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The Structure of Winds in AGB Stars
Moshe Elitzur (Kentucky)
Željko Ivezić (Princeton)
Dejan Vinković (Kentucky)
MNRAS 327, 403 (2001)
Once the sonic point is crossed…
• Radiation pressure decouples the outflow from the wind origin
• Same grains same wind structure however grains were formed!
gravityP
~dragP
~P radrad
wy
dyPQ
22
21
Wind Problem
• Radiation pressure
• Gas drag
• Gravity
tcosA2
1)y()y(
y
P
dy
dw2
22
wln)(
)w()(
)w)((
w)1(4wy1
11P
3
2/12/12
21
2/32/33122
2
11
Physical Domain
FcL
vM
<>F = (Q*/QV) V (1 + V)-0.36
Q* = <Q>B(T*)
cL
vM
Fudge factor –task for full models
Scaling
Away from boundaries, wind structure fully controlled by
Velocity Profile
Scale of v set by
222
22d
H
d cm10nn
k
r'r
1vv
V < 1: k = 2/3 (drift)
V > 1: k 0.4 (reddening)
K. Young 1995:
• v independent of L
• Mv 3.3
Drift!
Miras, low :M
Radiation pressure:
• v L1/2
• v independent of M
5.1v
3 )1(MAv
Drift Effect on Outflow
L/M 3/4V
222A
Same ndd/nH for C- and O-stars!
Drift+Reddening effect on v
• Lower – decoupling; v
• Higher – quenching; v
M
M
14/14max
14/34
6max
kmsL20v
yrML102)v(M
v = 18
• Shape V
• Flux level
SED Analysis
Zubko & Elitzur ’00
v = 0.83
Solutions by DUSTY http://www.pa.uky.edu/~moshe/dusty/
+ distance L
• L + v , 22M
W Hya
Thermal H2O Lines
• W Hya (ZE ‘00):
21 lines fitted H2O abundances
• VY CMa (Harwit & Bergin ‘02):
Same line ratios!
Hofmann et al ‘01
Vinković ‘02
Conclusions
• The “standard model” works
• Single variable –
• Dust drift – major ingredient
• Minimal = ?
22 ~ 1; why?
M
dFF1
dFF
Fc1
dFc1
dtdv
F
F
steady state: dt = (1/v)dr
F
F2
c12
dcL
dvM
drFrvdvr
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