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Using Fe II Emission Lines to Determine Dust Properties in Jets

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In cool post-shock regions, iron atoms may condense into dust, depleting [Fe II] ... Hartigan, P., Raymond, J., Pierson, R. 2004, ApJ, 614, L69-71 ... – PowerPoint PPT presentation

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Title: Using Fe II Emission Lines to Determine Dust Properties in Jets


1
Using Fe II Emission Lines to Determine Dust
Properties in Jets
  • Adam Ginsburg
  • Advisor Pat Hartigan

2
Outline
  • Background on Herbig Haro objects, dust, and
    forbidden line emission
  • Data extraction, calibration, and measurement
  • Results and early analysis
  • Shock model
  • Javascript code

3
Herbig Haro objects
  • Form from T-Tauri stars, young solar systems
  • Accretion disk consists of dust and gas and is
    presumed to be the source of the HH jets
  • Jets are ejected from the stars poles (or
    mag-netic poles) and impact the sur-rounding
    medium, causing a shock to form
  • Knots in the jet are emitted at variable
    velocities, causing many smaller shocks to form

4
Why is dust important?
  • A recent article from Harvards CfA showed
    pebbles in the protoplanetary disk around TW
    Hydrae
  • Dust forms into larger bodies (pebbles) which
    then form into planets
  • By studying dust in other systems, we can better
    understand the formation of our own

5
Dust Formation and Destruction
  • In cool post-shock regions, iron atoms may
    condense into dust, depleting Fe II emission
    relative to S II emission
  • Dust particles could be broken apart in the
    shock, splitting (or sputtering) back into
    ionizable gas particles, enhancing Fe II
    relative to S II
  • If we witness neither formation nor destruction,
    we could determine abundances, which could then
    be compared between star forming regions

6
Diagram vs. Image
7
Dust Detection
  • Fe II l8617 and S II ll(6717 6731) are good
    comparison lines
  • source upper state has similar energy
  • Therefore have similar temperature dependence
  • similar ionization energies
  • difficult to doubly ionize
  • Dust particles will not emit significantly in
    optical wavelengths, and do not show emission
    lines

8
The Data
  • Reduced spectra using standard IRAF tasks
  • Fluxes are measured relative to H-alpha
  • Some lines are too small to measure if they are
    present at all
  • Measurement uncertainty /- 5 for good S/N
  • Because of multiple steps of background
    subtraction, the continuum (zero flux) level was
    the dominant source of measurement error
  • Reddening correction C.34 derived from Balmer
    decrement (Ha/Hb 3)

9
Standard Star Calibration
  • Clouds were a problem for some nights
  • Standard star sensitivity functions had the right
    shape but wrong level
  • Matched levels to give correct line ratios

10
Tables
11
(No Transcript)
12
The Shock Code
13
Knot interaction in the jets
14
Javascript Model Analyzer
  • Accepts input of tab separated ratios to H-alpha
  • Can reddening correct line ratios
  • Once we have multiple data sets, will be able to
    show best fits in different star forming regions

15
HH34 Aperture Selection
16
Analysis
Calculated best-fit models without (left) and
with (right) iron lines included for the E shock.
With iron, the fit is about the same While
reddening correction improved the fit, it did not
change the result
17
Shock Velocity
18
Fe II/S II and Data
19
Conclusion
  • The null hypothesis, i.e. that there is no change
    in dust, is probably correct
  • Still need to work out some kinks in chi-squared
    fitting program
  • Data is in good agreement with Hartigan et al.
    1994, which gives shock speed 25-33 km/s and
    partial ionization of 1

20
Future Work
  • Same work for HH 111
  • Expand the database of shock models
  • Since there is no change in the dust, we can
    calculate abundances using a modification to the
    best fit code and the larger shock model database
  • Publish

21
HH111 Aperture Selection
22
References
  • Hartigan, P., Raymond, J., Pierson, R. 2004, ApJ,
    614, L69-71
  • Hartigan, P., Morse, J., Tumlinson, J., Raymond,
    J., Heathcote, S. 1999, ApJ, 512, 901-915
  • Brown, Korgsen, Evenson 1998, ApJ, 509927-930
  • Morse et al., 1993, AJ vol 106 no 3 p 1139
  • Hartigan, P., Morse, J., Raymond, J., 1994, ApJ,
    436, 125-143
  • Wilner et al., 2005, ApJ, 626, L109-112
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