 1 Oe? Such statement of the<br />

basic problem of terrestrial magnetism models nowadays is unacceptable. Space flights,<br />

started in 1960’s, and the further development of astronomy have allowed scientists<br />

to obtain data on magnetic fields of all planets of Solar system, as well as some their<br />

satellites and a number of stars. As a result, a remarkable and earlier unknown fact has<br />

been discovered. It appears that the magnetic moments of all space bodies (those which<br />

have been measured) are proportional to their angular momenta. The proportionality<br />

coefficient is approximately equal to G 1/2 /c, where G is the gravitational constant, c<br />

is the velocity of light (fig.7.1).<br />

Amazing is that this dependence remains linear within 20 orders of magnitude!<br />

This fact makes it necessary to reformulate the main task of the model of terrestrial<br />

magnetism. It should explain, first, why the magnetic moment of the Earth, as well<br />

as of other space bodies, is proportional to its angular momentum and, second, why<br />

the proportionality coefficient is close to the above given ratio of world constants. The<br />

aim of this paper is to show that it is possible to construct the theory of the Earth<br />

using the full energy minimization method. This theory allows us to apply a new<br />

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