The Interaction Between Infall and Winds in Young Stellar Objects

Guy Delamarter, Adam Frank, and Lee Hartmann

Submitted to ApJ

Abstract

We present simulations of the interaction between a collapsing sheet density distribution with a central spherically symmetric wind as might be found around a young stellar object (YSO).  We investigate how the morphology and velocity structure of the resulting outflows change as we vary the ratio (denoted f') of the inflow mass flux to the wind mass flux.  In addition to elucidating the behavior around YSOs of different wind strengths, this serves in part as a preliminary survey of the effect of time dependent winds from a single object on the resulting outflow. 

We find that relatively strong winds can carve out wide, conical outflow cavities and that relatively weak winds can be strongly collimated into jet-like structures.  If the winds become weak enough, they can be cut off entirely by the infalling environment. 
 
Learn more about the collapsing sheet environment used in these simulations. 
 

Comparative Density
Comparison between outflows at times of similar axial extent. The density of the f'=10,20,30,40, and 50 (left to right - strong wind to weak wind) cases are shown at their full heights at 100, 200, 220, 240, and 220 years, respectively.  Note the increased focusing of the bubbles as the wind becomes weaker.
 
 Compare these shapes to those in some observational images of outflows. 
 
 
f'=10 @ 180yr f'=30 @ 220yr
f'=50 @ 220 yr.
f '=10 (180 y)
f' =30 (220 y)
f' =50 (220y)
Density, pressure, temperature, velocity snapshots for three representative simulations.
 
 
 
f' =10
f' =50
Density and velocity animations for two cases.  Frames are taken 20 years apart.  The color scale corresponds to that used in the still frames shown earlier.
 
 
 
Mass vs. velocity curves over time for each simulation.  The left-hand shallow portion has a power law dependence of about -1.5, while the steeper portion has a dependence of -10 or steeper.  Note, however, the bottom f'=50 case where, as time passes, the steeper portion flattens.  This is likely due to the stong focusing in this case (see density snapshots above) accelerating more mass at high velocities than in the other cases.
Compare these plots to those made from observational data 
 
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 email: delamart@pas.rochester.edu