Abstract
A solution is given to the spatial-temporary distribution of temperature in the volume of the Earth, due to the specified power of the thermal radiation of the hot core. An estimate is made of the maximum possible cooling time of the core.
Highlights
The question considered in this paper is related to the analysis of the distribution of temperature within the Earth’s surface. We believe that it should only be caused by thermal radiation coming from the nucleus, the temperature of which, according to some independent, objective sources [1,2,3], is approximately equal to 5000 ÷ 6000 K
It is quite clear that the point source model does not here; the use of the thermal conductivity equation
Where the right part of this equality, according to decision (16), has a very transparent physical meaning, as it represents the difference between stationary temperatures, namely
Summary
The question considered in this paper is related to the analysis of the distribution of temperature within the Earth’s surface. We believe that it should only be caused by thermal radiation coming from the nucleus, the temperature of which, according to some independent, objective sources [1,2,3], is approximately equal to 5000 ÷ 6000 K. QN (t)δ(r), where QN(t)—is a power of thermal radiation core, is not acceptable. This means that to adequately account for the effect of thermal radiation of the core on the spatial-temporal distribution of temperature throughout the internal volume of the Earth V − VN, where V 4πR3 3.
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