Steady-state electric discharge in a weakly ionized gas at thermal equilibrium

1969 ◽  
Vol 12 (4) ◽  
pp. 501-504
Author(s):  
D. P. Leper
2012 ◽  
Vol 97 (5) ◽  
pp. 55003 ◽  
Author(s):  
E. A. Lisin ◽  
O. S. Vaulina ◽  
O. F. Petrov ◽  
V. E. Fortov

Author(s):  
P. Segur ◽  
M. Yousfi ◽  
J. P. Boeuf ◽  
E. Marode ◽  
A. J. Davies ◽  
...  
Keyword(s):  

1980 ◽  
Vol 24 (3) ◽  
pp. 503-514 ◽  
Author(s):  
V. J. Žigman ◽  
B. S. Milić

The properties of certain wave modes excited in a weakly ionized plasma placed in an external d.c. electric field are analyzed from the standpoint of the linearized kinetic equation, the electron steady-state distribution function being taken in the form of the extended Margenau–Davydov and, in particular, Druyvesteinian. The presence of absolute stability cones formed by certain propagation directions is found. The corresponding critical values of the electron drift, destabilizing each of the modes considered, is also evaluated for a plasma with a Druyvesteinian distribution.


1977 ◽  
Vol 32 (7) ◽  
pp. 697-703
Author(s):  
Fr. Kaiser

Abstract The Peierls-Boltzmann transport equation for phonons, which was re-formulated and modified in a previous paper, is extended to be applicable to arbitrary interactions and phonon processes. As a rule, it turns out that only two types of steady state solutions are possible: hysteresis and threshold. These two solutions reveal the possibility of “transport phase transitions”, i. e. a transition from the “thermodynamic” branch to a “nonthermodynamic” one via a cumulative excitation. It is shown that both the threshold and the hysteresis situation exhibit pronounced analogies to phase transi­tions in thermal equilibrium. The dependence of the steady states from the relevant parameters is discussed.


1975 ◽  
Vol 14 (70) ◽  
pp. 125-136 ◽  
Author(s):  
R. H. Thomas

Holes drilled into thin areas of the Brunt Ice Shelf encounter a layer of liquid brine less than 1 m thick approximately at sea-level. Assuming the brine to be moving horizontally, analysis of its effects on thermal equilibrium gives an estimate of steady-state annual brine flow that is in good agreement with the value deduced from a percolation model. The effect of firn density on percolation rates is such that the slope of an active brine layer increases rapidly as ice thickness increases. However, the heat transport model predicts that brine layers are unlikely to be active in both very thick and very thin ice shelves.


2019 ◽  
Author(s):  
Rodrigo C. Palharini ◽  
Joao Luiz F. Azevedo ◽  
Craig White
Keyword(s):  
Gas Flow ◽  

Sign in / Sign up

Export Citation Format

Share Document