The Birth-Time of the World and Other Scientific EssaysJoly, John
Science
The Birth-Time of the World and Other Scientific Essays
Joly, John
Science
coefficient of friction comparable with the usual coefficients of
solids on solids, but when the pressure is increased, the
coefficient falls to about half this value.
The following table embodies some results obtained on the
friction of ice and glass, using the methods I have shown you. I
add some of the more carefully determined coefficients of other
observers.
Wt. in On Plate On Ice On Ice
Grams. Glass. at 0 deg. C. at 10 deg. C.
Angle. Coeff. Angle. Coeff. Angle. Coeff
Aluminium 2.55 121/2 deg. 0.22 12 deg. 0.21 131/2 deg. 0.24
Same 155 121/2 deg. 0.22 6 deg. 0.11 7 deg. 0.12
Brass 6.5 121/2 deg. 0.22 10 deg. 0.17 101/2 deg. 0.18
Same 107 121/2 deg. 0.22 5 deg. 0.09 6 deg. 0.10
Steel on steel (Morin) - - - - 0.14
Brass on cast iron (Morin) - - 0.19
Steel on cast iron (Morin) - - 0.20
Skate on ice (J. Mueller) - - - 0.016--0.032
Best-greased surfaces (Perry) - 0.03--0.036
You perceive from the table that while the friction of brass or
aluminium on glass is quite independent of the weight used, that
of brass or aluminium on ice depends in some way upon the weight,
and falls in a very marked degree when the weight is heavy. Now,
I think that if we had been on the look out for any abnormality
in the friction of hard substances on ice, we would have rather
anticipated a variation in the
265
other direction. We would have, perhaps, expected that a heavy
weight would have given rise to the greater friction. I now turn
to the explanation of this extraordinary result.
You are aware that it requires an expenditure of heat merely to
convert ice to water, the water produced being at the temperature
of the ice, _i.e._ at 0 deg. C., from which it is derived. The heat
required to change the ice from the solid to the liquid state is
the latent heat of water. We take the unit quantity of heat to be
that which is required to heat 1 kilogram of water 1 deg. C. Then if
we melt 1 kilogram of ice, we must supply it with 80 such units
of heat. While melting is going on, there is no change of
temperature if the experiment is carefully conducted. The melting
ice and the water coming from it remain at 0 deg. C. throughout the
operation, and neither the thermometer nor your own sensations
would tell you of the amount of heat which was flowing in. The
heat is latent or hidden in the liquid produced, and has gone to
do molecular work in the substance. Observe that if we supply
only 40 thermal units, we get only one-half the ice melted. If
only 10 units are supplied, then we get only one eighth of a
kilogram of water, and no more nor less.
I have ventured to recall to you these commonplaces of science
before considering a mode of melting ice which is less generally
known, and which involves no supply of heat on your part. This
method involves for its
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