Scientific American Supplement, No. 363, December 16, 1882Various
Science
Scientific American Supplement, No. 363, December 16, 1882
Various
Science -- Periodicals
Where water containing such mineral and suspended matter is fed to a
steam boiler, there results a combined deposit, of which the carbonate
of lime usually forms the greater part, and which remains more or less
firmly adherent to the inner surfaces of the boiler, undisturbed by the
force of the boiling currents. Gradually accumulating, it becomes harder
and thicker, and, if permitted to accumulate, may at length attain such
thickness as to prevent the proper heating of the water by any fire that
may be maintained in the furnace. Dr. Joseph G. Rogers, who has made
boiler waters and incrustations a subject of careful study, declares
that the high heats necessary to heat water through thick scale will
sometimes actually convert the scale into a species of glass, by
combining the sand, mechanically separated, with the alkaline salts. The
same authority has carefully estimated the non-conducting properties
of such boiler incrustations. On this point he remarks that the evil
effects of the scale are due to the fact that it is relatively a
nonconductor of heat. As compared with iron, its conducting power is
as 1 to 37½, consequently more fuel is required to heat water in an
incrusted boiler than in the same boiler if clean. Rogers estimates that
a scale 1-16th of an inch thick will require the extra expenditure of
15 per cent. more fuel, and this ratio increases as the scale grows
thicker. Thus, when it is one-quarter of an inch thick, 60 per cent.
more fuel is needed; one-half inch, 112 per cent. more fuel, and so on.
Rogers very forcibly shows the evil consequences to the boiler from the
excessive heating required to raise steam in a badly incrusted boiler,
by the following illustration: To raise steam to a pressure of 90 pounds
the water must be heated to about 320° Fahr. In a clean boiler of
one-quarter inch iron this may be done by heating the external surface
of the shell to about 325° Fahr. If, now, one-half an inch of scale
intervenes between the boiler shell and the water, such is its quality
of resisting the passage of heat that it will be necessary to heat the
fire surface to about 700°, almost to a low red heat, to effect the same
result. Now, the higher the temperature at which iron is kept the more
rapidly it oxidizes, and at any heat above 600° it very soon becomes
granular and brittle, and is liable to bulge, crack, or otherwise give
way to the internal pressure. This condition predisposes the boiler to
explosion and makes expensive repairs necessary. The presence of such
scale, also, renders more difficult the raising, maintaining, and
lowering of steam.
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