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Observations of unusual CO isotopologue abundances toward protostars
Rachel L. Smith Nature Research Center/North Carolina Museum of Natural Sciences
Appalachian State University
Klaus M. Pontoppidan Space Telescope Science InstituteGeoffrey A. BlakeCalifornia Institute of TechnologyAdwin C.A. BoogertNASA Herschel Science CenterAlexandra C. LockwoodCalifornia Institute of Technology
Workshop on Ice and Planet FormationLund Observatory, Lund, Sweden
15 May 2013
Monday, May 20, 13
Orion
Ophiuchus
Serpens
Corona Australis
CRIRES observations of CO isotopologues toward protostars enable precise study of carbon and oxygen isotopic reservoirs
1.2
1.0
0.8
0.6
0.4
0.2
4720470046804660
12C16O ice
P (3), P(4), P (5)12C16O
Serpens molecular cloud, d Sun ~ 230 pc
EC 90 (1)
EC 90 (0)
Portion of VLT-CRIRES spectrum toward embedded binary protostar EC 90
Flux
Wavelength (nm)
Monday, May 20, 13
1.2
1.1
1.0
0.9
0.8
0.7
235423522350234823462344
P(3)
P(2)
P(1)R(0)
EC 90 (S) EC 90 (N)
Partial CO overtoneEC 90
Wavelength (nm)
Flux
Binaries, VLT-CRIRES EC 90, Serpens
1.2
1.0
0.8
0.6
0.4
0.2
4720470046804660
EC 90
12C16O ice
P (3), P(4), P (5)12C16O
EC 90 (S)
EC 90 (N)
Partial fundamental CO band
Flux
Wavelength (nm)
Ciardi et al. 2005
N
S
Monday, May 20, 13
McKeegan et al. 2011
High-resolution astronomical observations can be used to investigate isotope anomalies in the solar system
!
" iO =
iO16O#
$ %
&
' (
iO16O#
$ %
&
' ( SMOW
)1
*
+ , ,
- , ,
.
/ , ,
0 , ,
x103
Monday, May 20, 13
McKeegan et al. 2011!
" iO =
iO16O#
$ %
&
' (
iO16O#
$ %
&
' ( SMOW
)1
*
+ , ,
- , ,
.
/ , ,
0 , ,
x103
CO self-
shie
ldin
g?
High-resolution astronomical observations can be used to investigate isotopologue-specific photodissociation in protostellar environments
Monday, May 20, 13
High- to medium-resolution observations are used to investigate 12CO and 13CO reservoirs in protostars
TexXt
Local ISM
Solar system
13C, primary and secondary origin
13C, secondary origin
After Prantzos et al. 1996
After Milam et al. 2005
Solar ~ 89
ISM ~ 70
Assumption: the solar system represents the
isotopic composition of the local ISM ~ 4.6 Gya
Implication: protostars observed today should
represent their parent clouds
Monday, May 20, 13
Precise abundances of CO isotopologues are calculated using high resolution near-IR spectroscopy
CRIRES instrument R ~ 95,000
VLT-CRIRES
Smith et al. 2009
Monday, May 20, 13
CRIRES instrument R ~ 95,000
CO line profiles are used to determine column densities
€
NJ =τοb 2πλο
mecπe2 f&
' (
)
* +
Smith et al. 2009
Precise abundances of CO isotopologues are calculated using high resolution near-IR spectroscopy
Monday, May 20, 13
€
NTot = N0 2J +1( )exp −hcBJ(J +1)kT
# $ %
& ' (
J
j∑
Smith et al. 2009
Precise abundances of CO isotopologues are calculated using high resolution near-IR spectroscopy
Monday, May 20, 13
Sample Rotational Analyses
Disk
Foreground cloud
Shared envelope?
40
35
30
806040200
EC 90 (1)
(black diamonds) (blue stars)
13 K
23 K
11 K17 K
17 K
22 K
E/k (K)
Ln(N
J/(2J
+1))
EC 90 (S) and EC 90 (N)
12C17O 12C18O13C16O
12C16O
Embedded core
Smith et al. 2009, Smith et al. in revision
Monday, May 20, 13
(cold)
(warm)
Best-derived 12CO/13CO abundance ratios from CRIRES sources
Smith et al. in revision
Monday, May 20, 13
0.6
0.5
0.4
0.3
0.2
0.1
0.0
1801601401201008060
IRS 44 ,Oph
V V CrA
RE50
LLN 19, Vela
V V CrA(S,N), Corona A.
DoAr24E(0,1), Oph
RNO 91, L 43
IRS 63 ,Oph
HL Tau, Taurus
RE 50, Orion
RNO 91, L 43
IRS 63 ,Oph
EC 90(0), Ser
EC 90(1), Ser
IRS 51, Oph
CO Ic
e Fr
actio
n
[ 12C16O]/[ 13C16O]Gas
[12C16
O] Ic
e/([12
C16O
] Ice
+ [12
C16O
] Gas
)
Total 12C16O ice vs 12CO/13COgas
Smith et al. in revision
Monday, May 20, 13
0.6
0.5
0.4
0.3
0.2
0.1
0.0
1801601401201008060
IRS 44 ,Oph
LLN 19, Vela
V V CrA(S), Corona A.
DoAr24E(0,1), Oph
EC 90(0), Ser
EC 90(1), Ser
IRS 51, Oph
CO Ic
e Fr
actio
n
[ 12C16O]/[ 13C16O]Gas
[12C16
O] Ic
e/([12
C16O
] Ice
+ [12
C16O
] Gas
)
Smith et al. in revision
Targets with only cold gas lines provide most precise
evaluation of potential 12CO-13CO gas-ice interaction
45
40
35
30
806040200
(black diamonds) (blue stars)
13 K
23 K
17 K
22 K
E/k (K)
Ln(N
J/(2J
+1))
EC 90 (S) and EC 90 (N)
13C16O
12C16O
Monday, May 20, 13
0.6
0.5
0.4
0.3
0.2
0.1
0.0
1801601401201008060
IRS 44 ,Oph
LLN 19, Vela
V V CrA(S), Corona A.
DoAr24E(0,1), Oph
EC 90(0), Ser
EC 90(1), Ser
IRS 51, Oph
CO Ic
e Fr
actio
n
[ 12C16O]/[ 13C16O]Gas
[12C16
O] Ic
e/([12
C16O
] Ice
+ [12
C16O
] Gas
)
Targets with only cold gas lines provide most precise
evaluation of potential 12CO-13CO gas-ice interaction
Suggested trend between cold gas
[12CO/13CO]gas and CO ice fraction
Smith et al. in revision
45
40
35
30
806040200
(black diamonds) (blue stars)
13 K
23 K
17 K
22 K
E/k (K)
Ln(N
J/(2J
+1))
EC 90 (S) and EC 90 (N)
13C16O
12C16O
Monday, May 20, 13
Oxygen isotopes1000
500
0
-500
-1000 10005000-500-1000
V V CrA (S)Corona AustralisTaurusOrionSerpensL 43OphiuchusStar-forming regions:EC90(1)
IRS 44
RNO 91
mass-dependentmass
-inde
pend
ent
18O/17O = 4.1
18O/17O = 3.5
Local ISM
IRS 63
HL Tau
V V CrA (N)
RE 50
δ18O'=103ln(18Ri/18RLocal ISM)
δ17 O
'=103 ln
(17R i
/17R L
ocal
ISM)
Smith et al. in revision; Smith et al. 2009
!
" iO =
iO16O#
$ %
&
' (
iO16O#
$ %
&
' ( SMOW
)1
*
+ , ,
- , ,
.
/ , ,
0 , ,
x103
Monday, May 20, 13
1000
500
0
-500
-1000 10005000-500-1000
V V CrA (S)Corona AustralisTaurusOrionSerpensL 43OphiuchusStar-forming regions:EC90(1)
IRS 44
RNO 91
mass-dependentmass
-inde
pend
ent
18O/17O = 4.1
18O/17O = 3.5
Local ISM
IRS 63
HL Tau
V V CrA (N)
RE 50
δ18O'=103ln(18Ri/18RLocal ISM)
δ17 O
'=103 ln
(17R i
/17R L
ocal
ISM)
Oxygen isotopes
Signature of CO isotopologue-specific
photodissociation
Smith et al. in revision; Smith et al. 2009
!
" iO =
iO16O#
$ %
&
' (
iO16O#
$ %
&
' ( SMOW
)1
*
+ , ,
- , ,
.
/ , ,
0 , ,
x103
Monday, May 20, 13
Massive protostarsCO ice and gas in high-UV fields at greater dSun
80
60
40
20
4.694.684.67
Juggler Nebula, d Sun ~ 2 kpc
R (9)R (10)R (11)
Wavelength [µm]
Flux
R (13)R (12)
P (3)P (2)P (1)
13C16O
12C16O
Portion of KECK-NIRSPEC CO rovibrational spectrum toward massive protostar AFGL 2136
Keck-NIRSPEC
NIRSPECR~ 25,000
R(0)R(1)
P(1) P(2) P(3) ........
Smith et al., new data
Smith et al., new data
Monday, May 20, 13
Conclusions
Significant heterogeneity is observed in [12CO]/[13CO]gas toward a range of local protostellar environments
Weak isotopic signature indicates that interplay between CO ice and CO isotopic reservoirs could influence [12CO]/[13CO]gas
Signature of CO self-shielding in two disks
Binaries may trace isotopically similar gas environments
Embedded cores may trace varying chemical pathways within the same cloud and between clouds
Additional precise data for a range of protostellar evolutionary stages, dSun and RGC will help in further evaluation of CO gas and ice isotopic reservoirs
Monday, May 20, 13