The Romance of Modern Chemistry
Forfatter: James C. Phillip
År: 1912
Forlag: Seeley, Service & Co. Limited
Sted: London
Sider: 347
UDK: 540 Phi
A Description in non-technical Language of the diverse and wonderful ways in which chemical forces are at work and of their manifold application in modern life.
With 29 illustrations & 15 diagrams.
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NATURE’S STORES OF FUEL
We must not forget to include in our fuel capital the
vast stock of timber on the surface of the globe, and the
enormous quantities also of peat found in many countries.
How far may we regard these as reliable sources of fuel ?
Wood, is, of course burned in many countries where there
is a large extent of forest, but it would be absolute
madness to use up all our timber in this way. It is the
vegetation of the world which, as we shall see, is the
necessary counterpart of animal life, and gradually to
cut down all the forests on the face of the globe would
be a suicidal policy. Besides, there is a large demand for
timber for architectural and constructive purposes, and
even as matters are at present, the forest-covered land of
North America and Europe is being laid bare at a rapidly
increasing rate. Trees do not grow in a hurry, and once
the primeval forests are cut down, the keeping up of a
supply of timber by planted trees is hardly feasible.
And what about peat? In Ireland alone there are
over 1,000,000 acres of peat bogs, and it is estimated
that an acre of a bog of an average depth of even 8
feet would yield about 1250 tons of dried peat. In
Russia there are about 100,000,000 acres of bogs, so
that altogether the fuel stored up in the form of peat
must be very considerable. What militates against the
use of peat as a fuel is the very large amount of moisture
which it holds. When freshly dug it may contain as
much as 80 to 90 per cent, of water, and the problem is
how best to get rid of this and obtain the fibre of the
peat in a condition fit for burning. The usual method
of exposing the wet peat to air until it is dry requires
much time and space. It is further a very bulky fuel,
and, probably owing to these causes, the output of peat
has never been much greater than sufficed for local de-
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