Classical Diffusion of a Stationary Toroidal Plasma

1969 ◽  
Vol 12 (1) ◽  
pp. 255 ◽  
Author(s):  
John L. Johnson
1971 ◽  
Vol 13 (10) ◽  
pp. 905-912 ◽  
Author(s):  
E K Maschke

1989 ◽  
Vol 54 (7) ◽  
pp. 1821-1829
Author(s):  
Bedřich Porsch ◽  
Simon King ◽  
Lars-Olof Sundelöf

The differences between the QELSS and classical diffusion coefficient of a polydisperse polymer resulting from distinct definitions of experimentally accessible average values are calculated for two assumed specific forms of molar mass distributions. Predicted deviations are compared with the experiment using NBS 706 standard polystyrene. QELSS Dz of this sample relates within 2-4% to the classical diffusion coefficient, if the Schulz-Zimm molar mass distribution is assumed to be valid. In general, differences between the height-area and QELSS diffusion coefficient of about 20% may be found for Mw/Mn ~ 2, and this value may increase above 35%, if strongly tailing molar mass distribution pertains to the sample.


2021 ◽  
Vol 92 (2) ◽  
pp. 023506
Author(s):  
A. Goriaev ◽  
T. Wauters ◽  
S. Möller ◽  
R. Brakel ◽  
S. Brezinsek ◽  
...  

1973 ◽  
Vol 16 (8) ◽  
pp. 1329 ◽  
Author(s):  
J. C. Hosea
Keyword(s):  

1987 ◽  
Vol 38 (2) ◽  
pp. 209-222 ◽  
Author(s):  
Hussain M. Rizk

The relation between various surface quantities required in hydrodynamic calculations, and the relation between the parallel and perpendicular currents in an arbitrary magnetic toroidal plasma configuration with scalar pressure, are generalized to the case of anisotropic pressure. Magnetic co-ordinates for hydrodynamic equilibria in this configuration are defined. A general expression for the mean velocity of diffusion through a magnetic surface, on the basis of the one-fluid magnetohydrodynamic equation with anisotropic pressure, is derived.


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