The Wolfire/Kaufman models are primarily based on the work of
Tielens & Hollenbach 1985;
Wolfire et al. 1990;
Hollenbach et al. 1991;
Kaufman et al. 1999;
and Kaufman et al. 2006.
For a given set of gas phase elemental abundances and grain properties,
each model is described by a constant H nucleus number density,
The ratio plots are used to determine the beam averaged values of
It is important
to correct for the different beam area filling factors for various species.
For example, diffuse [C II] emission may fill the observing beam whereas
[O I] emission may arise from a smaller, high density and high temperature
region. In such a case, it would not be appropriate to take the ratio
of observed fluxes for fitting. Instead the ratio of intensities
should be used or the ratio of fluxes corrected for the separate emitting
solid angles. Note also that the ([C II] + [O I])/
These model data start with the 2006 PDR model code and add improved physics and chemistry. Critical updates include those discussed in
Neufeld & Wolfire 2016, plus photo rates from
Heays et al. 2017, oxygen chemistry rates from
Kovalenko et al. 2018 and
Tran et al. 2018,
and carbon chemistry rates from
Dagdigian 2019. We have also implemented new collisional
excitation rates for [O I] from
Lique et al. 2018 (and Lique private
communication) and have included 13C chemistry along with the
emitted line intensities for [13C II] and 13CO. In Box 1, we show the currently available spectral lines and those we expect to deploy later in the project. In addition, we will compute ModelSets for a full range of metallicity
In pdrtpy, these are referred to as the wk2020 ModelSet.
These models
are identical to those available in the "classic" web-based PDR Toolbox. They have metallicity
In pdrtpy, these are referred to as the wk2006 ModelSet.
Our
2006 models
use the standard parameters from Kaufman et al. 1999. Changes for the
2020 models are listed below.
The formation rate of H2 goes as
Parameter | Symbol | Value |
---|---|---|
Turbulent Doppler velocity | 1.5 km s-1 | |
Carbon abundance | ||
Oxygen abundance | ||
Silicon abundance | ||
Sulfur abundance | ||
Iron abundance | ||
Magnesium abundance | ||
Dust abundance relative to diffuse ISM | 1 | |
FUV dust absorption/visual extinction | 1.8 | |
Dust visual extinction per H | ||
Formation rate of H2 on dust | ||
PAH abundance | ||
Cloud H density | ||
Incident UV flux |
Parameter | Symbol | Value |
---|---|---|
Carbon abundance | ||
Oxygen abundance | ||
Dust visual extinction per H | ||
Formation rate of H2 on dust | ||
PAH abundance |
The KOSMA-tau models This KOSMA-tau code was developed from an earlier PDR code, written by A. Sternberg from Tel Aviv University in Israel (Sternberg & Dalgarno 1989; Sternberg & Dalgarno 1995). His original code uses a plane-parallel geometry and was updated to employ spherical geometry (Gierens, Stutzki and Winnewisser 1992; Köster et al. 1994; Störzer, Stutzki and Sternberg 1996; Zielinsky, Stutzki & Störzer 2000).
The KOSMA-tau models come in "clumpy" and "non-clumpy" variety, with 3.1 ≤RV ≤ 5.5 depending on the model. For the non-clumpy models, the mass parameter is the mass of the spherical clump. The density profile and the mass determine the clump radius and the total AV to the clump center. In the clumpy models there are three mass parameters. The main mass parameter in the clumpy models is the total (ensemble) mass of all clumps which are distributed according to a power law with the mass range [Mlow, Mup]. Typically the upper and lower masses are fixed and the total mass is varied.
For more information about these models, see the KOSMA-tau website.
This feature is not fully implemented yet, but it can be used with a little extra work on your part. To be imported in to PDRT, model files must be in FITS format and must follow our given standards. If you would like to try and use alternate models, please contact Marc Pound.