scholarly journals The diffusion of ions into gases at low pressure

1. In papers published in the ‘Proceedings’ of the Royal Society, the charges on ions produced by the action of Rontgen rays and radium on air were determined by a method depending on the diffusion of the ions, and in the course of the investigations it was observed that the removal of water- vapour from the gas produced a large change in the motion of negative ions. In this paper the results are given of some accurate experiments on the ions produced by radium, and experiments at low pressures on the motion of the ions produced by ultra-violet light are described. In the latter case, effects similar to those observed by Prof. Townsend when the gas was ionised by Rontgen rays have been found, and some interesting results at pressures lower than those previously employed have been obtained. 2. The arrangement of the apparatus is here reproduced (fig. 1). The ions are generated in the field A by radium placed in shallow horizontal grooves f , covered with aluminium foil, in brass blocks F. They pass under the action of the electric force through the grating g and the aperture h into the field B, which was kept constant by means of the brass rings G maintained at definite potentials. Here they diffuse and the ratio R of the charge received by the disc D to the charge received by the disc and the ring S together is measured. This ratio is a known function of c = N e Z/P, where e is the charge on an ion, N the number of molecules in a cubic centimetre of air at pressure P at the temperature of the laboratory, and Z the electric force in the field B.

A general method of finding the rate of diffusion of ions into a gas has been described in a previous paper, and an account was there given of the results obtained with ions produced by Röntgen rays. The present paper gives the results obtained with ions produced by a radio-active substance, by point discharges, and by ultra-violet light. The principle of the method consists in calculating the rate of diffusion from observations on the loss of conductivity of a gas as it passes along metal tubing. The experiments were arranged so that the loss due to diffusion should be much greater than the loss due to other causes. In order to ensure this, there are two effects which must be considered in fixing the dimensions of the tubing: the recombination which occurs when there are both positive and negative ions present in the gas; and the effect due to the mutual repulsion of the ions which takes place when most of the ions are charged with electricity of the same sign. It is therefore necessary either to correct for these sources of error or to arrange the conditions of the experiments so that the loss of conductivity due to these causes is negligible.


Some experiments by Prof. J. S. Townsend on the lateral diffusion of a narrow stream of ions moving in an electric field led to the conclusion that negative ions in perfectly dry air are much smaller than those in air containing a small quantity of moisture. It was consequently to be expected that the complete removal of water vapour would cause an increase in the velocity with which negative ions move under the influence of an electric field of force. At his suggestion the following investigation of the velocities of ions in air at low pressures was undertaken, and it was found that, while the complete removal of water vapour had only a small effect on the velocities of positive ions, yet the same cause increased the velocities of the negative ions by a factor varying between 2 and 30 for the range of pressures and electric forces used in the experiments. The method adopted was to let the ions travel between two gauzes under a known electric force for a time t and then to reverse the field. If v is the velocity of the ions and d is the distance between the gauzes, then ions starting from one gauze will reach the other if t ≮ d / v . If t is gradually decreased, it is possible to find, by means of an electrometer, when ions cease to reach the second gauze; when this happens v = d / t .


1899 ◽  
Vol 64 (402-411) ◽  
pp. 127-129 ◽  

The experiments here described consist mainly in determinations of the least degree of supersaturation necessary to cause water vapour to condense on nuclei from various sources.


In a previous communication (‘Phil. Trans.,’ A, vol. 189, p. 265, 1897) I described experiments proving that when dust-free air, initially saturated with water vapour, is allowed to expand adiabatically, condensation takes place, if the maximum degree of supersaturation resulting from the expansion exceeds a certain limit. Using v 2 / v 1 the ratio of the final to the initial volume as a measure of the expansion, we may describe the phenomena briefly as follows :— Condensation only takes place throughout the gas if v 2 / v 1 exceeds 1.25; the drops are comparatively few, provided a second limit ( v 2 / v 1 = 1.38) is not exceeded. Beyond this second limit the rate of increase in the number of drops with increasing expansion is extremely rapid, very dense fogs resulting from expansions even slightly exceeding this limit.


Clouds are produced in an expansion chamber filled with air and water vapour by irradiating with ultra-violet light through a quartz window, and expanding shortly afterwards. It is shown that the condensation does not occur upon charged particles, but on certain electrically neutral nuclei, not yet identified. By varying the wave-length of the ultra-violet light it is shown that the condensation is initiated by atomic oxygen, liberated by the action of the radiation on oxygen molecules. Similar effects are produced when an intense beam of deuterons is passed into the chamber.


When a metal plate is "illuminated" by Röntgen rays, part of the energy of these incident rays is coverted into high-speed secondary cathode particles, which are ejected from the plate in all directions. The mere detection of this emission of negative electricity is an easy matter, since the illuminated plate, if insulated in vacuo charges up positively. By measuring the rate of charging, it would be possible to determine the number of particles ejected per second, while by applying an electric force of such a magnitude and in such a direction as to stop the emission, it might be thought that their speed could be measured. In practice, however, this method of measuring velocities is restricted to slowly moving rays, such as are produced, for example, by ultra-violet light. The particles ejected by Röntgen rays have in most cases a speed corresponding to a potential fall through many thousands of volts, and at present it is not possible to perform accurate experiments with potentials of this magnitude. Quite the best way of determining high velocities is the magnetic deflection method, in which a magnetic force of known strength is applied to a fine beam of the moving particles in such a way as to act at right angles to their direction of motion; form observations of the curvature of the path described by the particles their speed can be calculated. This method, unfortunately, is at present impossible in the case of secondary cathode particles, since their intensity is never sufficient to allow of their being formed into anything like a narrow beam. There is, however, a method of attacking the problem which it is the object of this paper to outline. The experimental data available are somewhat incomplete, and the conclusions drawn from them of necessity share this incompleteness.


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