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The second most important constituent of the biosphere is k0j4P^d
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liquid water. This can only exist in a very narrow range of temperatures, -x6_HibbD
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since water freezes at 0°C and boils at 100°C. This is [7.Num_L
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only a tiny range compared with the low temperatures of some Ynf "g#(
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other planets and the hot interior of the earth, let the temperature __1__ X_X7fRC0
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of the sun. by controlpanel JzywSQ
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As we know, life would only be possible on the face of a __2__ FYik}wH]
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planet had temperatures somewhere within this range. __3__ W!ug^2"
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The earth’s supply of water probably remains quite fairly constant __4__ (BH<\&yHE
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in quantity. A certain number of hydrogen atoms, which tlO=>
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are one of the main constituents of water, are lost by escaping [Y
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from the atmosphere to out space, but they are probably just __5__ kygj" @EX
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about to be replaced by new water rising away from the depths of the __6__ F6CuY$0m=
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earth during volcanic action. The total quantity of water is not fMf;
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known, and it is about enough to cover the surface of the globe __7__ ~g[D!HV|yu
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to a depth of about two and three-quarter kms. Most of it—97% JK{2hr_a
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is in the form of the salt waters of the oceans. The rest is OFv-bb*YZ
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fresh, but three quarter of this is in the form of ice at the Poles __8__ :k_)Bh?+
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and on mountains, and cannot be used by living systems when __9__ 3:sc%IDP
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melted. Of the remaining fraction, which is somewhat fewer __10__ ZrP
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than 1%of the whole, there is 10-20 times as much stored as underground U\{I09@E 0
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water as is actually on the surface. There is also a minor,