scholarly journals The influence of exchange interaction and dynamic demagnetizing field on dispersion properties of Damon-Eshbach surface wave. Part 2. Dispersion relation.

2019 ◽  
Vol 2019 (9) ◽  
Author(s):  
V.I. Shcheglov ◽  
2010 ◽  
Vol 107 (6) ◽  
pp. 064505 ◽  
Author(s):  
Feiyan Cai ◽  
Zhaojian He ◽  
Degang Zhao ◽  
Zhengyou Liu

1978 ◽  
Vol 28 (11) ◽  
pp. 927-929 ◽  
Author(s):  
Deva N. Pattanayak ◽  
Joseph L. Birman

1975 ◽  
Vol 14 (1) ◽  
pp. 179-194 ◽  
Author(s):  
P. C. Clemmow ◽  
J. N. Elgin

The exact surface-wave dispersion relation is expressed in terms of elementary functions for a plasma characterized by a ‘resonance’ velocity distribution function. An approximate form of the relation is derived for the case when the thermal velocity spread is much less than c. The pure surface wave obtained by dropping the term responsible for Landau damping is compared with that predicted on the basis of a fluid model of the plasma. The effect of Landau damping is then investigated, both by analytic approximations and by computation. Two branches of the solution to the dispersion relation are found; and it is shown that the surface wave suffers increasingly severe damping as the frequency grows beyond 1/ √ 2 times the plasma frequency. It is argued that qualitatively similar damping would be present were the plasma to have a Maxwellian equilibrium distribution function.


2019 ◽  
Vol 16 (06) ◽  
pp. 1840030 ◽  
Author(s):  
Shishir Gupta ◽  
Santimoy Kundu ◽  
Prasenjit Pati

The objective of this paper is to study the effect of loosely bonded interface on torsional surface wave propagation in a fiber reinforced composite medium constrained between dry sandy layer and an anisotropic gravitating poroelastic substrate. All the media are assumed to be under initial stress. The dispersion relation on this proposed multilayer ground structure has been derived in closed form under certain boundary conditions, which contain Whittaker function and its derivative, which is further expanded asymptotically, retaining up to only the linear terms. The numerical solution for the limiting case of torsional surface waves is also discussed. As a special case of the problem, when the entire medium is isotropic and one of the upper layer vanishes and removing the initial stress and gravity, the dispersion relation obtained is in agreement with the classical Love type wave equation. The influence of various technical constants, such as sandy parameter, reinforcement parameter, porosity parameter, Biot’s gravity parameter, loosely bonded parameters, initial stress of both the layers and half spaces on the phase velocity of torsional surface wave has been pointed out by means of graphs.


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