The Dynamic Characteristics of a Low Pressure Discharge
- 1 May 1952
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review B
- Vol. 86 (3) , 351-358
- https://doi.org/10.1103/physrev.86.351
Abstract
Square-wave modulation of current at a frequency of 167-400 cps was imposed on a dc discharge in a tube containing mercury vapor at a pressure of and argon at 3.5 mm (Hg). The intensity of and other data were recorded on oscillograms. Each sudden change of the arc current was accompanied by an instantaneous change in the same direction, of the longitudinal voltage gradient , the electron temperature , the 2537 output, and the ion current to the wall. These instantaneous changes were followed by much slower adjustments toward the steady-state values corresponding to the arc current. The time required for a rough adjustment was 0.2-0.5 msec when the current was increased, and 1-3 msec when it was decreased, for ratios of maximum to minimum current ranging from 1.6 to 3.9. When the current was decreased, there was an excess of ions that had to diffuse to the tube wall.
Keywords
This publication has 9 references indexed in Scilit:
- Gas Temperatures and Elastic Losses in Low Pressure Mercury-Argon DischargesJournal of Applied Physics, 1951
- Production of 2537 Radiation and the Role of Metastable Atoms in an Argon-Mercury DischargeJournal of Applied Physics, 1950
- Techniques for Measuring the Dynamic Characteristics of a Low Pressure DischargeJournal of Applied Physics, 1950
- Modulation of the Resonance Lines in a Cesium Arc*Journal of the Optical Society of America, 1947
- Cesium Vapor Lamps*Journal of the Optical Society of America, 1946
- Ionization and Excitation in Mercury Vapor Produced by Electron BombardmentPhysical Review B, 1939
- The Quantitative Study of the Collisions of Electrons with AtomsReviews of Modern Physics, 1933
- Electrical Discharges in Gases. Part I. Survey of Fundamental ProcessesReviews of Modern Physics, 1930
- A General Theory of the Plasma of an ArcPhysical Review B, 1929