Scientific American Supplement, No. 443, June 28, 1884 — John Shaqi
Scientific American Supplement, No. 443, June 28, 1884Various
Science
Scientific American Supplement, No. 443, June 28, 1884
Various
Science -- Periodicals
It is difficult to give the full explanation of the dust free spaces
in a few words, but we may say roughly that there is a molecular
bombardment from all warm surfaces by means of which small suspended
bodies get driven outward and kept away from the surface. It is a sort
of differential bombardment of the gas molecules on the two faces of a
dust particle somewhat analogous to the action on Mr. Crookes'
radiometer vanes. Near cold surfaces the bombardment is very feeble,
and if they are cold enough it appears to act toward the body, driving
the dust inward--at any rate, there is no outward bombardment
sufficient to keep the dust away, and bodies colder than the
atmosphere surrounding them soon get dusty. Thus if I hold this piece
of glass in a magnesium flame, or in a turpentine or camphor flame, it
quickly gets covered with smoke--white in the one case, black in the
other. I take two conical flasks with their surfaces blackened with
camphor black, and filling one with ice, the other with boiling water,
I cork them and put a bell jar over them, under which I burn some
magnesium wire; in a quarter of an hour or so we find that the cold
one is white and hoary, the hot one has only a few larger specks of
dust on it, these being of such size that the bombardment was unable
to sustain their weight, and they have settled by gravitation. We thus
see that when the air in a room is warmer than the solids in it--as
will be the case when stoves, gas-burners, etc., are used--things will
get very dusty; whereas when walls and objects are warmer than the
air--as will be the case in sunshine, or when open fireplaces are
used, things will tend to keep themselves more free from dust. Mr.
Aitken points out that soot in a chimney is an illustration of this
kind of deposition of dust; and as another illustration it strikes me
as just possible that the dirtiness of snow during a thaw may be
partly due to the bombardment on to the cold surface of dust out of
the warmer air above. Mr. Aitken has indeed suggested a sort of
practical dust or smoke filter on this principle, passing air between
two surfaces--one hot and one cold--so as to vigorously bombard the
particles on to the cold surface and leave the air free.
Public-domain text, read in full here on John Shaqi.
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