The electron, its isolation and measurement and the determination of some of its properties — John Shaqi
The electron, its isolation and measurement and the determination of some of its propertiesMillikan, Robert Andrews
Philosophy
The electron, its isolation and measurement and the determination of some of its properties
Millikan, Robert Andrews
Electrons
But in order to form the cloud, Thomson utilized C. T. R. Wilson’s
discovery just touched upon above, that a sudden expansion and
consequent cooling of the air in (Fig. 1) would cause the ions
in to act as nuclei for the formation of water droplets. To
produce this expansion the piston is suddenly pulled down so as
to increase the volume of the space above it. A cloud is thus formed
about the ions in . Instead of measuring the weight of this cloud
directly, as Townsend had done, Thomson computed it by a theoretical
consideration of the amount of cooling produced by the expansion and
[Pg 52]
the known difference between the densities of saturated water vapor
at the temperature of the room and the temperature resulting from the
expansion. This method of obtaining the weight of the cloud was less
direct and less reliable than that used by Townsend, but it was the
only one available with Thomson’s method of obtaining an ionized gas
and of measuring the charge per cubic centimeter on that gas. The
average size of the droplets was obtained precisely as in Townsend’s
work by applying Stokes’s Law to the observed rate of fall of the top
of the cloud in chamber .
[Pg 53]
The careful consideration of Thomson’s experiment shows that it
contains the theoretical uncertainties involved in Townsend’s work,
while it adds some very considerable experimental uncertainties. The
most serious of the theoretical uncertainties arise from (1) the
assumption of Stokes’s Law, and (2) the assumption that the number of
ions is equal to the number of droplets. Both observers sought for some
experimental justification for the second and most serious of these
assumptions, but subsequent work by H. A. Wilson, by Quincke, and by
myself has shown that clouds formed by C. T. R. Wilson’s method consist
in general of droplets some of which may carry one, some two, some
ten, or almost any number of unit charges, and I have never been able,
despite quite careful experimenting, to obtain conditions in which it
was even approximately true that each droplet carried but a single unit
charge. Quincke has recently published results from which he arrives at
the same conclusion.[35]
Public-domain text, read in full here on John Shaqi.
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