The reason why : $b a careful collection of many hundreds of reasons for things which, though generally believed, are imperfectly understood. A book of condensed scientific knowledge for the million
John Stuart Mill · en
219. _Why is the air often found excessively hot in chalk districts?_
Because the soil _reflects_ upon objects near to it the heat of the
solar rays.
220. _How does the heat of the sun's rays ultimately become diffused?_
It is first _absorbed_ by the earth. Generally speaking, the earth
_absorbs_ heat by day, and _radiates_ it by night. In this way an
equilibrium of temperature is maintained, which we should not otherwise
have the advantage of.
221. _Does not the air derive its heat directly from the sun's rays?_
Only partially. It is estimated that the air absorbs only _one-third_
of the caloric of the sun's rays--that is to say, that a ray of solar
heat, entering our atmosphere at its most attenuated limit (a height
supposed to be about _fifty miles_), would, in passing through the
atmosphere to the earth, part with only one-third of its calorific
element.
[Verse: "As for the earth, out of it cometh bread; and under it is
turned up as it were fire."--JOB XXVIII.]
222. _What becomes of the remaining two-thirds of the solar heat?_
They are _absorbed_ chiefly by the _earth_, the great medium of
calorific _absorption_; but some portions are taken up by _living
things_, both animal and vegetable. When the _rays of heat_ strike upon
the earth's surface, they are passed from particle to particle into the
interior of the earth's crust. Other portions are distributed through
the air and water by _convection_, and a third portion is thrown
back into space by _radiation_. These latter phenomena will be duly
explained as we proceed.
223. _How do we know that heat is absorbed, and conducted into the
internal earth?_
It is found that there is a given depth beneath the surface of the
globe at which an equal temperature prevails. The depth increases as we
travel south or north from the equator, and corresponds with the shape
of the earth's surface, _sinking under the valleys, and rising under
the hills_.
224. _Why may we not understand that this internal heat of the earth
arises, as has been supposed by many philosophers, from internal
combustion?_
Because recent investigations have thrown considerable and satisfactory
light upon the subject. It has been ascertained that the internal
temperature of the earth _increases_ to a certain depth, _one degree in
every fifty feet_. But that below that depth the temperature _begins to
decline_, and continues to do so with every increase of depth.
225. _Do plants absorb heat?_
Yes. They both _absorb_ and _radiate_ heat, under varying
circumstances. The majestic tree, the meek flower, the unpretending
grass, all perform a part in the grand alchemy of nature.
[Verse: "Consider the lilies of the field, how they grow; they toil
not, neither do they spin."]