The progression of nonlinear electron-acoustic waves (EAWs) in a magnetized and collision-free plasma made up of cold inertial electrons, inertialess superthermal electrons, and stationary background ions with special reference to Saturn’s magnetosphere (SMS) is explored. The method of reductive perturbation (MRP) is employed to obtain the evolution equation (i.e., Zakharov– Kuznetsov equation (ZKE)) that governs the propagation of electron acoustic solitons (EASs). Using the elegant and efficient Hirota bilinear method (HBM), multi-soliton solutions (MSSs) of the ZKE are determined. The impact of the effects of hot-to-cold electron density ratio, magnetic field (MF) strength, and superthermality on single as well as the interaction of EASs is examined. Estimates of the values of the electric field at several radii of SMS (i.e., 12Rs − 17.8Rs, where Rs is the radius of Saturn) are presented, which are found in μV/m to mV/m range and are in perfect agreement with the data from Cassini radio and plasma wave science wideband receiver. Moreover, the influence of the relevant plasma parameters on the interaction time and spatial extent of the interacting EASs is also explored.
In connection with double layers, electrostatic solitary waves (SWs) were observed in different plasma regions, first in the terrestrial auroral zone on S3-3 mission in 1970,1,2 and since then they have been observed in the terrestrial magnetotail,3 magnetopause,4 magnetosheath,5 and bow shock.6 Apart from the terrestrial environment, SWs have been observed in the proximity of Jupiter’s moon Europa7 and Saturn.8 The SWs are the pulses in the electric field waveform data and are formed when the dipole antenna is aligned with the background magnetic field.8 Electron-acoustic solitons (EASs) are associated with the high-frequency (HF) component (HFC) of broadband electrostatic noise (BEN) and have been observed in the dayside auroral ionosphere by Viking spacecraft.9 Gurnett et al.10 initially identified the BEN that was observed in several missions predominantly at the boundary layer along auroral field lines and in turbulent sweep but was not linked with the electrostatic SWs. Fast Fourier transform was used by Matsumoto et al.3 to transform the magnetotail findings of the electrostatic SWs and BEN (being observed in the time and frequency domains, respectively) to make a connection between them.11
HF electrostatic waves have caught the attention of numerous researchers on account of their observations in the laboratory12,13 and space plasmas.14,15 The electron-acoustic waves (EAWs) may exist in plasmas comprising two non-isothermal populations (cold and hot) of electrons with cold background ions.16 The inertia can be provided by cold electrons, whereas the hot-electron thermal pressure is the source of the restoring force, and the massive ions play the role of a neutralizing background.16 The two-temperature electrons (TTEs) population plasmas have been reported in magnetospheres of Earth, Saturn, laser-plasma corona, and other planetary magnetospheres.17,18 The existence of EAWs was initially proposed by Fried and Gould in 196119 and later confirmed experimentally by Henry and Trguier in 1972.20 These HF electrostatic waves have frequency ω between ion plasma frequency ωpi and electron plasma frequency ωpe and the phase velocity (PhV) λ obeying the inequality , where and , are, respectively, the cold and hot electron’s thermal velocities.21
The nonlinear studies of EA solitary waves (EASWs) have been reported by various researchers both in unmagnetized22,23 and magnetized plasmas.24,25 Plasmas consisting of TTEs with stationary ions were studied in the context of EASWs using the method of reductive perturbation (MRP) and Sagdeev potential approach.26 They inferred that MRP is not appropriate to study the medium-strength Korteweg-de Vries (KdV) solitons. Devanandhan et al.27 explored the EAWs in an unmagnetized multicomponent plasma with non-isothermal electrons and background ions. The authors concluded that the amplitude of the EAS is affected by the cold electron temperature and the density of the superthermal electrons. EASs have been studied in a multicomponent plasma comprising cold electrons, hot electrons, beam electrons, and ions.22 It was reported that the electron beam component in the plasma causes generation of the compressive EASs, however, Verheest et al.28 added that the positive polarity potential EASs are also possible without an electron beam, provided the hot-electron inertia is taken into account. Dayside measurements of the Viking spacecraft from the auroral zone have been examined by considering the findings of a plasma model for EASs by Singh et al.15
Magnetized plasmas have also been extensively studied by many authors over the years. For instance, Mohan and Buti29 explored the two-component current carrying magnetoplasma by obtaining a modified KdV (mKdV) equation with hot ions and cold electrons. The authors deduced that the electron to ion temperature ratio (Te/Ti) affects the soliton amplitude and hence its velocity. The propagation of EASs in a high beta multicomponent plasma with two non-isothermal ions having mass disparity was also examined.30 Supersonic holes were shown along with solitons that were reported to be caused by large amplitude perturbations. Dubouloz et al.31 investigated the generation of turbulence in the dayside auroral zone by a gas of EASs in magnetoplasmas. The results were compared with the Viking findings in the dayside auroral zone to explain the high-frequency component of BEN. Small amplitude compressive solitons can be classified as three-dimensional EA beam solitons in an auroral return current region. Berthomier et al.32 showed that at altitudes less than 4000 km (FAST altitude range), spherical SWs were observed, while at high altitudes over the POLAR altitude range, the SWs were seen to be stretched out transverse to the magnetic field. They surmised that the formation of fast solitons observed by FAST and POLAR missions could be generated by the slow EASs.
Classical plasmas are high-temperature tenuous plasmas naturally occurring in near-earth space plasmas, the magnetosphere of Mercury, solar wind, and Saturn.33 The electrons have been considered Maxwellian distribution (MD) in most of the research studies on EASs. However, data from satellites reveal the distribution of electrons to deviate from MD in space plasmas where collisions of the particles are infrequent.34,35 Such distribution of electrons is described as kappa distribution, which is identical to MD at low energies, but, exhibits a departure from it at high energies.36 Vasyliunas37 led the way by proposing kappa distribution to fit the findings of OGO I and OGO III from the terrestrial magnetosphere.35 Since then, it has been shown by numerous observations that kappa distribution with 2 ≤ κ ≤ 6 fits the terrestrial magnetosheath, plasma sheet, radiation belts, solar wind, terrestrial magnetosphere, magnetospheres of Saturn, Mercury, and Uranus as well as other observational data.33,38 Many researchers used kappa distribution to investigate the effect of non-Maxwellian electrons on the propagation features of (non)linear EASs in various plasma models.39,40 We are interested in a laboratory rich in populations of TTEs like Saturn’s magnetosphere (SMS) to study the EASs.
Plasmas in the SMS have diverse characteristics owing to their varying composition observed at different radial distances. The first ever mission on Saturn was Pioneer XI to sample the plasma.41 Depending upon the electron density profile at increasing radial distances, two boundaries can be allocated in the magnetosphere of Saturn. Therefore, it can be categorized in three altitudes (i) below 9Rs (Rs = 60,268km is the radius of Saturn) the inner magnetosphere, (ii) between 9 and 13Rs, the middle magnetosphere, and (iii) above 13Rs, the outer magnetosphere.42 Plasmas in the SMS can come both from its rings and moons such as Enceladus,43 Rhea and Dione,44 Tethys,45 and Titan.46 Electrons having energies from 2eV to 10MeV have been reported in the SMS by combining measurement data on Saturn from three experiments, namely, the plasma science (PLS), low energy charged particle (LECP) instrument, and cosmic ray system (CRS) experiment.47 Cassini mission with two instruments on board CAPS/ELS48 and MIMI/LEMMS,49 being in orbit from 2004 to 2017 around Saturn, produced new data for electron observations and it was shown that the energy spectrum ranges from a few eV to few tens of MeV.42 Different ion species including N+, O+, H+, OH+, and H2O+ have also been observed in several missions with varying temperatures and densities as one moves away from Saturn.18
A Zakharov–Kuznetsov equation (ZKE) can be characterized by the balance between the dispersion arising from charge separation, gyroradius effects, and nonlinearity.33 This equation can typically be used for investigating the propagation of finite but small amplitude acoustic waves in a plasma and many other mediums. Note that the ZKE can only be studied in the context of magnetized plasmas. EASs have been studied by numerous researchers in magnetoplasmas by deriving ZKE.50,51 When it comes to the transfer of energy and momentum, solitons become significant because of the property of holding its identity after interaction. The wave propagation in naturally occurring physical systems calls for the consideration of multi-soliton solutions (MSSs). MSSs are crucial for comprehending nonlinear wave interaction in these systems because the majority of the natural occurrences are inherently nonlinear. A variety of techniques can be utilized including Hirota bilinear method (HBM),52,53 Bäcklund transformation,54 inverse scattering transform,55 and Darboux transformation56 to obtain the MSSs. To obtain the MSSs, the HBM53 is applied to truncate the perturbation expansions at higher orders. In recent years, numerous papers have employed HBM to study interaction of solitons in unmagnetized plasmas,57–59 however, the soliton interaction in magnetized plasmas has received relatively far less attention. In this paper, we have investigated the single soliton and MSSs in a multicomponent magnetized plasma formed from cold inertial electrons, superthermal hot electrons, and stationary ions in the vicinity of the SMS. The paper is structured as follows: The set of model equations for EAWs in a multicomponent magnetoplasma are given in Sec. II. In Sec. III, the MRP is employed by reducing the basic fluid equations of the current plasma model to the two-dimensional (2D)-ZKE. In Sec. IV, HBM is carried out for determining the MSSs, that is, one- and two-soliton solutions of the ZKE. Parametric analysis of the 2D-ZK solitary wave (SW) solutions is presented in Sec. V. The summary of the major findings is given in Sec. VI.
Theoretical model
A homogeneous collision-free magnetoplasma made up of stationary background ions, cold inertial electrons, and hot inertialess superthermal electrons bearing kappa type distribution is considered. An ambient magnetic field (MF) is assumed to be in the x-direction, that is, , where indicates a unit vector in x direction. For simplicity, it is assumed that the temperature of cold electrons Tc → 0, which is relevant under the condition Tcnh ≪ Thnc,26 even though some studies have taken into account the cold electron temperature,58 the following equilibrium condition is fulfilled nio = nho + nco, where nio, nco, and nho denote the unperturbed number densities of stationary positive ions, cold inertial electrons, and hot inertialess superthermal electron, respectively. The dynamics of inertial cold electrons are governed by the following model equations.58
The number density and momentum conservation equations are given as follows
and the model is closed with the following Poisson’s equation
Here, is the hot (cold) electron density scaled by , uc denotes the electron fluid velocity scaled by the EA speed , (KB → Boltzmann constant, Th → temperature of hot electrons, and m → mass of electron) and ϕ is the electrostatic potential scaled by KBTh/e, (e → charge on electron). Also, α = nho/nco, , where is the cold electron plasma frequency, and Ωce = eBo/mc is the electron cyclotron frequency, where c is the light velocity. The time t is scaled by , space variable by , and .
In space plasmas, most particle distributions have been observed to have high energy tail for superthermal electrons.60 The function distribution (FD) to the inertialess superthermal/kappa distributed electrons reads as58
Here, the spectral index κ depicts the degree of superthermality of energetic electrons forming the tail of the distribution which fulfills the condition κ > 3/2, is the hot-electron thermal speed, is the effective thermal speed, and Γ(κ) is the Gamma function. Small values of kappa are associated with high superthermality which essentially means more particles in the superthermal domain. Values of the spectral index κ have a physical significance for 1.5 < κ < ∞. In the κ → ∞ limit, Maxwellian distribution is retrieved and ϑth → ν. Integrating the aforementioned function in equation (4) over the velocity space, the following expression for superthermal electron density is obtained36
The expression in equation (5) can be expanded in Taylor series form for smaller values of the potential to get the form nh = 1 + C1ϕ + C2ϕ2 + ⋯, where C1 and C2 are expansion constants given as
The velocity of the wave driven by inertial cold electrons can be written as , where the subscripts x, y, and z with uc represent the components of the wave velocity along x, y, and z directions. The normalized form of the mentioned model from equations (1)–(5) can be written as follows
and
where α is the density ratio of hot-to-cold electrons and ∇xy = ucx∂x + ucy∂y .
Derivation of the 2D-ZKE
Here, the MRP is applied for reducing equations (7)–(11) to the 2D-ZKE for describing the small amplitude acoustic SWs on the electron time scale in the current plasma model. According to the mentioned method, both time and space coordinates are stretched as61
where Λ determines the normalized PhV of the EAW, and ϵ indicates a small perturbation parameter that describes the amplitude of nonlinearity. The expansion of the physical dependent quantities in terms of ϵ is expressed as follows
To get the linear dispersion relation (LDR), multiscale expansion of the variables given in equation (13) is incorporated in equations (7)–(11) and the collection of the lowest order terms of ϵ, that is, O(ϵ) → ϵ3/2 yields
And from Poisson’s equation, we get
Solving equations (14) and (15) yields the following linear PhV Λ of the EAW
The squared order terms in ϵ for equation (10) give
Collecting the next order terms of ϵ, that is, O(ϵ) → ϵ5/2 from equations (7)–(11), we obtain the following set of equations for second-order perturbed quantities
and
By algebraic manipulation of equations (17)–(20) and utilizing nc1 and uc1 from equation (14), the following 2D-ZKE is obtained
with
and
It has been noticed that linear phase velocity Λ appears in the coefficient of nonlinear term A and dispersion coefficients terms B and C and, therefore, their dependence on densities of the electrons and superthermality is evident, whereas dispersion can vary with magnetic field variation as β appears in both of the dispersion coefficients.
Multi-soliton solution to the 2D-ZKE
Here, the HBM,52 which is a renowned technique to obtain the multi-soliton solution (MSS) of many integrable equations including the 2D-ZKE, is employed. It uses the following transformation equation62,63 to obtain the SW solution of 2D-ZKE
Here, represents the Hirota operators with regard to ξ, η, and τ, respectively. The Hirota derivatives operate in a unique fashion on the product of functions, defined mathematically as53
and expansion of the function g (ξ, η, τ) in terms of ɛ reads
One-soliton solution
According to HBM,52 for exactly one-soliton solution, we employ the exponential function, the series in equation (28) truncates at first order of ɛ and, therefore, we have
Here, ɛ can be visualized as a global phase factor and the infinite series truncates at g1 only if
Incorporating g in equation (24) gives the following one-soliton solution of the ZKE
where ϕo = 15Bk2/A is the soliton’s amplitude and k is the propagation vector in predominant direction of propagation.
Two-soliton solution
The two-soliton solution is procured by assuming the function g1 as the superposition of exponential functions and g2 as the interaction of two exponential functions. The expansion of g in equation (28) truncates at squared order of ɛ for considered values of the perturbed terms of g in the required two-soliton solution
where ζi = kiξ + piη + ωiτ, and i = 1, 2 and a12 is the phase shift or indicates the interaction parameter. Using g in equations (25) and (26) and after geometrical manipulation, we obtain
and
Therefore, the value of g is given by
and the above equation is used in the transformation of equation (24) to arrive at the following two-soliton solution
Results and discussion
We shall use the parameters of Cassini’s data42 within 20Rs (Rs is the radius of Saturn ) in SMS because most plasma sources in the system are reported to orbit within this radius.42 The hot and cold electron densities and the magnetic field values within 5.4Rs − 17.8Rs of Saturn are reported to range from 0.01cm−3 (5.4Rs) − 0.18cm−3 (13.1Rs) and 10.5cm−3 (5.4Rs) − 0.15cm−3 (17.8Rs)18 and 0.1nT − 8000 nT,8 respectively, which have been used to study the characteristics of EASs and their overtaking interaction at different radii from Saturn. It is worth mentioning here that all the electron-acoustic solitons formed in the considered model are rarefactive due to the negative nonlinearity coefficient A given in equation (22) which defines the amplitude of the SW solution.
Plot of the electrostatic (ES) potential of 2D-ZK soliton against variation in density ratio α = 0.4, 0.5, 0.6, and 2 with other parameters as, k = 0.6, κ = 3.5, Bo = 0.0001G, nco = 0.25cm−3, nho = 0.1, 0.125, 0.15, and 0.5.
, the EAS profile is plotted against the variation of density ratio α. We can see that amplitude of the EAS shrinks with increasing α. The soliton’s amplitude varies in the same manner as in an unmagnetized plasma for increasing density ratio (see the paper by Jahangir et al.58). It is, however, noted that the usual existence condition of EAS in an unmagnetized plasma, that is, 0.2 ≤ nco/neo ≤ 0.864 with ne0 = nc0 + nh0, is found to change for the magnetized plasma model. It is evident that the soliton’s amplitude mitigates drastically when the hot electrons’ density becomes greater than the cold electrons’ density, that is, for α > 1. The impact of the MF strength B0 on the EAS profile is demonstrated in Figure 2
Plot of the ES potential of 2D-ZK soliton against variation in ambient magnetic field Bo = 0.0001G, 0.00015G, and 0.0002G with k = 0.6, κ = 3.5, nco = 0.25cm−3, and nho = 0.1cm−3.
. It is seen that the single ZK soliton’s amplitude enhances as the MF gets stronger. This happens because the dispersion coefficient B appears in the amplitude of the single ZK EAS as given in equation (31). As mentioned earlier, the MF strengthens the dispersion and, therefore, the velocity and the amplitude of the EAS increase with increasing Bo.
Plot of the ES potential of 2D-ZK soliton against variation in superthermality κ = 3, 3.5, 4, and 10 (Maxwellian) with k = 0.6, Bo = 0.0001G, nco = 0.25cm−3, and nho = 0.1cm−3.
manifests the effect of the superthermality on the profile of the 2D-ZK EAS. Decreasing the superthermality (i.e., increasing the spectral index κ) would enhance the soliton’s amplitude and width. Reducing the superthermal particles leads us to the Maxwellian distribution. This means that the soliton has maximum amplitude for Maxwellian distribution as shown in Figure 3. This also leads us to the conclusion that the mitigating superthermality causes an increase in the soliton’s speed. We have also explored the profile of the 2D-ZK EAS by using the parameters at different radii in the SMS as delineated in Figure 4
Variation of the ES potential of 2D-ZK soliton with increasing distance from Saturn R = 12Rs, 14Rs, and 17.8Rs. Parameters being used k = 0.95 (fixed) (i) α = 0.12, κ = 3.5, and Bo = 0.00012G at 12Rs (dotted line), (ii) α = 0.67, κ = 6, and Bo = 0.00011G at 14Rs (dashed), and (iii) k = 0.95, α = 0.47, κ = 3.8, and Bo = 0.00008G at 17.8Rs (dot-dashed).
. All the plasma parameters at different radii of the SMS have different values as shown in the table given in Ref. [18]. It is shown that the soliton’s amplitude and width diminish as the radii increase. The electric field vector corresponding to the potential of the soliton solution may be evaluated as
for which the magnitude becomes . The values of the electric field have been calculated at different radii from Saturn and are in the range from 308 μV/m at 17.8Rs to 7.34 mV/m at 12Rs. These values match excellently with the data from Cassini radio and PWS wideband receiver.8,10,11 Since all the parametric variations have been included for the single soliton, therefore, we now move to the numerical analysis of the overtaking interaction of solitons. Figures 5–7
Contour plot of the interaction of the 2D-ZK solitons versus the varying electron density ratio α = 0.4 and 0.6 with k1 = 0.6, k2 = 0.4, Bo = 0.0001G, and κ = 3.5. (a) α = 0.4, nco = 0.25cm−3, and nho = 0.1cm−3, (b) α = 0.6, nco = 0.25cm−3, and nho = 0.15cm−3.
Contour plot of the interaction of the 2D-ZK solitons versus the varying magnetic field (a) Bo = 0.0001G and (b) Bo = 0.00015G. Other fixed parameters being used are k1 = 0.6, k2 = 0.4, α = 0.4, and κ = 3.5.
Contour plot of the interaction of the 2D-ZK solitons versus the varying superthermality (a) κ = 3.5 and (b) κ = 6. Other fixed parameters being used are k1 = 0.6, k2 = 0.4, α = 0.4, and Bo = 0.0001G.
show the parametric analysis by incorporating variation in density ratio, MF, and superthermality of the 2D-ZK soliton interaction given by equation (36). The effect of the variation of electron density ratio on the interaction of EASs in a magnetized plasma is shown by contour plots in Figure 5(a) and 5(b). First of all, note that the interaction point of the two solitons is the same for both the figures (i.e., in both the figures, interaction of the solitons occurs at time t = 0). In Figure 5(a), the two interacting solitons are initially farther apart (for electron density ratio, α = 0.4) by comparison with their counterparts in Figure 5(b) (for α = 0.6) and since the interaction point is the same, this means that increasing the electron density ratio slows down the interaction time. Note that the converse happens in Figure 6(a) and 6(b) when we increase the MF because increasing the MF enhances the magnitude of the soliton which results in the greater distance between the interacting solitons to begin with or the faster interaction time. A comparison of Figure 6(a) and 6(b) shows an expansion of about 144km between the interacting solitons, that is, from 251km to 395km. Figure 7(a) and 7(b) depict the effect of superthermality on soliton interaction. It is noticed that the spatial interaction regime for lower superthermality (i.e., higher spectral index κ) increases from 251km to 287km. This suggests that pumping out the superthermal electrons from the low-phase space density regions of the electron DF energizes the EAS and consequently speeds up the interaction time. Figure 8(a)-8(c)
Contour plot of the interaction of 2D-ZK solitons at disparate radii from Saturn R = 12Rs, 14Rs and 17.8Rs. Parameters being used k1 = 0.6 and k2 = 0.4 as fixed and others are (a) nco = 1cm−3, nho = 0.11cm−3, κ = 3.5, and Bo = 0.00013G at 12Rs, (b) nco = 0.15cm−3, nho = 0.10cm−3, κ = 6, and Bo = 0.00011G at 14Rs, and (c) nco = 0.15cm−3, nho = 0.07cm−3, κ = 3.8, and Bo = 0.00008G at 17.8Rs.
show the interaction of EASs corresponding to the plasma parameters found at different Saturn radii. It is found that as we increase the Saturn radii, the spatial extent between the interacting solitons decreases and the interaction time slows down which essentially illustrates that both the amplitude and width of the interacting solitons decrease as we move away from Saturn.
Conclusion
The formation and interaction of electron-acoustic solitons (EASs) have been examined in a plasma comprising two temperature electrons (inertial cold and superthermal kappa distributed hot) and stationary ions. Two-dimensional Zakharov–Kuznetsov equation (2D-ZKE) has been derived under the small amplitude limit. One- and two-soliton solutions of 2D-ZKE have been obtained using Hirota’s direct method. Response of the single soliton and interaction mechanism for EASs have been studied by varying parameters like electron density ratio, magnetic field (MF) strength, and spectral index, κ, at different radial distances from Saturn. The study of single soliton has revealed that, for increasing hot-to-cold electron density ratio and superthermality, the amplitude and speed of the soliton decrease, whereas enhancing the MF augments the amplitude of the 2D-ZK EAS. The amplitude of the solitons has been found to decrease significantly at longer distances from Saturn. The theoretically obtained electric field values in Saturn’s magnetosphere (SMS) have been found to range from a few hundreds of μV/m to a few tens of mV/m at different Saturn’s radii which concur very well with the data from Cassini radio and plasma wave science wideband receiver. As regards the interaction, EASs have been found to retain their shape after the interaction. It has been found that the increasing values of hot-to-cold electron density ratio and the spectral index, κ, slow down the interaction time and shorten the separation distance between the interacting solitons, whereas the enhancement in the magnetic field speeds up the interaction time and enhances the separation distance between the interacting solitons. We have given the estimates of the separation distance between the interacting solitons for the variation in the plasma parameters for SMS. We have examined the interaction of solitons at different radii from Saturn and it has been deduced that the interaction time and spatial interaction regions vary as one moves away from Saturn. The present study will help to comprehend the formation and interaction of EASs in SMS, however, it may be pointed out that the theoretical framework presented here is general and can be applied to laboratory plasmas.
The future work could include physical effects like collisional force between the particles inside the plasma or nonplanar geometrical effects which make the resulting nonlinear evolution equations nonintegrable.65–67 For solving and analyzing these evolution equations, some approximate techniques such as the family of the homotopy perturbation method (HPM),68,69 the family of Adomian decomposition method (ADM),70 and many other numerical methods71 could be gainfully employed.
Footnotes
Acknowledgments
The authors express their gratitude to Princess Nourah bint Abdulrahman University Researchers Supporting Project number (PNURSP2023R378), Princess Nourah bint Abdulrahman University, Riyadh, Saudi Arabia. One of the authors (W. Masood) acknowledges the support from the Abdus Salam International Centre for Theoretical Physics (AS-ICTP) for his visit under the Regular Associateship Scheme.
Declaration of conflicting interests
The author(s) declared no potential conflicts of interest with respect to the research, authorship, and/or publication of this article.
Funding
The author(s) received no financial support for the research, authorship, and/or publication of this article.
ORCID iD
S A El-Tantawy
Data Availability Statement
Data sharing is not applicable to this article as no new data were created or analyzed in this study.
References
1.
TemerinMCernyKLotkoW, et al.Observations of double layers and solitary waves in the auroral plasma. Phys Rev Lett1982; 48(17): 1175–1179.
2.
ErgunRECarlsonCWMcFaddenJP, et al.Debye-scale plasma structures associated with magnetic-field-aligned electric fields. Phys Rev Lett1998; 81(4): 826–829.
3.
MatsumotoHKojimaHMiyatakeT, et al.Electrostatic solitary waves (ESW) in the magnetotail: BEN wave forms observed by GEOTAIL. Geophys Res Lett1994; 21(25): 2915–2918.
4.
CattellCACrumleyJDombeckJ, et al.Polar observations of solitary waves at the Earth's magnetopause. Geophys Res Lett2002; 29(5): 1–9.
5.
PickettJSChenLJKahlerSW, et al.Isolated electrostatic structures observed throughout the cluster orbit: relationship to magnetic field strength. Ann Geophys2004; 22pp. 2515–2523.
6.
BaleSDKelloggPJLarsenDE, et al.Bipolar electrostatic structures in the shock transition region: evidence of electron phase space holes. Geophys Res Lett1998; 25(15): 2929–2932.
7.
KurthWSGurnettDAPersoonAM, et al.The plasma wave environment of Europa. Planet Space Sci2001; 49(3-4): 63–345.
8.
WilliamsJDChenLJKurthWS, et al.Electrostatic solitary structures observed at Saturn. Geophys Res Lett2006: 33(6).
9.
DuboulozNPotteletteRMalingreM, et al.Generation of broadband electrostatic noise by electron acoustic solitons. Geophys Res Lett1991; 18(2): 155–158.
10.
GurnettDAFrankLALeppingRP. Plasma waves in the distant magnetotail. J Geophys Res1976; 81(34): 6059–6071.
11.
PickettJSKurthWSGurnettDA, et al.Electrostatic solitary waves observed at Saturn by Cassini inside 10 R s and near Enceladus. J Geophys Res: Space Phys2015; 120(8): 6569–6580.
12.
AndereggFDriscollCFDubinDH, et al.Electron acoustic waves in pure ion plasmas. Phys Plasmas2009; 16(5): 055705.
13.
ChowdhurySBiswasSChakrabartiN, et al.Experimental observation of electron-acoustic wave propagation in laboratory plasma. Phys Plasmas2017; 24(6): 062111.
14.
TokarRLGarySP. Electrostatic hiss and the beam driven electron acoustic instability in the dayside polar cusp. Geophys Res Lett1984; 11(12): 1180–1183.
15.
SinghSVLakhinaGS. Generation of electron-acoustic waves in the magnetosphere. Planet Space Sci2001; 49(1): 107–114.
16.
WatanabeKTaniutiT. Electron-acoustic mode in a plasma of two-temperature electrons. J Phys Soc Jpn1977; 43(5): 1819–1820.
17.
BezzeridesBForslundDWLindmanEL. Existence of rarefaction shocks in a laser-plasma corona. Phys Fluids1978; 21(12): 85–2179.
18.
SinghMSainiNSKourakisI. Kinetic Alfvén solitary waves in a plasma with two-temperature superthermal electron populations: the case of Saturn's magnetosphere. Mon Not Roy Astron Soc2019; 486(4): 5504–5518.
19.
FriedBDGouldRW. Longitudinal ion oscillations in a hot plasma. Phys Fluid1961; 4(1): 139–147.
20.
HenryDTrguierJP. Propagation of electronic longitudinal modes in a non-Maxwellian plasma. J Plasma Phys1972; 8(3): 311–319.
21.
StixTH. Waves in plasmas. Berlin, Germany: Springer Science & Business Media, 1992.
22.
BerthomierMPotteletteRMalingreM, et al.Electron-acoustic solitons in an electron-beam plasma system. Phys Plasmas2000; 7(7): 2987–2994.
23.
ShuklaPKMamunAA. Lower hybrid drift wave turbulence and associated electron transport coefficients and coherent structures at the magnetopause boundary layer. J Geophys Res: Space Phys2002; 107(A11).
24.
MaceRLHellbergMA. The Korteweg-de Vries-Zakharov-Kuznetsov equation for electron-acoustic waves. Phys Plasmas2001; 8(6): 2649–2656.
25.
ShuklaPKMamunAAEliassonB. 3D electron-acoustic solitary waves introduced by phase space electron vortices in magnetized space plasmas. Geophys Res Lett2004; 7: 31.
26.
MaceRLBaboolalSBharuthramR, et al.Arbitrary-amplitude electron-acoustic solitons in a two-electron-component plasma. J Plasma Phys1991; 45(3): 323–338.
27.
DevanandhanSSinghSVLakhinaGS. Electron acoustic solitary waves with kappa-distributed electrons. Phys Scripta2011; 84(2): 025507.
28.
VerheestFCattaertTHellbergMA. Compressive and rarefactive electron-acoustic solitons and double layers in space plasmas. Space Sci Rev2005; 121(1): 299–311.
ButiB. Nonlinear electron-acoustic waves in a multi-species plasma. J Plasma Phys1980; 24(1): 169–180. DOI: 10.1017/S0022377800022716
31.
DuboulozNTreumannRAPotteletteR, et al.Turbulence generated by a gas of electron acoustic solitons. J Geophys Res1993; 98(A10): 17–22.
32.
BerthomierMPotteletteRMuschiettiL, et al.Scaling of 3D solitary waves observed by FAST and POLAR. Geophys Res Lett2003; 30(22): 2148.
33.
KhattakMYMasoodWJahangirR, et al.Interaction of ion-acoustic solitons for multi-dimensional Zakharov Kuznetsov equation in Van Allen radiation belts. Chaos, Solit Fractals2022; 161: 112265.
ZouganelisI. Measuring suprathermal electron parameters in space plasmas: implementation of the quasi-thermal noise spectroscopy with kappa distributions using in situ Ulysses/URAP radio measurements in the solar wind. J Geophys Res: Space Phys2008; 113(A8).
36.
El-TantawySAAlshehriHDuraihemZ, et al.Dark soliton collisions and method of lines approach for modeling freak waves in a positron beam plasma having superthermal electrons. Results Phys2020; 19: 103452.
37.
VasyliunasVM. Low-energy electrons on the day side of the magnetosphere. J Geophys Res1968; 73(23): 7519–7523.
38.
ShahKHQureshiMNMasoodW, et al.Electron acoustic nonlinear structures in planetary magnetospheres. Phys Plasmas2018; 25(4): 042303.
39.
El-HanbalyAMEl-ShewyEKElgarayhiA, et al.Propagation of electron acoustic soliton, periodic and shock waves in dissipative plasma with a q -nonextensive electron velocity distribution. Commun Theor Phys2015; 64(5): 529–536.
40.
HassanMRSultanaTISSultanaS. Electron-acoustic solitons in magnetized collisional nonthermal plasmas. IEEE Trans Plasma Sci2021; 49(12): 3749–3758. DOI: 10.1109/TPS.2021.3129920
41.
FrankLABurekBGAckersonKL, et al.Plasmas in saturn’s magnetosphere. J Geophys Res1980; 85(A11): 708–5695.
42.
SchippersPBlancMAndréN, et al.Multi-instrument analysis of electron populations in Saturn’s magnetosphere. J Geophys Res: Space Phys2008; 113(A7).
43.
EspositoLKrimigisSM. Saturn from Cassini-huygens: Berlin, Germany: Springer.
44.
AndersonJDSchubertG. Saturn’s satellite Rhea is a homogeneous mix of rock and ice. Geophys Res Lett2007; 34(2): L02202.
45.
BurchJLGoldsteinJLewisWS, et al.Tethys and Dione as sources of outward-flowing plasma in Saturn’s magnetosphere. Nature2007; 447(7146): 833–835.
46.
BugaevSPNikolaevAGOksEM, et al.The ‘TITAN' ion source. Rev Sci Instrum1994; 65(10): 3119–3125.
47.
MauriceSSittlerECCooperJF, et al.Comprehensive analysis of electron observations at Saturn: voyager 1 and 2. J Geophys Res: Space Phys1996; 101(A7): 15211–15232.
48.
YoungDTBerthelierJJBlancM, et al.Cassini plasma spectrometer investigation. The Cassini-Huygens Mission2004: 114: 1–112.
49.
KrimigisSMMitchellDGHamiltonDC, et al.Magnetosphere imaging instrument (MIMI) on the Cassini mission to Saturn/Titan. The Cassini-Huygens Mission, 2004; 2: 233–329.
50.
ElwakilSAEl-ShewyEKAbdelwahedHG. Solution of the perturbed Zakharov-Kuznetsov (ZK) equation describing electron-acoustic solitary waves in a magnetized plasma. Chin J Phys2011; 49(3): 44–732.
51.
DevanandhanSSinghSVLakhinaGS, et al.Small amplitude electron acoustic solitary waves in a magnetized superthermal plasma. Commun Nonlinear Sci Numer Simul2015; 22(1-3): 22–30.
52.
HirotaR. Exact Solution of the Korteweg-de Vries Equation for Multiple Collisions of Solitons. Phys Rev Lett1971; 27: 1192–1194.
53.
HirotaR. The direct method in soliton theory. Cambridge, UK: Cambridge University Press, 2004.
54.
WadatiM. Wave propagation in nonlinear lattice. I. J Phys Soc Jpn1975; 38(3): 673–680.
55.
AblowitzMJAblowitzMAClarksonPA, et al.Solitons, nonlinear evolution equations and inverse scattering. Cambridge, UK: Cambridge University Press, 1991.
56.
MatveevVBSalleMA. Darboux transformations and solitons. Berlin Heidelberg: Springer-Verlag, 1991.
57.
BatoolNMasoodWSiddiqM, et al.Exact solution of CKP equation and formation and interaction of two solitons in pair ion-electron plasma, Phys Plasmas, 2016; 23: 082306.
58.
JahangirRMasoodW. Interaction of electron acoustic waves in the presence of superthermal electrons in terrestrial magnetosphere. Phys Plasmas2020; 27(4): 042105.
59.
ShohaibMMasoodWJahangirR, et al.Interaction of dust ion acoustic solitons with cubic nonlinearity in a magnetized dusty plasma with(r,q) distributed electrons, Contributions to Plasma Physics2022; 62(3): e202100134.
60.
ChuangSHHauLN. The characteristics of ion acoustic solitons in non-Maxwellian plasmas. Phys Plasmas2009; 16(2): 022901.
61.
WashimiHTaniutiT. Propagation of ion-acoustic solitary waves of small amplitude. Phys Rev Lett1966; 17(19): 996–998.
62.
QuQXTianBLiuWJ, et al.Soliton solutions and interactions of the Zakharov-Kuznetsov equation in the electron-positron-ion plasmas. The European Physical Journal D2011; 61(3): 709–715.
63.
Yousaf KhattakMMasoodWJahangirR, et al.Interaction of ion acoustic solitons for Zakharov Kuznetsov equation in relativistically degenerate quantum magnetoplasmas. Waves Random Complex Media2021, pp. 1–17. DOI: 10.1080/17455030.2021.1968536
64.
GarySPTokarRL. The electron-acoustic mode. Phys Fluids1985; 28(8): 39–41.
65.
El-TantawyBSSAEl-TantawySA. Homotopy perturbation method for modeling electrostatic structures in collisional plasmas. The European Physical Journal Plus2021; 136: 121.
HongBWangJ. Exact solutions for the generalized Atangana-Baleanu-Riemann fractional (3 + 1)-dimensional Kadomtsev-Petviashvili equation. Symmetry Plus2023; 15(3): 1–17.
68.
HeJH. Application of homotopy perturbation method to nonlinear wave equations. Chaos, Solit Fractals2005; 26: 695–700.
69.
HeJH. Recent development of the homotopy perturbation method. Topol Methods Nonlinear Anal2008; 31: 205–209.
70.
El-TantawyNHSAEl-TantawySA. Simulation study on nonlinear structures in nonlinear dispersive media. Chaos2020; 30: 053117.
71.
El-TantawySASalasAHAlharthiMR. On the analytical and numerical solutions of the linear damped nlse for modeling dissipative freak waves and breathers in nonlinear and dispersive mediums: an application to a pair-ion plasma. Frontiers in Physics2021; 9: 580224.