Convection Simulation of an A-star - PowerPoint PPT Presentation

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Convection Simulation of an A-star

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No magnetic fields (Scaled) Solar abundances. Uniform ... No radiative levitation of individual species. LTE EOS and radiation. A few collaborators ... – PowerPoint PPT presentation

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Title: Convection Simulation of an A-star


1
Convection Simulation of an A-star
  • By
  • Regner Trampedach
  • Mt. Stromlo Observatory, Australian National
    University
  • 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
Radiation Dynamics
  • Simplified by only needing forward solution
  • More expensive by factor NxNyNf Nt
  • Binning the rad. transfer according to opacity gt
    speed-up by Nbin /N? , Nbin 4
  • Binning is calibrated against 1D average sim.
  • About to change to Sparse/Selective OS
  • More stable accurate and converges

4
Assumptions
  • No rotation
  • No magnetic fields
  • (Scaled) Solar abundances
  • Uniform gravitational field
  • No diffusion
  • No radiative levitation of individual species
  • LTE EOS and radiation

5
A few collaborators
  • Convection-code Robert F. Stein, Michigan State
    University
  • Ã…ke
    Nordlund, Copenhagen Observatory
  • Equation of State Werner Däppen, University of
    Southern California
  • Radiative Transfer Martin Asplund, Mt. Stromlo
    Observatory
  • Asteroseismology Jørgen Christensen-Dalsgaard,
    Aarhus Univ.
  • Dali
    Georgobiani, Stanford
  • and many more...

6
The Dynamic Sun
7
Vertical Temperature cut of? -Boo
8
Solar Line Calculation
  • 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.
  • Agree both in shape (bisectors) and shifts

9
The A-star simulation
  • 7300 K, logg4.3, Fe/H 0.0
  • 10010082 grid-points
  • 11.4511.4513.10 Mm
  • About 5 pressure scale-heights
  • 5.6 and 6.4 decades of pressure and density
  • 19 mins. with 50 s resolution
  • p-modes with ? 12 mins., A1.5 km/s

10
3D-1D(a 1)
  • gt? -inversion
  • gt T-gradient
  • More structure in photosphere
  • lt u and Pturb
  • Seperate conv. Zones
  • Diff. internal structure

11
3D-1D(a 2)
  • Larger? ,T
  • gt T-gradient
  • More structure in photosphere
  • gt Pturb-peak
  • No overshoot
  • Very Different internal struct.

12
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13
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14
T-inversion
  • Up to 10 000 K
  • Factor 10 density invers.
  • Related to ionization?

15
Summary
  • Have changed lower boundary to accomodate
    radiative zone
  • Have included optically thick radiative transfer
  • Have started running a simulation on the border
    between A and F

16
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 an improved radiative transfer scheme
    in the convection simulations
  • Build a grid of convection models, using the new
    EOS, opacities and rad. Transfer
  • Expanding coverage in (Teff, g, Z )
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