Is Mars habitable? A critical examination of Professor Percival Lowell's book "Mars and its canals," with an alternative explanation — John Shaqi
Is Mars habitable? A critical examination of Professor Percival Lowell's book "Mars and its canals," with an alternative explanationWallace, Alfred Russel
Science
Is Mars habitable? A critical examination of Professor Percival Lowell's book "Mars and its canals," with an alternative explanation
Wallace, Alfred Russel
Lowell, Percival, 1855-1916. Mars and its canals; Mars (Planet)
Heat is now believed to be entirely due to ether-vibration, which
produces a correspondingly rapid vibration of the molecules of matter,
causing it to expand and producing all the phenomena we term 'heat.' We
can conceive this vibration to increase indefinitely, and thus there
would appear to be no necessary limit to the amount of heat possible,
but we cannot conceive it to decrease indefinitely at the same uniform
rate, as it must soon inevitably come to nothing. Now it has been found
by experiment that gases under uniform pressure expand 1/273 of their
volume for each degree Centigrade of increased temperature, so that in
passing from 0° C. to 273° C. they are doubled in volume. They also
decrease in volume at the same rate for each degree below 0° C. (the
freezing point of water). Hence if this goes on to-273° C. a gas will
have no volume, or it will undergo some change of nature. Hence this is
called the zero of temperature, or the temperature to which any matter
falls which receives no heat from any other matter. It is also sometimes
called the temperature of space, or of the ether in a state of rest, if
that is possible. All the gases have now been proved to become, first
liquid and then (most of them) solid, at temperatures considerably above
this zero.
The only way to compare the proportional temperatures of bodies, whether
on the earth or in space, is therefore by means of a scale beginning at
this natural zero, instead of those scales founded on the artificial
zero of the freezing point of water, or, as in Fahrenheit's, 32° below
it. Only by using the natural zero and measuring continuously from it
can we estimate temperatures in relative proportion to the amount of
heat received. This is termed the absolute zero, and so that we start
reckoning from that point it does not matter whether the scale adopted
is the Centigrade or that of Fahrenheit.
_The Complex Problem of Planetary Temperatures._
Public-domain text, read in full here on John Shaqi.
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