Alfvn waves propagation in homogeneous and dusty astrophysical plasmas - PowerPoint PPT Presentation

1 / 40
About This Presentation
Title:

Alfvn waves propagation in homogeneous and dusty astrophysical plasmas

Description:

A low temperature plasma containing disperse particles of solid material, ... If dust particles are charged, they interact with the waves, and give rise ... – PowerPoint PPT presentation

Number of Views:194
Avg rating:3.0/5.0
Slides: 41
Provided by: Vera172
Category:

less

Transcript and Presenter's Notes

Title: Alfvn waves propagation in homogeneous and dusty astrophysical plasmas


1
Alfvén waves propagation in homogeneous and dusty
astrophysical plasmas
  • M. C. de Juli, D. Falceta-Gonçalves and
  • V. Jatenco-Pereira
  • Instituto de Astronomia, Geofísica e Ciências
    Atmosféricas IAG/USP

2
Index
  • 1. Introduction
  • 2. The dusty plasma physics
  • 2.1 Dusty plasma versus electron-ion plasma
  • 2.2 Electric charge and dust charging process
  • a) Regular variations
  • b) Stochastic variations (charge fluctuations)
  • 3. Astrophysical Applications
  • 3.1 Stellar winds
  • 3.2 Star formation regions
  • 4. Summary

3
1. Introduction
  • Although the universe is 99 plasma, there are
    few astrophysical problems where plasma physics
    solutions have been suggested.
  • Astrophysical plasma coexist with dust particles
    in many situations.
  • These particles are charged either negatively or
    positively depending on their surrounding plasma
    environments.
  • This system of such charged dust, electrons, and
    ions forms a so-called dusty plasma.

4
2. The dusty plasma physics
  • - Dusty plasma
  • It is a fully or partially ionized plasma.
  • A low temperature plasma containing disperse
    particles of solid material, dielectric or
    conductor.
  • - Dusty particles or dust grains
  • These particles are highly massive (md 106
    1018 mp), and highly charged (q 103 104 e).
  • Their electric charge depends of grains size,
    their composition and conditions of surrounding
    plasma.
  • The electric charge signal will be determined
    through competition among different charging
    processes.

5
2.1 Dusty plasma versus electron-ion plasma
  • The dust particles properties determine the
    peculiar behavior of the dusty plasmas in compare
    with an electron-ion plasma.
  • Some of the differences between a dusty plasma
    and an electron-ion plasma, are
  • a) The charge-mass ratio of dust particles is
    very small.
  • So, the dust plasma frequency and the dust
    cyclotron
  • frequency, given respectively by

6
are very smaller than these frequencies for
electrons and ions. In these expressions nd0
is the dust particle density in the equilibrium,
Zd is electric charge number in the dust
particles, md is their mass, B0 is external
magnetic field strength, and c is the light
velocity in the vacuum.
7
  • New modes of propagation in a dusty plasma arise
    from the fact that frequencies associated with
    dust particles are smaller than electrons and
    ions one.
  • Dust modes
  • These modes have ultra-low frequencies (? ? ?d)
    and are associated with the dust particles
    inertia.
  • Charged dust grains have a collective behavior
    and take part in the wave dynamic.
  • Examples
  • dust acoustic waves (DAW) and
  • the electrostatic dust-cyclotron waves (EDCW).

8
b) Electron and ion number in a dusty plasma is
not equal. This fact occurs because the dust
particles are charged. They get their electric
charge by electron and ion capture, electron
emission, and others charging processes. The
new quasi-neutrality condition of the plasma
where is dust charge in
the equilibrium and
for positive and
negative charged dust,
respectively.
9
  • The presence of dust particles can modify the
    propagation of waves modes.
  • - Ion modes
  • Modes of an electron-ion plasma modified via
    quasi-neutrality condition.
  • These modes have low-frequencies ( ? ? ?i ) and
    are associated with the ion inertia.
  • Examples
  • dust-ion-acoustic waves (DIAW) and
  • electrostatic dust-ion-cyclotron waves (EDICW).

10
  • c) The gravitational force has an important role
    in the dust particle dynamics because these
    particles have a large mass.
  • Example modifications in the Jeans criterion of
    instability.
  • d) The electric charge of the dust particle is
    not constant.
  • The electric charge of dust grains is determined
    by electric potential of surrounding plasma
    environments and if a wave modify this potential,
    electric charge of dust grain will be affected.
  • Since the dust charge varies in time, in general,
    it will be necessary to use a new variable, q,
    electric charge of grains, in order to describe
    the plasma fd fd ( r, p,t,q) .

11
  • e) The Debye shielding in a dusty plasma is
    different of one in an electron-ion plasma.
  • In a dusty plasma, the electric charge shielding
    of dust
  • particles, by the others plasma particles, in not
    exponential.
  • This fact occurs due the existence of charging
    processes of dust particles.
  • In these processes electrons and ions flow
    towards the grains, that results in an imperfect
    shielding of the dust particles.

12
  • f) The grain size is not uniform.
  • There is a size distribution modeled, in
    general, by a power law in the dust particle
    radius.
  • That implies in a continuous range of the
    charge-mass ratio of dust particles.
  • Consequently the frequencies associated to dust,
    ?d and ?pd, assume different values in a
    particular band.

13
2.2 Electric charge and dust charging processes
  • A dust particle, in a plasma, is charged by
    different processes. This electric charge in not
    constant.
  • The dust charge variation is an important
    characteristic that differ a dusty plasma from an
    electron-ion plasma.
  • We can divide the charge variation of the dust
    particles in two different cases

14
  • a) Regular variations
  • - The charge variation of dust particles is
    associated with spatial and temporal variations
    in the environment of the plasma parameters, like
    temperature and density of the electrons and
    ions, electric currents, etc.
  • Spatial variation gradients effects of the
    plasma parameters (plasma inhomogeneities)
  • Temporal variations charge variations
    associated with plasma oscillations.
  • - The electric charge q, that a grain has in a
    particular time instant, is determined by equation

where I(r,q,t) is the total charging current the
reach the grain surface.
15
The total charging current that reach the grain
surface is given by
  • - The current Iext is associated to one or more
  • of the following processes
  • photoemission by incidence of ultraviolet
    radiation
  • secondary electron emission by electron or ion
    impact
  • thermionic emission
  • radioactivity, etc.

16
  • - The currents I?(r,q,t) with ? e,i, are
    constituted by electrons and ions from plasma.
  • The dust grains get their electric charge
    through inelastic collisions with these
    particles.
  • Since, electrons have a higher mobility than
    ions, the grains in plasma will acquire a
    negative charge.
  • In general, a summation of the processes
    included in Iext and I?(r,q,t) will determine
    the effective steady-state charge of the dust
    particle.
  • In our work only I?(r,q,t) currents are included
    in the charging process.

17
b) Stochastic variations (Charge fluctuations)
  • In this case, electric charge variation of dust
    particles arise from stochastic nature of
    charging processes and from discrete character of
    electric charge.
  • In equilibrium situation, the dust particle
    captures, in average, an equal electron and ion
    number by time unit, which implies in a constant
    mean charge.
  • However, the capture of an electron by dust
    particle is not immediately following by the
    capture of a positive ion, that results in an
    instantaneous fluctuation of electric charge of
    dust particles.
  • The stochastic nature of charging process of the
    dust particles must only be considered in the
    case of dust particles with a size about one
    nanometer.

18
3. Astrophysical Applications
  • We discuss the effects of the dust particles on
    the propagation and absorption of the Alfvén
    waves in
  • 3.1) Stellar Winds
  • 3.2) Star formation regions

19
3.1 Stellar Winds
  • - Alfvén waves in stellar winds
  • Since the early observations of MHD waves in the
    solar wind various authors have suggested that
    Alfvén waves could be important to transfer
    momentum to the wind.
  • The ? of, B, with the distance of the star, r,
    is smaller than the ? of the gas density, ?, ?
    the Alfvén velocity, increase with distance (vA
    B/(4? ?)1/2).
  • The energy flux, per area unit, transported by
    the wave, ?M, is
  • ?M ? ? vA ? (1/2) ?0 ??v2?
    vA,
  • where ? is the energy density of the waves.
    This energy flux is constant, when there is no
    damping, or decreases due to damping, such that ?
    decreases with r.

20
  • Since the pressure associated with the wave is ?
    to ? then this pressure decreases with r. The
    result is a pressure gradient that accelerates
    the gas.

- Previous damping mechanisms studied
  • The non-linear damping occur when two opposite
    modes interact, generating acoustic waves that
    accelerates the plasma.
  • The resonant damping will occur at the surface
    of the tube, because of the gradient of density
    between the two mediums.
  • Turbulent damping similar to the Kolmogorov
    turbulence.

21
- The no-charged dust grain influence in an
Alfvén wave driven late-type winds
  • P-Cygni profile for CaII K line is observed in
    late-type stars, indicating the presence of
    massive and cool winds.
  • The observed wind terminal velocities are, in
    general, lower than the surface escape velocity (
    ).
  • Authors have proposed several mechanisms for the
    wind acceleration, from radiation pressure to
    (MHD) waves. The most promising involves the
    damping of Alfvén waves.
  • These works have been developed using a pure
    plasma wind, but observations confirms the
    presence of grains in these regions. The
    nucleation region is close to the sonic point of
    the wind.
  • Since the presence of grains is important, the
    effect of grains presence on Alfvén waves damping
    must be evaluated.

22
- The Model
  • The model used is based on that presented by
    Jatenco-Pereira Opher (1989), where an Alfvén
    wave flux is responsible for accelerating the
    wind.
  • Similar to the solar case, the wind has
    non-radial divergence geometry on its base
    becoming radial after a distance, called
    transition radius ( rt ). The cross section of
    the flux tube, showed in figure, is given by
  • The wind equation solved is given by

where u is the wind velocity, ve the escape
velocity, vt the thermal velocity, MA the Mach
number and L the damping length of the wave.
23
  • Havnes, et al. (1989) studied the influence of
    grains in the Alfvén wave damping.
  • They noted that the waves are significantly more
    damped in regions where grains exist.
  • At this work we simulated the grain presence,
    inputing an exponentially decaying damping
    length. The used damping length is given
  • where, A is a damping factor, and r1 is the grain
    formation region.

24
- The grain presence region
  • The damping by grains must be introduced only in
    the region where grains can exist. Observations
    can not show us where the nucleation occurs, but
    theoretical models can (Gail Sedlmayr (1984,
    1986, 1987).

The figure shows the nucleation region, as
function of the effective surface temperature and
the mass loss rate for two grain type. For cool
supergiant (T?2000K) we may use
ro lt r lt 2ro.
25
- Results
We present the results of a simulation of grains
presence including an non-isothermal profile
applied to a K5 supergiant star, of M16M?,
ro400R?, S5 and ?o3.36x106 erg/s/cm2.
The wind velocity profile where the dotted line
is the Jatenco-Pereira and Opher pure plasma and
isothermal wind, and the filled line is the
presented model. The grain formation region is
showed also.
At the grain formation region, the sudden damp of
the waves causes the rapid deposition of
momentum, accelerating the wind to upper
velocities when compared to JPO model.
26
- Conclusions
In this work we present a model of mass loss in
late-type stars, using a flux of Alfvén waves as
an accelerating mechanism. Grains presence are
simulated.
The model was applied to an K5 star, showing that
the sudden damping of the waves causes a local
acceleration of the wind. The results were
compared to Jatenco-Pereira and Opher (1989)
model.
The comparison shows important differences
between the models. Our model results in upper
velocities. The differences are not despicable,
and more studies in the future could improve this
model.
Our model was used to simulate the Betelgeuse
(?Ori) wind also. The results are in agreement
with recent observations of this red supergiant.
27
  • - Present work (variable charge of the dust
    particles)
  • At the moment, we are considering the Alfvén in a
    magnetized dusty plasma with variable charge on
    the dust particles, in the context of the kinetic
    theory.
  • In a paper in preparation, we consider the case
    of propagation of the waves exactly parallel to
    the external magnetic field and Maxwellian
    distributions for the electrons and ions in the
    equilibrium.
  • We show that the presence of dust particles with
    variable charge in the plasma produces an
    additional damping of the Alfvén waves.

28
3.2 Alfvén wave pressure against dusty molecular
cloud collapse (charged dust)
  • The Interstellar Medium is plenty of giant
    structures, cold and dense, which main
    constituent is quasi-neutral matter as atoms,
    molecules and dust particles.
  • This structures are called as Molecular Clouds.
  • They are known as the main star formation
    regions.
  • Dwarf Molecular Clouds (DMCs) are 5 pc lenght
    structures, and have masses of hundreds of solar
    masses.
  • Observations indicates that most DMCs can live
    more than 108 years in equilibrium.
  • However they are cold, T 10 20 K, and the
    thermal pressure could not support the
    gravitational collapse.

29
  • The Jeans mass
  • for typical parameters of DMCs is 3 solar
    masses.
  • Also, the free-fall time would be
  • which gives 106 years for the typical
    parameters, much lower than the 108 DMC lifetime.

30
- Stability Mechanisms
  • DMCs present also magnetic fields of few
    µGauss.
  • Magnetic field pressure can support
    gravitational collapse, however only in the
    perpendicular direction of its field lines.
  • For the parallel direction of the field there is
    no explanation yet. Some of the main cadidates
    for the support are
  • rotation, internal turbulence and MHD waves.
  • Among the MHD waves, Alfvén waves propagate
    through the magnetic field lines in the parallel
    direction.
  • Some authors advice the need for low damping
    mechanisms acting on the Alfvén wave flux, with
    damping lenghts greater than 1pc, to guarantee
    the stability in such DMCs lenghtscales.

31
- Alfvén wave damping
  • There are several damping mechanisms in the
    literature. In particular, ion-neutral
    collisional damping and the non-linear damping
    are the most used in such regions.
  • Typical parameters, applied to the above
    mechanisms, confirm the low damping of Alfvén
    waves in DMCs.
  • However, previous authors did not considered
    that DMCs are, actually, a Dusty Magnetized
    Plasma.
  • In this case, dust particles can play an
    important role on the Alfvén waves dispersion
    relation.

32
- The role of dust (size distribution)
Observations indicate that the distribution of
dust sizes in space is with p 3 4,
considering different dust compositions. For ex,
for graphite dust particles the radius range of
a 10-7 10-4 cm is obtained. These dust
particles are, in general, charged with Zd 101
103 e-. If dust particles are charged, they
interact with the waves, and give rise to a
dust cyclotron resonance damping. The dispersion
relation for a dust size distribution is
calculated by Cramer, N., Verheest, F.
Vladimirov, S. (2002)
where
33
The imaginary part of k gives the damping lenght
of the wave. am is the ratio of
maximum and minimum dust radii. For am 1.3
the resonance band occurs for 0.59 ??/?dmax? 1.
In the interstellar medium am 102 and we
expect resonance band can be even larger
affecting almost all spectrum of low frequency.
(a) The real part of the wave number for am 1.1
(solid line) and am 1.3 (dotted line). (b) The
imaginary part of the wave number for am 1.1
(solid line) and am 1.3 (dotted line).
34
- Cloud stability
  • The model used is described below
  • In this scheme, we show the propagation direction
    of the Alfvén waves and the
  • way as they increase the cloud
    support against gravity.
  • The temporal mean of the momentum equation for a
    cloud in mechanical
  • equilibrium can be written by

35
  • Using a WKB aproximation, the wave energy density
    gradient will be given
  • by
  • , where
    is the wave damping lenght.
  • The Poisson equation determines the gravity by
  • Using also the wave frequency spectrum
  • ,
  • and defining
  • as the ratio of the wave density energy and
    the gas energy density,

36

The wave power spectrum, damped by dust-cyclotron
resonance, for different cloud locations z. We
note that the frequency band is almost completely
damped up to z 0.01 pc. These waves cannot
reach the boundareis of DMCs ( 1 - 10 pc).
Density profile as a function of distance for
different values of the parameter ?. Dotted line
represents equilibrium without Alfvenic support,
and the dashed, dot-dashed and solid lines
represent the cases of ? 0.05, ? 0.15 and ?
0.25, respectively. The sudden damping of the
wave flux results in compact and denser cloud
cores already observed in DMCs.
37
- Conclusions
Typical dwarf molecular cloud parameters as nH2
104 cm-3 and T 20 K lead to the MJ of
3 solar masses, which is ?? Mcloud (Mcloud
100 M?). Considering B 10 µGauss, the cloud
stability may be reached, however only on
the perpendicular direction. Alfvén waves
propagating along B could provide an extra
pressure in the parallel direction. On the
other hand, DMCs presents high amounts of charged
dust particles, which interact with B and
provide a dust cyclotron damping mechanism
for the waves. Using this damping mechanism and
a particle size distribution, just like the
observed in the ISM, we show that the flux is
dissipated suddenly in a region ?? 1 pc much
smaller than the cloud size of 1 10 pc. The
sudden damping of the wave flux results in
compact and denser cloud cores already
observed in DMCs, which could be explained.
38
Summary
  • Most of the material in the universe is in the
    plasma state and it coexists with dust particles
    in many situations.
  • Dust grains become charged if they are immersed
    in a plasma.
  • The system composed of charged dusts, electrons
    and ions forms a so called dusty plasma.
  • We have presented the results of some works in
    which we consider the presence of dust grains in
    the plasma and their effects in the propagation
    and damping of Alfvén waves.
  • We have concentrated in two astrophysical
    problems

39
  • - 1) Stellar winds
  • In the literature, several acceleration
    mechanisms of winds have been proposed. Among
    them, one of the most promising involves the
    damping of a flux of Alfvén waves.
  • Models without dust
  • Direct momentum transference from waves to
    plasma particles (electrons and ions).
  • Models with no charged dust
  • Damping associated with the collision of
    electrons and ions with neutral particles (dust
    grains)
  • Models with charged dust (variable charge of
    dust particles)
  • The presence of dust particles with variable
    charge in the plasma produces an additional
    damping of the Alfvén waves. A damping associated
    with the charge variation of the dust particles.

40
  • - 2) Star formation regions (size distribution of
    charged dust particles)
  • When wave damping is not considered, the wave
    flux can support the cloud against gravity,
    preventing its collapse, as also pointed out by
    Martin et al. (1997).
  • We have presented a model in which a flux of
    waves propagating in a dwarf molecular cloud is
    damped due to resonant interaction with dust
    charged particles.
  • Taking into account this wave damping, discussed
    by Cramer et al. (2002), the flux is dissipated
    suddenly (in a region ltlt 1pc), leading to the
    formation of a compact and dense core.
  • In this case, the waves could not reach the
    outer layers of the cloud, and if this is so,
    they could not be used to explain the size of
    these objects, although they could still be used
    to inhibit star formation.
Write a Comment
User Comments (0)
About PowerShow.com