The Chautauquan, Vol. 04, October 1883Chautauqua Literary and Scientific Circle
Philosophy
The Chautauquan, Vol. 04, October 1883
Chautauqua Literary and Scientific Circle
Chautauqua Institution -- Periodicals; Chautauqua Literary and Scientific Circle -- Periodicals
Now what is this vapor of water? You will understand its nature if you
watch what takes place when a kettle boils. From the mouth of the spout
a stream of white cloud comes out into the air. It is in continual
motion; its outer parts somehow or other disappear, but as fast as they
do so they are supplied by fresh materials from the kettle. The water
in the kettle is all the while growing less, until at last, if you do
not replenish it, the whole will be boiled away, and the kettle left
quite dry. What has become of all the water? You have changed it into
vapor. It is not destroyed or lost in any way, it has only passed from
one state into another, from the liquid into the gaseous form, and is
now dissolved in the air.
Carbonic acid gas is also one of the invisible substances of the
atmosphere, of which, though it forms no more than four parts in
every ten thousand, yet it constitutes an important ingredient. You
will understand how important it is when you are told that, from this
carbonic acid in the air, all the plants which you see growing upon the
land extract nearly the whole of their solid substance. When a plant
dies and decays, the carbonic acid is restored to the air again. On the
other hand, plants are largely eaten by animals, and help to form the
framework of their bodies. Animals in breathing give out carbonic acid
gas; and when they die, and their bodies decay, the same substance is
again restored to the atmosphere. Hence the carbonic acid of the air is
used to build up the structure both of plants and animals, and is given
back again when these living things cease to live. There is a continual
coming and going of this material between the air and the animal and
vegetable kingdoms.
You know that though you can not see the air you can feel it when it
moves. A light breeze, or a strong gale, can be just as little seen by
the eye as still air; and yet we readily feel their motion. But even
when the air is still it can make itself sensible in another way, viz:
by its temperature. For air, like common visible things, can be warmed
and cooled.
This warming and cooling of the air is well illustrated by what
takes place in a dwelling-house. If you pass out of a warm room, on
a winter’s day, into the open air when there is no wind, you feel a
sensation of cold. Whence does this sensation come? Not from anything
you can see, for your feet, though resting on the frozen ground, are
protected by leather, and do not yet feel the cold. It is the air which
is cold, and which encircles you on all sides, and robs you of your
heat; while at the same time you are giving off or radiating heat from
your skin into the air. On the other hand, if, after standing a while
in the chilly winter air, you return into the room again, you feel a
sensation of pleasant warmth. Here, again, the feeling does not come
from any visible object, but from the invisible air which touches every
part of your skin, and is thus robbed of its heat by you.
Public-domain text, read in full here on John Shaqi.
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