The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are relatedTyndall, John
Science
The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are related
Tyndall, John
Alps -- Description and travel; Glaciers -- Alps
But what is true for an atom is also true for a planet or a sun.
Supposing our earth to be brought to rest in her orbit by a sudden
shock, we are able to state the exact amount of heat which would be
thereby generated. The consequence of the earth's being thus brought to
rest would be that it would fall into the sun, and the amount of heat
which would be generated by this second collision is also calculable.
Helmholtz has calculated that in the former case the heat generated
would be equal to that produced by the combustion of fourteen earths of
solid coal, and in the latter case the amount would be 400 times
greater.
[Sidenote: SHIFTING OF ATOMS.]
Whenever a weight is lifted by a steam-engine in opposition to the force
of gravity an amount of heat is consumed equivalent to the work done;
and whenever the molecules of a body are shifted in opposition to their
mutual attractions work is also performed, and an equivalent amount of
heat is consumed. Indeed the amount of work done in the shifting of the
molecules of a body by heat, when expressed in ordinary mechanical work,
is perfectly enormous. The lifting of a heavy weight to the height of
1000 feet may be as nothing compared with the shifting of the atoms of a
body by an amount so small that our finest means of measurement hardly
enable us to determine it. Different bodies give heat different degrees
of trouble, if I may use the term, in shifting their atoms and putting
them in new places. Iron gives more trouble than lead; and water gives
far more trouble than either. The heat expended in this molecular work
is lost as heat; it does not show itself as temperature. Suppose the
heat produced by the combustion of an ounce of candle to be concentrated
in a pound of iron, a certain portion of that heat would go to perform
the molecular work to which I have referred, and the remainder would be
expended in raising the temperature of the body; and if the same amount
of heat were communicated to a pound of iron and to a pound of lead, the
balance in favour of temperature would be greater in the latter case
than in the former, because the heat would have less molecular work to
do; the lead would become more heated than the iron. To raise a pound of
iron a certain number of degrees in temperature would, in fact, require
more than three times the absolute quantity of heat which would be
required to raise a pound of lead the same number of degrees.
Conversely, if we place the pound of iron and the pound of lead, heated
to the same temperature, into ice, we shall find that the quantity of
ice melted by the iron will be more than three times that melted by the
lead. In fact, the greater amount of molecular work invested in the iron
now comes into play, the atoms again obey their own powerful forces, and
an amount of heat corresponding to the energy of these forces is
generated.
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