Radiative%20Transfer%20for%20Simulations%20of%20Stellar%20Envelope%20Convection - PowerPoint PPT Presentation

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Radiative%20Transfer%20for%20Simulations%20of%20Stellar%20Envelope%20Convection

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Energy: dE /dt = - uE (T - Pgas) u ? qrad. Regular horizontal and ... Monochrome, ODF, N? =2750. Multi-group, Nbin=4. Horizontal and temporal averages ... – PowerPoint PPT presentation

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Title: Radiative%20Transfer%20for%20Simulations%20of%20Stellar%20Envelope%20Convection


1
Radiative Transfer for Simulations of
StellarEnvelope Convection
  • By
  • Regner Trampedach
  • 8/19/04

2
Hydro-dynamics
  • Solve Euler equations
  • Conservation of
  • Mass d? /dt -u ? ? -? ? u
  • Momentum ? du /dt -? u ? u ? (T - Pgas) ?
    g
  • Energy dE /dt -? uE (T - Pgas)?
    u ? qrad
  • Regular horizontal and optimized vertical grid

3
(No Transcript)
4
Vertical Temperature-cut of ? -Boo
5
Applications of the Simulations
  • Improving stellar structure models
  • T-t -relations atmospheric boundary cond.
  • Calibration of the mixing-length parameter, a
  • Abundance analysis
  • Agreement between FeI, FeII and meteoritic
  • Lower C, N and O abundances at odds with
    helioseismology
  • Synthetic spectra/line-profiles
  • No free parameters, e.g., micro-/macro-turb.

6
Input Physics
  • Equation of State (EOS)
  • Pressure for hydro-static support
  • Response to temperature-/density-changes
  • Opacity ff bf bb
  • radiative transfer gt
  • radiative heating qrad,? 4p ? ? (J?-S? )

7
FeI Opacity According to LAOL
  • Hübner et. Al (1977)
  • Semi-hydrogenic wave-functions
  • Hundreds of lines...

8
FeI Opacity According to OP
  • Seaton et. Al (1994)
  • Intermediate S-L coupling
  • Hundreds of millions of lines!

9
bf-Opacity Before OP/OPAL
  • From Peach (1962)

10
Confronting Experiment
  • From Nahar, S. N., 2003, Phys. Rev. A (submitted)

11
Radiative Transfer
  • Determines heating/cooling gt structure
  • Determines emergent flux/intensity gt link to
    observations
  • Transfer Eq. d I? /dt ? (I? S? ) solved
    for more than 105 wavelengths
  • Not possible in convection simulations
  • Yet...

12
Statistical Methods
  • Have used opacity binning (Nordlund 1982) a.k.a.
    the multi-group method
  • Works well, and has correct asymptotic behaviour
    in optical thick/thin cases
  • Employs a number of somewhat arbitrary bridging
    functions and extrapolations
  • Does not converge for N bin? 8

13
Selective/Sparse Opacity Sampling
14
S O S
  • Carefully select NSOS wavelengths
  • covering the whole energy spectrum
  • that reproduce the full solution, e.g., heating
    qrad, flux Frad, and J and K.
  • Perform radiative transfer on those ?
  • Paves the way for including velocity-effects
  • Spans the convective fluctuations better than the
    opacity binning method
  • Converges for NSOS? 8

15
Multi-group vs. SOS
  • SOS, N? 50
  • Monochrome, ODF, N? 2750
  • Multi-group, Nbin4

16
Horizontal and temporal averages
  • 50 bins same as 4 bins!
  • Too little cooling in conv/rad trans.
  • Too little heating in lower photosph.
  • No action at or above T-min

17
- and their differences
  • ___ straight average
  • - - - RMS average
  • Systematic diffs for multi-group
  • gt4 times larger RMS differences

18
Summary
  • Developed new radiative transfer scheme
  • Performs better than multi-group method
  • Much closer to monochromatic solution
  • More stable against convective fluctuations
  • Reproduce first three moments of I(µ )
  • Convergent for NSOS? 8

19
Prospects for the Future
  • Calculate new and improved EOS-tables
  • Use it as basis for new opacity calculation using
    the newest cross-section data
  • Implement the SOS radiative transfer scheme in
    the convection simulations
  • Build a grid of convection models, using the new
    EOS, opacities and SOS scheme
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