- Open Access
Electrogravitational stability of oscillating streaming fluid cylinder ambient with a transverse varying electric field
© Hasan; licensee Springer. 2011
- Received: 29 May 2011
- Accepted: 11 October 2011
- Published: 11 October 2011
The electrogravitational instability of a dielectric oscillating streaming fluid cylinder surrounded by tenuous medium of negligible motion pervaded by transverse varying electric field has been investigated for all the perturbation modes. The model is governed by Mathieu second-order integro-differential equation. Some limiting cases are recovering from the present general one. The self-gravitating force is destabilizing only in the axisymmetric perturbation for long wavelengths, while, the axial electric field interior, the fluid has strong destabilizing effect for all short and long wavelengths. The transverse field is strongly stabilizing. In the case of non-axisymmetric perturbation, the self-gravitating force is stabilizing for short and long waves, while the electric field has stabilizing effect on short waves.
- electrogravitational stability
The stability of self-gravitating fluid cylinder has been studied, for the first time, by Chandrasekhar and Fermi . Later on, Chandrasekhar  made several extensions as the fluid cylinder is acted by different forces. Radwan [3, 4] studied the stability of an ideal hollow jet. Radwan  considered that the fluids are penetrated by constant and uniform electric fields. The stability of different cylindrical models under the action of self-gravitating force in addition to other forces has been elaborated by Radwan and Hasan [5, 6]. Radwan and Hasan  studied the gravitational stability of a fluid cylinder under transverse time-dependent electric field for axisymmetric perturbations. Hasan [7, 8] has discussed the stability of oscillating streaming fluid cylinder subject to combined effect of the capillary, self-gravitating, and electrodynamic forces for all axisymmetric and non-axisymmetric perturbation modes. Hasan [7, 8] studied the instability of a full fluid cylinder surrounded by self-gravitating tenuous medium pervaded by transverse varying electric field under the combined effect of the capillary, self-gravitating, and electric forces for all the modes of perturbations.
Geophysics: the fluid of the core of the Earth and other theorized to be a huge MHD dynamo that generates the Earth's magnetic field because of the motion of the liquid iron.
Astrophysics: MHD applies quite well to astrophysics since 99% of baryonic matter content of the universe is made of plasma, including stars, the interplanetary medium, nebulae and jets, stability of spiral arm of galaxy, etc. Many astrophysical systems are not in local thermal equilibrium, and therefore require an additional kinematic treatment to describe all the phenomena within the system.
Engineering applications: there are many forms in engineering sciences including oil and gas extraction process if it surrounded by electric field or magnetic field, gas and steam turbines, MHD power generation systems and magneto-flow meters, etc.
In this article, we aim to investigate the stability of oscillating streaming self-gravitating dielectric incompressible fluid cylinder surrounded by tenuous medium of negligible motion pervaded by transverse varying electric field for all the axisymmetric and non-axisymmetric perturbation modes.
where ω is constant and U is the speed at time t = 0.
The basic equations for investigating the problem under consideration are being the combination of the ordinary hydrodynamic equations, Maxwell equations concerning the electromagnetic theory, and Newtonian self-gravitating equations concerning the self-gravitating matter (see [2, 7–10]).
where ρ, , and P are the fluid density, velocity vector, and kinetic pressure, respectively, and and are the electric field intensity and self-gravitating potential of the fluid while and are these of tenuous medium surrounding the fluid cylinder, and G is the gravitational constant.
where ϕ and ψ are the potential of the velocity of the fluid and electrical potential.
where the subscript 0 here and henceforth indicates unperturbed quantities.
where η(t) is the amplitude of the perturbation at an instant time t, k, any real number, is the longitudinal wave number along z-direction while m, an integer, is the azimuthal wave number.
where A1(t), B1(t), B2(t), C1(t), and C2(t) are arbitrary functions of integrations to be determined, while I m (kr) and K m (kr) are the modified Bessel functions of the first and second kind of order m.
The non-singular solutions of the linearized perturbation equation given by the systems (21)-(25) and the solutions (16)-(17) of the unperturbed systems (12)-(14) must satisfy certain boundary conditions. Under the present circumstances, these appropriate boundary conditions could be applied as follows.
(i) Kinematic conditions
where x = k R0 is, dimensionless, the longitudinal wave number.
(ii) Self-gravitating conditions
(iii) Electrodynamic condition
where the quantity ξ1 is given in Appendix 1.
(iv) The dynamical stress condition
where the quantity β11 and β12 is given in Appendix I.
Equation 47 is Mathieu differential equation. The properties of the Mathieu functions are explained and investigated by Melaclan . The solutions of Equation 47, under appropriate restrictions, could be stable and vice versa. The conditions required for periodicity of Mathieu functions are mainly dependent on the correlation between the parameters a and q. However, it is well known, see , that (a, q)-plane is divided essentially into two stable and unstable domains separated by the characteristic curves of Mathieu functions. Thence, we can state generally that a solution of Mathieu integro-differential equation is unstable if the point (a, q) say, in the (a, q)-plane lies internal and unstable domain, otherwise it is stable.
The appropriate solutions of Equation 47 are given in terms of what called ordinary Mathieu functions which, indeed, are periodic in time t with period π and 2π.
where Δ(0) is the Hill's determinant.
An approximation criterion for the stability near the neighborhood of the first stable domains of the Mathieu stability domains given by Morse and Feshbach  which is valid only for small values of h2 or q, i.e., the frequency ω of the electric field is very large.
The electrogravitational stability and instability investigations analysis should be carried out in the following two cases
(i). 0 < b < 2/3
and this is contradiction, so α1 must be positive and consequently α2 ≥ 0 as well (noting that α2 > α1). This means that both the quantities (h2 -α1) and (h2 -α2) are negative and that in turn show that the inequality (51) is identically satisfied.
(ii). 2/3 < b < 1
In this case, in which b < 1 and simultaneously 3b > 2, it is found that Δ2 is negative, i.e., Δ is imaginary; therefore, the two roots α1 and α2 are complex. We may prove that the inequality (51) is satisfied as follows.
which is positive definite.
where σ is the temporal amplification and note by the way that has a unit of time. The relation (62) is identical to the gravitational dispersion relation derived for the first time by Chandrasekhar and Fermi . In fact, they  have used a totally different technique rather than that used here. They have used the method of representing the solenoidal vectors in terms of poloidal and toroidal vector fields for axisymmetric perturbation.
To determine the effect of ω, it is found more convenient to investigate the eigenvalue relation (62) since the right side of it is the same the middle side of (60).
based on the values of x.
Here, it is found that the quantity Q0 (x) may be positive or negative depending on x α 0 values. Numerical investigations and analysis of the relation (62) reveal that σ2 is positive for small values of x while it is negative in all other values of x. In more details, it is unstable in the domain 0 < x < 1.0667 while it is stable in the domains 1.0667 ≤ x < ∞ where the equality is corresponding to the marginal stability state.
Therefore, we deduce that the electrodynamic force (with a periodic time electric field) has stabilizing influence and could predominate and overcoming the self-gravitating destabilizing influence of the dielectric fluid cylinder dispersed in a dielectric medium of negligible motion.
However, the self-gravitating destabilizing influence could not be suppressed whatever is the greatest value of the magnitude and frequency of the periodic electric field because the gravitational destabilizing influence will persist.
For β = 0.5 corresponding to M = 0.1, 0.3, 0.5, 0.7, 1.0, and 1.5 it is found that the electrogravitational unstable domains are 0 < x < 1.1175, 0 < x <1.19759, 0 < x < 1.27235, 0 < x 1.29599, 0 < x < 1.362741, and 0 < x < 1.3978, the neighboring stable domains are 1.1175 ≤ x < ∞, 1.19759 ≤ x < ∞, 1.27235 ≤ x < ∞, 1.29599 ≤ x < ∞, 1.362741 ≤ x < ∞, and 1.3978 ≤ x < ∞, where the equalities correspond to the marginal stability states (see Figure 2).
For β = 1.0 corresponding to M = 0.1, 0.3, 0.5, 0.7, 1.0, and 1.5 it is found that the electrogravitational unstable domains are 0 < x < 1.22669, 0 < x < 1.5266, 0 < x < 1.750969, 0 < x < 1.90513, 0 < x < 2.05422, and 0 < x < 2.19341, the neighboring stable domains are 1.22669 ≤ x < ∞, 1.5266 ≤ x < ∞, 1.750969 ≤ x < ∞, 1.90513 ≤ x < ∞, 2.05422 ≤ x < ∞, and 2.19341 ≤ x < ∞, where the equalities correspond to the marginal stability states (see Figure 3).
For β = 1.5 corresponding to M = 0.1, 0.3, 0.5, 0.7, 1.0, and 1.5 it is found that the electrogravitational unstable domains are 0 < x < 1.35924, 0 < x < 1.9735, 0 < x < 2.3982, 0 < x < 2.6563, 0 < x < 2.8835, and 0 < x < 3.0798, the neighboring stable domains are 1.35924 ≤ x < ∞, 1.9735 ≤ x < ∞, 2.3982 ≤ x < ∞, 2.6563 ≤ x < ∞, 2.8835 ≤ x < ∞, and 3.0798 ≤ x < ∞, where the equalities correspond to the marginal stability states (see Figure 4).
For β = 2.5, corresponding to M = 0.1, 0.3, 0.5, 0.7, 1.0, and 1.5 it is found that the electrogravitational fluid cylinder is completely stable not only for short wavelengths, but also for very long wavelengths and the gravitational unstable domains are completely suppressed (see Figure 5).
For β = 3.0, corresponding to M = 0.1, 0.3, 0.5, 0.7, 1.0 and 1.5 it is found that the electrogravitational fluid cylinder is completely stable not only for short wavelengths, but also for very long wavelengths and the gravitational unstable domains are completely suppressed (see Figure 6).
From the presented numerical results, we may deduce the following. For the same value of M, it is found that the unstable domains are increasing with increasing of β values. This means that the influence of electric field has a destabilizing effect for all short and long wavelengths.
If β > 2.0, then the model is completely stable not only for short wave lengths, but also for long wave lengths.
We are grateful to the Editor of the Journal and the Reviewers for their suggestions and comments on this article.
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