Aspects of plant life; with special reference to the British floraPraeger, R. Lloyd (Robert Lloyd)
Science
Aspects of plant life; with special reference to the British flora
Praeger, R. Lloyd (Robert Lloyd)
Plants -- Great Britain
Vegetation as we know it on our world requires certain physical and
chemical conditions for its existence. For instance, a temperature
which, at least during the growing season, is well above the
freezing-point of water is requisite; yet the temperature must remain a
long way below the boiling-point of water; neither could plants as we
know them exist in the absence of an atmosphere containing oxygen,
carbon dioxide, and water vapour, and incidentally, by its capacity for
retaining heat, warding off violent extremes of temperature which
otherwise would be a daily and nightly occurrence. What evidence is
there as to the condition in these respects of those heavenly bodies
which are sufficiently near to allow us to know something of them? To
take first our own Moon. Astronomers are agreed that on the Moon there
is neither air nor water; it is a dead mass of solid material, scorched
by the Sun by day, held in the grip of appalling frost by night. The
Moon was no doubt at some remote period of the Earth’s history cast off
from that body, and it carried off with it a portion of the Earth’s
atmosphere, or of the materials which later formed the Earth’s
atmosphere. But the attraction of the Moon is so small that it was
unable to retain these gases on its surface; they diffused into space,
much of them returning probably to the Earth, leaving the Moon without
any covering of nitrogen or oxygen or hydrogen or water vapour, and thus
condemning it to permanent sterility.
As regards Mercury, the planet nearest the Sun, conditions appear
equally unfavourable. Mercury has ceased to revolve round the Sun, and
continually presents one side towards that luminary. On the opposite
side an extraordinarily low temperature prevails, low enough to solidify
and bind permanently most of the gases of any possible atmosphere;
while, on the other side, the very high temperature, due to perpetual
and intense sunshine, has assisted the diffusion into space of the more
volatile gases, such as hydrogen, which might have remained unfrozen.
Public-domain text, read in full here on John Shaqi.
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