the distribution of cosmic-ray ionization rates in diffuse molecular clouds as probed by h 3 +
DESCRIPTION
The Distribution of Cosmic-Ray Ionization Rates in Diffuse Molecular Clouds as Probed by H 3 +. Nick Indriolo Johns Hopkins University. In Collaboration with. Ben McCall (University of Illinois) Brian Fields (University of Illinois) Tom Geballe (Gemini Observatory) Geoff Blake (Caltech) - PowerPoint PPT PresentationTRANSCRIPT
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The Distribution of Cosmic-Ray Ionization
Rates in Diffuse Molecular Clouds as Probed by H3
+
Nick IndrioloJohns Hopkins University
February 10, 2012 Chemistry, Astronomy, & Physics of H3
+
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In Collaboration with...• Ben McCall (University of Illinois)• Brian Fields (University of Illinois)• Tom Geballe (Gemini Observatory)• Geoff Blake (Caltech)• Miwa Goto (MPIA)• Tomonori Usuda (Subaru Telescope)• David Neufeld (Johns Hopkins)• Takeshi Oka (University of Chicago)
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Outline• Introduction to cosmic rays and
interstellar H3+
• Calculating the cosmic-ray ionization rate
• Observations of H3+ and example
spectra• Line-of-sight properties and ζ2
• The distribution of ionization rates• Ionization rate and location• Complementary tracers and future
work
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Cosmic Rays• Discovered in 1912 by Victor Hess
during balloon borne experiments that showed increased radiation at higher altitudes
• Later dubbed cosmic rays (Millikan 1926)
• Now known to be highly energetic charged particles (p, e-, e+, α, nuclei)
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Energy Distribution• Power law in
energy (φ~E-2.7) spanning 12 decades in E, and 30 decades in flux
• Spectral shape is consistent for all species
Swordy 2001
Ave et al. 2008
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Particle Interactions• Ionization
p + H2 H2+ + e- + p'
• Spallation and Fusion[p, ] + [12C, 14N, 16O] [6Li,7Li,9Be,10B,11B]
• Nuclear Excitation[p, ] + 12C 12C* 12C + γ4.44 MeV
• Inelastic Collisionsp + H p' + H + 0 γ +
γ
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Ionization by Cosmic Rays• Cosmic rays ionize H, He, and H2
throughout diffuse molecular clouds, forming H+, He+, and H3
+
• Initiates the fast ion-molecule reactions that drive chemistry in the ISM
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Ion-Molecule Reactions
CRH2+
H2
H2 H3+
CO HCO
+
O
OH+
N2
N2H+
H2H2O+
H2 H3O+
CRH H
+
OO+
H2
OH
H2O
e-e-e-
H+
H
hν
hν
O
H3+
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ζ2 over the past 50 years
Hayakawa et al. 1961; Spitzer & Tomasko 1968; O'Donnell & Watson 1974; Hartquist et al. 1978; van Dishoeck & Black 1986; Federman et al. 1996; Webber 1998; McCall et al. 2003; Indriolo et al. 2007; Gerin et al. 2010; Neufeld et al. 2010
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H3+ Chemistry
• Formation– CR + H2 H2
+ + e- + CR'–H2
+ + H2 H3+ + H
• Destruction–H3
+ + e- H + H + H (diffuse clouds)–H3
+ + O OH+ + H2 (diffuse & dense clouds)
–H3+ + CO HCO+ + H2 (dense clouds)
–H3+ + N2 HN2
+ + H2 (dense clouds)
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Steady State Equation
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Necessary Parameters
• ke measured in lab (adopt McCall et al. 2004)• xe approximated by x(C+)≈1.510-4 Cardelli et
al. 1996; Sofia et al. 2004• nH estimated from rotational excitation analysis
of C2 (Sonnentrucker et al. 2007) or thermal pressure analysis of fine structure lines of C I (Jenkins et al. 1983; Jenkins & Tripp 2001)
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• N(H2)–UV observations of H2 lines
(Savage et al. 1977; Rachford et al. 2002, 2009)
–N(CH)/N(H2)≈3.510-8 (Sheffer et al. 2008)
–NH≈E(B-V)5.81021 cm-2 mag-1 (Bohlin et al. 1978; Rachford et al. 2002)
• All that remains is N(H3+)
Necessary Parameters (cont.)
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Targeted Transitions• Transitions of the 2 0
band of H3+ are available
in the infrared• Given average diffuse
cloud temperatures (70 K) only the (J,K)=(1,0) & (1,1) levels are significantly populated
• Observable transitions are:– R(1,1)u: 3.668083 μm– R(1,0): 3.668516 μm– R(1,1)l: 3.715479 μm– Q(1,1): 3.928625 μm– Q(1,0): 3.953000 μm
Energy level diagram for theground vibrational state of H3
+
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Instruments & Telescopes
Phoenix: Gemini South
CRIRES: VLT UT1
CGS4: UKIRT
NIRSPEC: Keck II
IRCS: Subaru
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Survey Status
• Observations targeting H3+ in diffuse
clouds have been made in 50 sight lines
• H3+ is detected in 21 of those
Dame et al. 2001
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Example Spectra
CRIRES at VLT
S/N Wλ (10-6 μm) N(H3+) (1014 cm-2)
HD 110432
1200 0.7 0.5
HD 313599
300 4.5 3.2
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ζ2 vs. Position
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ζ2 vs. Total Column Density
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Particle Range
Padovani et al. 2009
Range for a 1 MeV proton is ~31020 cm-2
Range for a 10 MeV proton is ~21022 cm-2
Diffuse cloud column densities are about 1021 ≤ NH ≤ 1022 cm-2
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Distribution of Ionization Rates
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Where do we stand?
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Regional Distributions
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Ophiuchus-Scorpius region
Image Credit: Rogelio Bernal Andreo
o Sco HD 147889
ρ Oph D
χ Oph
3 pc
N
E
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Per OB2 region
4.6 pc
10.5 pc
Image Credit: Rogelio Bernal Andreo
PSR J0357+3205
ζ Per
o Per
ξ Per
X Per
40 PerBD +31 643
N
E
N(H2)=4.1×1020 cm-2
N(H2)=4.8×1020 cm-2
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Why the Differences?• Particle range determined by energy• Cosmic rays must get from
acceleration site to observed clouds• Ionization rate controlled by
proximity of cloud to nearest acceleration site
• If true, ζ2 should be large near known source, e.g. IC 443, a supernova remnant
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IC 443 Survey
ALS 8828
HD 254577
HD 254755
HD 43582
Image credit: Gerhard Bachmayer
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ALS 8828
HD 254577
HD 43582
HD 254755
IC 443 Results
• SNRs accelerate cosmic rays• Proximity to IC 443 boosts ζ2
• Ionization rates vary over a few pc
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Conclusions• ζ2 is NOT a constant!!!!!• !!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
!!!!• The cosmic-ray ionization rate is
controlled by the distance between a cloud and acceleration site
• Different regions of the sky show different distributions of ζ2
• ζ2 can vary on size scales of a few pc
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H3+ work in progress/development
• Observe H3+ near W 28 & Vela SNRs
• High S/N survey of compact regions (Sco-Oph & Per OB2)
• Southern hemisphere survey (CRIRES)
• ESO Archive survey
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Ion-Molecule Reactions
CRH2+
H2
H2 H3+
CO HCO
+
O
OH+
N2
N2H+
H2H2O+
H2 H3O+
CRH H
+
OO+
H2
OH
H2O
e-e-e-
H+
H
hν
hν
O
H3+
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ζ from OH+ and H2O+
• Oxygen chemistry closely linked to ionization rate of H (ζH)
• ε is fraction of H+ that forms OH+
• Needs to be determined
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W 51
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Preliminary results• from H3
+: ζ2=(12.5±9.3)×10-16 s-1
• from OH+: ζHε=(0.52±0.28)×10-16 s-1
• taking 2.3ζH=1.5ζ2: ζ2ε=(0.79±0.43)×10-16 s-1
• ε=0.06 ± 0.03• >90% of the time, cosmic-ray
ionization of H does not result in OH+
• Grain neutralization on PAH-
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γ-ray Signatures
IC 443, VERITAS;Acciari et al. 2009
W28, Fermi-LAT;Abdo et al. 2010
W51C, Fermi-LAT;Carmona et al. 2011
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Diffuse γ-ray Signatures
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Thanks!