The question now is, what should be the atmosphere? When temperatures in excess of nearly a thousand times the temperature of the molten iron Cakobau is computing the surface temperature of the Sun, the majority of the solids, if not all, should come in gaseous state; and although the enormous attractive force of the Sun must greatly to keep that desire to take the form of vapor, is still not be the slightest doubt that if the body of the Sun consists of molten substances, some of them must constantly be evaporation. Incredibly, to dense gases constantly generated in such by the way, was the entire atmosphere of the Sun. If we have the right to do any conclusions based on the hypothesis of the foggy mass, or on analogies we present planets, we must come to the conclusion that external part of the solar atmosphere consists of so-called permanent gases, i.e. of those who are unable to condense in the drip liquid even at low temperature. If we take in consideration the order of things which shall was to exist here on Earth, at a time when the surface of the Earth was in molten state, we see that around molten and to this time the surface of the Sun exist, in all likelihood, a layer vozduhovodnogo dense substance, consisting of sublimed metals and metal compounds, and above this layer other consisting of relatively rare medium, like air. What happens in those two layers? If they both consisted of permanent gases, they would not be able to stay separate from one another; obeying the law, they would constitute when favorable circumstances monotonous mix. But this does not can happens when the lower layer consists of substances in the gaseous only at very high temperatures.
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The question now is, what should be the atmosphere? When
temperatures in excess of nearly a thousand times the temperature of the molten
iron Cakobau is computing the surface temperature of the Sun,
the majority of the solids, if not all, should come in
gaseous state; and although the enormous attractive force of the Sun must
greatly to keep that desire to take the form of vapor, is still not
be the slightest doubt that if the body of the Sun consists of
molten substances, some of them must constantly be
evaporation. Incredibly, to dense gases constantly generated in such
by the way, was the entire atmosphere of the Sun. If we have the right to do
any conclusions based on the hypothesis of the foggy mass, or on analogies
we present planets, we must come to the conclusion that external
part of the solar atmosphere consists of so-called permanent gases, i.e.
of those who are unable to condense in the drip liquid even at low
temperature. If we take in consideration the order of things which shall
was to exist here on Earth, at a time when the surface of the Earth was in
molten state, we see that around molten and to
this time the surface of the Sun exist, in all likelihood, a layer
vozduhovodnogo dense substance, consisting of sublimed metals and
metal compounds, and above this layer other consisting of relatively
rare medium, like air. What happens in those two layers? If
they both consisted of permanent gases, they would not be able to stay
separate from one another; obeying the law, they would constitute
when favorable circumstances monotonous mix. But this does not can
happens when the lower layer consists of substances in the gaseous
only at very high temperatures.
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