structure and stability of phase transition layers in the...

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Structure and Stability of Phase Transition Layers in the Interstellar Medium Tsuyoshi Inoue , Shu-ichiro Inutsuka & Hiroshi Koyama 1 1 2 Kyoto Univ. Kobe Univ. 1 2 Small Ionized and Neutral Structures in the Diffuse Interstellar Medium May 21-24, 2006 AOC, Socorro astro-ph/0604564 submitted to ApJ This work is supported by the Grant-in-Aid for the 21st Century COE "Center for Diversity and Universality in Physics" from the Ministry of Education, Culture, Sports, Science and Technology (MEXT) of Japan.

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Structure and Stability of Phase TransitionLayers in the Interstellar Medium

Tsuyoshi Inoue,Shu-ichiro Inutsuka & Hiroshi Koyama

1

1 2

Kyoto Univ. Kobe Univ.1 2

Small Ionized and Neutral Structures inthe Diffuse Interstellar Medium

May 21-24, 2006

AOC, Socorro

astro-ph/0604564 submitted to ApJ

This work is supported by the Grant-in-Aid for the 21st Century COE"Center for Diversity and Universality in Physics" from the Ministry ofEducation, Culture, Sports, Science and Technology (MEXT) of Japan.

Introduction Low & Middle Temperature Parts of the ISM

Warm Neutral Medium ( WNM ) : Cold Neutral Medium ( CNM ) :

Radiative equilibrium state of the ISM

Heating : external UV field, X-rays, and CR’sCooling : line-emissions

n

P

CNMWNM

CNM and WNM can coexist in pressure equilibrium

Studies on Dynamics of 2-phase Medium

Recently, many authorsare studying dynamics ofthe two-phase medium.

Koyama & Inutsuka 2002

Audit & Hennebelle 2005

Heitsch et al. 2005

Vazquez-Semadeni et al. 2006

Inutsuka, Koyama & Inoue, 2005, AIP conf. Proc.

Generation of clouds by collidingtwo flows via thermal instability

Motivation

Turbulent motion of the cloudlets Instability of the interface??

Calculation of 2-phase medium from static initial conditionwithout external forcing. Koyama & Inutsuka 2006

We study the phase transition layers (yellowregion).

Typical size of cloudlets ~ Field length Self-sustained motions !

3 Types of Steady Transition Layer

If P=Ps Static (or saturation) transition layer

: Corresponding to the Maxwell’s arearule in thermodynamics.

If P>Ps : Condensation layer (Steady flow from WNM to CNM).

If P<Ps : Evaporation layer (Steady flow from CNM to WNM).

Zel’dovich & Pikel’ner ’69, Penston & Brown ’70

WNM

CNMx

T Transition layer

n

P

saturation

Saturation

In the case of plane parallel geometry

Net cooling function

n

PCondensation

If P>Ps : Condensation layer (Steady flow from WNM to CNM).

If P<Ps : Evaporation layer (Steady flow from CNM to WNM).

WNM

CNMx

T Transition layer

flow

Condensation

3 Types of Steady Transition Layer

If P=Ps Static (or saturation) transition layer

: Corresponding to the Maxwell’s arearule in thermodynamics.

Zel’dovich & Pikel’ner ’69, Penston & Brown ’70 In the case of plane parallel geometry

Net cooling function

n

P

Evaporation

If P>Ps : Condensation layer (Steady flow from WNM to CNM).

If P<Ps : Evaporation layer (Steady flow from CNM to WNM).

WNM

CNMx

T Transition layer

flow

Evaporation

3 Types of Steady Transition Layer

If P=Ps Static (or saturation) transition layer

: Corresponding to the Maxwell’s arearule in thermodynamics.

Zel’dovich & Pikel’ner ’69, Penston & Brown ’70 In the case of plane parallel geometry

Net cooling function

Structure of the Transition Layers Steady 1D fluid eqs with thermal conduction & cooling function

Boundary conditions :

Thickness of the transitionlayers are essentially determinedby the Field length in the WNM.

BCs are satisfied, if j( ) is a eigenvalue.

P

n

T

x [pc]

2nd order ODE with respect to T

Stability Analysis of Transition Layers

x

y transition layerWNMCNM

x

y transition layerWNMCNM

Long wavelengthanalysis: neglect thicknessof layers

Short wavelengthanalysis: isobaricperturbation

We adopt 2 approaches.

flowflow

Long wavelength analysis long wavelength approx.

perturbation scale thickness of the layers

x

y transition layerWNMCNM

Dispersion relations of the layers can be obtainedanalytically by matching the perturbation of CNM andWNM at the discontinuity using conservation laws.

for evaporation

for condensation

Amplitude of the front perturbation :

Evaporation layer is unstable

Discontinuous layer

Mechanism of the Instability

x

yWNMCNM

Evaporation

Convergence of flow increasespressure and it pushes the layer.

Fluxconservation Momentum conservation

Growth rate of the instabilityis proportional to

We cannot estimate the mostunstable scale and its growth rate

Similar instability is known in thecombustion front (Darrieus-Landau instability)

CNMWNM

FuelExhaust

This similarity is also pointed out by Aranson et al.1995 in the context of thermally bistable plasma.

transition layer

Mechanism of the Instability

WNMCNM

Condensation

Convergence of flow increasespressure and it pushes the layer.

Fluxconservation Momentum conservation y

x

Growth rate of the instabilityis proportional to

We cannot estimate the mostunstable scale and its growth rate

Similar instability is known in thecombustion front (Darrieus-Landau instability)

CNMWNM

FuelExhaust

This similarity is also pointed out by Aranson et al.1995 in the context of thermally bistable plasma.

transition layer

Short wavelength analysis

Short wavelength approx.

Scale of perturbation Acoustic scale

For such a small scale modes, pressure balance sets in rapidly.

To study the small scale behavior of the instability, we analyzelinear stability of the continuous solution of the transition layer.

Instability of the evaporationlayer is stabilized roughly atthe scale of thickness of thelayer (0.1 pc) owing to thethermal conduction.

Isobaric approx.

Dispersion relation can be obtainedby solving the eigenvalue problem.

Isobaric perturbed energy equation withthermal conduction + cooling functionBoundary condition : perturbations vanish atinfinity.

the instability is stabilized at the scale of the thickness of thetransition layer Field length in the WNM 0.1 pc (see blue line)

Summary We show that evaporation layer is unstable,whereas condensation layer seems to be stable. From long wavelength analysis (discontinuous layer approx.) Growth rate is proportional to (see red line)

From short wavelength analysis (isobaric approx.)

Discussion

Growth timescale

We propose that this instability is one of the mechanismsof self-sustained motions found in 2-phase medium.

We can expect growth rate withoutapproximation as the green line.

The most unstable scale is roughlytwice the thickness of the layer

Sufficient to drive 2-phase turbulence

Flow Velocity of the Steady FrontFlow velocity vs. pressure

Our Choice of Cooling Function Net cooling function

: Photo electric heating by dust grains

: Ly-alpha cooling

: C+ fine structure cooling