Appletons' Popular Science Monthly, May, 1900: Vol. 57, May, 1900 to October, 1900Various
Science
Appletons' Popular Science Monthly, May, 1900: Vol. 57, May, 1900 to October, 1900
Various
Science -- Periodicals; Technology -- Periodicals
In every chemical change a definite amount of heat is either liberated
or absorbed--a distinct, measurable quantity. This fact was established
by Hess in 1840, and since then the thermal values of many reactions
have been determined, notably by Thomsen in Denmark and Berthelot
in France. The data are already numerous, but as yet they have not
been co-ordinated into any general law. They are in great measure the
raw material with which some future scholar is to build. One fact,
however, is already clear--namely, that the heat of formation or
of combustion of any compound is conditioned by its structure. Two
isomeric substances may differ widely in their calorific constants, an
observation which has repeatedly been verified. Thus the conception of
structure, of atomic grouping, appears again a chief factor in a set of
unsolved problems.
In the relations of chemistry to heat perhaps the greatest advances
have been made in the extension of our resources, particularly in
regard to the development and control of temperatures. At the beginning
of the century the range of temperatures available to the chemist was
narrowly limited--from the freezing point of mercury at one end to the
heat of a blast furnace at the other. His command of heat and cold are
now vastly greater than then, and the steps which have been taken are
worth tracing.
At the lower end of the scale the greatest progress has been made
through the liquefaction of gases. When a liquid evaporates, heat is
absorbed, or, reversely stated, cold is produced, and the more rapid
the evaporation the greater is the cooling effect. A command of more
volatile liquids is therefore a command of cold, and the liquefied
gases represent the extreme limit of our power in that direction.
Near the beginning of the century, by combining cold and pressure,
sulphurous acid and chlorine were reduced to the liquid state. In
1823 Faraday succeeded in liquefying still other gases, and in 1835
Thilorier went even further and reduced carbonic acid to a snowlike
solid. Liquid chlorine, sulphurous acid, and carbonic acid, stored in
strong cylinders of steel, are now commercial products, manufactured
and sold in large quantities like any other merchandise. They can be
transported to long distances and kept indefinitely, to the great
convenience of chemists and the furtherance of research.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account