The second most important constituent of the biosphere is liquid water. This can only exist in a very narrow range of temperatures,since water freezes at 0°C and boils at 100°C. This is only a tiny range compared with the low temperatures of some other planets and the hot interior of the earth, let the temperature(1)of the sun.
As we know, life would only be possible on the face of a(2)planet had temperatures somewhere within this range. (3)The earth’s supply of water probably remains quite fairly constant(4)in quantity. A certain number of hydrogen atoms, which are one of the main constituents of water, are lost by escaping from the atmosphere to out space, but they are probably just (5)about to be replaced by new water rising away from the depths of the (6)earth during volcanic action.
The total quantity of water is not known, and it is about enough to cover the surface of the globe (7)to a depth of about two and three-quarter kms. Most of it&mdash
The second most important constituent of the biosphere is liquid water. This can only exist in a very narrow range of temperatures,since water freezes at 0°C and boils at 100°C. This is only a tiny range compared with the low temperatures of some other planets and the hot interior of the earth, let the temperature(1)of the sun.
As we know, life would only be possible on the face of a(2)planet had temperatures somewhere within this range. (3)The earth’s supply of water probably remains quite fairly constant(4)in quantity. A certain number of hydrogen atoms, which are one of the main constituents of water, are lost by escaping from the atmosphere to out space, but they are probably just (5)about to be replaced by new water rising away from the depths of the (6)earth during volcanic action.
The total quantity of water is not known, and it is about enough to cover the surface of the globe (7)to a depth of about two and three-quarter kms. Most of it&mdash
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