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Astrochimistry – Spring 2013 Lecture 3:
H2 Formation
Julien Montillaud1st February 2013
2
OutlineI. The most abundant molecule in the Universe (6 p.)
I.1 Relative abundancesI.2 Historical milestonesI.3 Observational evidenceI.4 Destruction of H2I.5 Chemistry prefers ménages-à-trois
II. The inefficient gas-phase formation of H2 (4 p.)
II.1 ProcessesII.2 Astrophysical applications
III. Grain-catalyzed formation of H2 (11 p.)
III.1 A new partner: dust grainsIII.2 The Langmuir-Hinshelwood mechanismIII.3 The Eley-Rideal mechanismIII.4 Other mechanisms
IV. From processes to interstellar H2 formation rate (10 p.)
IV.1 Relative contribution to H2 formation rate
IV.2 Implementing H2 formation in astrophysical models
IV.3 Astrochemical application
V. Summary
VI. Some bibliographic references
3
I. The most abundant molecule in the UniverseI.1 Relative abundance
The “astronomer's periodic table”McCall, Phil. Trans. R. Soc. A (2006)
● H = most abundant chemical element( 10 x He ; 10000 x C, N, O ; …)
● H = radical ⇒ a very reactive species
http://en.wikipedia.org/wiki/File:Periodic_Table_2.svg
Ene
rgy
1s
2s2p
x2p
y2p
z
H: incomplete shell ⇒ radical
4
I. The most abundant molecule in the UniverseI.2 Historical milestones
Gould & Salpeter (1963): first model of H2 formation on dust grains (dirty ice, no defects)
H2 never detected yet still a theoretical hypothesis ! ⇒
Hollenbach & Salpeter (1971): first model of H2 formation on dust grains including defects
Jura (1974): determination of the H2 formation rate from UV observations (Copernicus)
Measurement of H2 density from UV absorption lines
Measurement of UV radiation field from UV continuum ⇒ Derivation of H2 destruction rate
Assuming destruction rate = formation rate ⇒ Measure of the H
2 formation rate: 3e-17 n
H n(H) cm3s-1
Launch of ISO (1995): detection of H2 in the IR
Le Bourlot et al. (1995): Rationalization of H2 formation from grain characteristics
1990' – 2000': multiplication of theoretical and experimental studies of catalyzed formation of H2
+ observational evidence for H2 formation in unexpected conditions
(e.g. Habart et al. 2004, 2005, 2011)
Le Bourlot et al. (2012): detailed modeling of H2 formation in a realistic astrophysical model
5
I. The most abundant molecule in the UniverseI.3 Observational evidence: electronic and rotational lines
High-resolution UV spectroscopy using HST
Meyer et al. 2001
http://www.stolaf.edu/depts/chemistry/imt/js/h2energy/h2.htm
Mid-IR spectroscopy using Spitzer
Guillard et al. 2010
J=0
J=1
J=2
J=3
J=4
6
I. The most abundant molecule in the UniverseI.3 Observational evidence: electronic and rotational lines
H2 can be formed in very various conditions:
Hot/coldDense/not densedEven in some high-UV or X-ray radiation fieldsRight after shock waves
⇒ many different formation paths exist
7
I. The most abundant molecule in the UniverseI.4 Destruction of H
2
Destruction rate:
diss = <p
diss>
photoext ~ 4 x 10-11 s-1
diss : photodissociation rate
<pdiss
> : dissociation probability averaged over
the photoexcitation channels
photoext : rate of photoexcitation by UV photons
: scaling factor of the interstellar radiation field (IRSF)
Hollenbach & Tielens 1999
In steady-state:
diss n(H
2) = R
gr n
H n(H)
with nH = 100 cm-3 and =1:
n(H2)/n(H) ~ 10-4
8
I. The most abundant molecule in the UniverseI.5 Chemistry prefers ménages-à-trois
Enough energy to cross the activation barrier from reactants to products<=>
Enough energy to cross the activation barrier from products to reactants
Survival of products if energy is released via a third “body”:- loss of a particle (atom, small molecule, electron)- emission of photons- dilution of the energy in a very large system (=emission of phonons)- 3-body collisions (efficient only at high density)
It has to happen during the collision process ~1e-13 s
9
II. The inefficient gas-phase formation of H2
I. The most abundant molecule in the Universe
II. The inefficient gas-phase formation of H2
II.1 ProcessesII.2 Astrophysical applications
III. Grain-catalyzed formation of H2
IV. From processes to interstellar H2 formation rate
V. Summary
10
II. The inefficient gas-phase formation of H2II.1 Processes
H + H → H2 Collision timescale ~ 1 vibration period ~ 1e-13 s
Energy to be released ~ 4.5 eV (binding energy)
● From electronic ground state ?
(Ro-)vibrational emission: nhu in up to 4.5 eV for vibrationally or rotationaly excited H2
But Einstein coefficient: A << 1e-5 s-1 ( << 1e13 s-1 )
“only one in 1e5 collisions would result in the formation Of molecular hydrogen” (Duley & Williams 1984)
● From electronicaly excited states ?
A increases when n increases, but still very small :
Latter & Black 1991
11
II. The inefficient gas-phase formation of H2II.1 Processes
Other processes
H + H* → H2
+ + e- (Rawlings et al. 1993)
H2
+ + e- → H2
More efficient than H + H → H2 for high n(e-) and low
H + e- → H- + H- + H → H
2 + e-
The most efficient gas-phase process (Glover 2003) for high n(e-) and low
H + H+ → H2
+ + H
2
+ + H → H2 + H+
The second most efficient gas-phase process (Glover 2003)
H + H + H → H2 + H (Palla et al. 1983)
Requires nH > 1e8 cm-3
12
II. The inefficient gas-phase formation of H2II.2 Astrophysical application
From chemical processes to astrophysical modeling: chemical kinetics
H + e- → H- + k1
H- + H → H2 + e- k
2
H + H+ → H2
+ + k3
H2
+ + H → H2 + H+ k
4
H- + H+ → 2H k5
H- + → H + e- k6
⇒
Glover 2003
13
II. The inefficient gas-phase formation of H2II.2 Astrophysical application
Where there is no dust:
Early Universe
Latter & Black 1991
Where dust grains are hot, and gasis hot, dense, and with a large enough ionization fraction:→ X-ray dissociation regions(AGNs, embedded massive protostars, ...)
Novae ejecta
Wikipedia
Centaurus A
Very specific cases! For all the other cases, gas-phase formation is neglegible wrt catalyzed routes.
14
III. Grain-catalyzed formation of H2
I. The most abundant molecule in the Universe
II. The inefficient gas-phase formation of H2
III. Grain-catalyzed formation of H2
III.1 A new partner: dust grainsIII.2 The Langmuir-Hinshelwood mechanismIII.3 The Eley-Rideal mechanismIII.4 Other mechanisms
IV. From processes to interstellar H2 formation rate
V. Summary
15
III. Grain-catalyzed formation of H2
III.1 A new partner: dust grains
Various compositions: C, Si, Mg, Fe, … (+H, O)+ molecular ices according to environments
⇒ various surface properties
Various sizes
16
III. Grain-catalyzed formation of H2
III.2 The Langmuir-Hinshelwood mechanism
Distance to surface
Chemisorptionsite
Physisorptionsite
Pot
entia
l ene
rgy
(1) (2) (3) (4) (5)
(1) physisorption of one H-atom
(2) physisorption of one other H-atom on the same grain
(3) traveling of physisorbed H-atom on grain surface
(4) encounter chemical binding of H-atoms
(5) desorption of the new H2 molecule
Physisorption = weak van der Waals interactionChemisorption = strong covalent bound
17
(1) (2) (3) (4) (5)
(1) physisorption of one H-atom
(2) physisorption of one other H-atom on the same grain
Depends on:
- surface nature (silicate, carbonaceous, ice) - structure (amorphous, cristaline, porosity)- presence of defects
III. Grain-catalyzed formation of H2
III.2 The Langmuir-Hinshelwood mechanism
18
(3) (4) (5)(3)
(3) traveling of physisorbed H-atom on grain surface
Depends on:
- surface nature (silicate, carbonaceous, ice) - structure (amorphous, cristaline, porosity)- presence of defects
Processes:→ thermal diffusion
(moving over barriers from site to site)
→ quantum tunneling(moving through barriers from site to site)
III. Grain-catalyzed formation of H2
III.2 The Langmuir-Hinshelwood mechanism
19
(3) (4) (5)(4)
(4) encounter chemical binding of H-atoms
(5) desorption of the new H2 molecule
Depends on:
- surface nature (silicate, carbonaceous, ice) - structure (amorphous, cristaline, porosity)- presence of defects
A related issue: distribution of the energy released→ translational kinetic energy→ grain vibrational energy→ H
2 vibrational/rotational energy
Consequences:→ nebula energetics (gas temperature)→ excited-H2 spectroscopic diagnostics→ grain temperature (possible feedback on H2 formation rate)→ chemistry involving excited H2 (e.g. formation of CH+)
(5)
III. Grain-catalyzed formation of H2
III.2 The Langmuir-Hinshelwood mechanism
20
(1) (2) (3) (4) (5)
Behaviour with grain temperature:
→ too low T: H-atoms do not move efficiently→ too high T: H-atoms evaporate before encountering an other H-atom
⇒ efficient for T ~ 10 – 50 K
III. Grain-catalyzed formation of H2
III.2 The Langmuir-Hinshelwood mechanism
21
III. Grain-catalyzed formation of H2
III.3 The Eley-Rideal mechanism
(1) (2) (3)
(1) chemisorption of one H-atom
(2) collision between a gas-phase H-atomand the chemisorbed H-atom
(3) desorption of the new H2 molecule
Distance to surface
Chemisorptionsite
Physisorptionsite
Pot
entia
l ene
rgy
Physisorption = weak van der Waals interactionChemisorption = strong covalent bound
22
(1) (2) (3)
Depends on:
- surface nature (silicate, carbonaceous, ice) - structure (amorphous, cristaline, porosity)- presence of defects
no traveling H-atom ⇒ less efficient than LHStrong bounds ⇒ robust with temperature
III. Grain-catalyzed formation of H2
III.3 The Eley-Rideal mechanism
23
Binding and barrier energies can depend on the position of the chemisorption site:
Rauls & Hornekaer 2008
III. Grain-catalyzed formation of H2
III.3 The Eley-Rideal mechanism
24
Binding and barrier energies also depend on history of the grain:
How many H-atoms are already bound to the grain ?
Rauls & Hornekaer 2008Rauls & Hornekaer 2008
III. Grain-catalyzed formation of H2
III.3 The Eley-Rideal mechanism
25
III. Grain-catalyzed formation of H2
III.4 Other mechanisms
Intermediate mechanisms:
→ physisorbed atoms can tunnel to chemisorption sites→ gas-phase atoms can strike physisorbed atoms→ traveling physisorbed atoms can find chemisorbed atoms
Distance to surface
Chemisorptionsite
Physisorptionsite
Pot
entia
l ene
rgy
26
IV. From processes to interstellar H2 formation rate
I. The most abundant molecule in the Universe
II. The unefficient gas-phase formation of H2
III. Grain-catalyzed formation of H2
IV. From processes to interstellar H2 formation rate
IV.1 Relative contribution to H2 formation rate
IV.2 Implementing H2 formation in astrophysical models
IV.3 Astrochemical application
V. Summary
27
IV. From processes to interstellar H2 formation rate
IV.1 Relative contributions to H2 formation rate
Cazaux et al. 2005Modelling H
2 formation efficiency
on carbonaceous grains
Assuming:→ Tdust = constant→ Tgas = Tdust + 500 K→ Some particular values for binding and barrier energies
LH: dominates at low Tdust
ER: significant at high Tdust
LH versus ER
28
IV. From processes to interstellar H2 formation rate
IV.1 Relative contributions to H2 formation rate
Grain size and the effect of temperature fluctuations
Surface(Small grains) > Surface(Big grains) H⇒2 formation dominated by small grains
BUT: → small grain
⇒ small thermal capacity ⇒ large thermal fluctuations ⇒ stochastic behaviour
→ small grain ⇒ small surface per grain ⇒ higher risk that means
are meaningless (e.g. 0.3 H-atom per grain)
29
IV. From processes to interstellar H2 formation rate
IV.2 Implementing H2 formation in astrophysical models
Rate equations (example of LH implementation)
= surface density of physisorbed H-atomsf = flux of impinging H-atomsW = desorption rate coefficienta = hopping rate ~ H
2 formation rate coefficient
H(g)
→ H: (f)
H: → H(g)
(W)
H: + H: → H2(g)
(a)
The H2 formation rate per unit surface of grain is then given by a2
BUT: small grains ⇒ small surface ⇒ “surface density” is meaningless
30
IV. From processes to interstellar H2 formation rate
IV.2 Implementing H2 formation in astrophysical models
Master equations (example of LH implementation)
Dealing with probabilities:n = number of Hatoms physisorbed on one grainP(n) = probability of having n Hatoms physisorbed on one grainS = maximum number of physisorption sites closure formula⇒dP(n)/dt = time derivative of P(n)F = flux of impinging H-atomsW = desorption rate coefficientA = hopping rate ~ H
2 formation rate coefficient
H(g)
→ H: (F)
H: → H(g)
(W)
H: + H: → H2(g)
(A)
31
IV. From processes to interstellar H2 formation rate
IV.2 Implementing H2 formation in astrophysical models
Master equations (example of LH implementation)
Mean number of H-atoms per grain:
H2 formation rate for one grain:
H2 formation efficiency:
Relation to rate equation:
32
IV. From processes to interstellar H2 formation rate
IV.2 Implementing H2 formation in astrophysical models
Rate equations versus Master equations
Biham & Lipshtat 2002
Master equations are more accurate but slower to solve (bigger system of equations)
33
IV. From processes to interstellar H2 formation rate
IV.2 Implementing H2 formation in astrophysical models
Moment equations
H2 formation rate for one grain: = A (<n2> - <n>)
Depends only on the 2 first moments of n !
The system must be closed. Possible for a limited number Nmax of physisorption sites:If Nmax = 2:
… and can be solved much faster than master equations.For Nmax reasonnable, the system must be truncated ⇒ approximate solution.
( “NH” is “n” )
Open system !
34
IV. From processes to interstellar H2 formation rate
IV.2 Implementing H2 formation in astrophysical models
ComparisonLipshtat & Biham 2003
35
IV. From processes to interstellar H2 formation rate
IV.3 Astrochemical application
Color = CO J=6-5Black = CH+ J=3-2White contours=H2* v=1-0 S(1)
Nagy et al. 2013
36
IV. From processes to interstellar H2 formation rate
IV.3 Astrochemical application
Detailled modelling of H2 formation
and excitation (Meudon PDR code)
⇒
good understanding of CH+ formationand excitation
⇒
CH+ is a good tracer of the external, warm layers of molecular cloudsNagy et al. 2013
37
V. Summary
H2 formation still not fully understood
Widely dominated by grain-catalyzed reactions
Many theoretical and experimental studies provide molecular data, but still not enough
Understanding is limited by:
- limited knowledge of dust grains- the huge number of parameters (e.g. grain size, composition, structure, fluffyness, ...)- the observational difficulties
The gas-grain chemistry requieres special care for modelling
In the future, progresses should be achieved from joint studies of H2 formation/excitation
and chemical evolution of other species (molecules, ions, grains) + improvements in modelling the ISM (energetics, morphology, radiative transfer, ...)
38
VI. Some bibliographic references
General:- McCall, Phil. Trans. R. Soc. A, 364 : 2953-2963 (2006)- Hollenbach & Tielens, Reviews of Modern Physics, 71 : 173 (1999)- Gould & Salpeter, ApJ, 138 : 393 (1963)- Hollenbach & Salpeter, ApJ, 163 : 155 (1971)- Jura, ApJ, 191 : 375-379 (1974)- Maloney et al., ApJ, 466 : 561–584 (1996)
Astrophysical aspects:- Glover, ApJ, 584 : 331-338 (2003)- Le Bourlot et al., A&A, 302 : 870 (1995)- Habart et al., A&A, 414 : 531 (2004)- Nagy et al. A&A in press (2013)
Theoretical chemistry aspects- Parneix & Bréchignac, A&A, 334 : 363–375 (1998)- Rauls & Hornekaer, ApJ, 679 : 531–536 (2008)- Latter & Black, ApJ, 372 : 161-166 (1991)
Experimental chemistry aspects- Pirronello et al., ApJ, 475 : L69–L72 (1997)- Islam, PHD thesis, UCL (2009)
Modelling aspects- Le Bourlot et al., A&A 541 : A76 (2012)- Biham & Lipshtat, arXiv:cond-mat/0208550v2 (2002)- Lipshtat & Biham, A&A, 400 : 585–593 (2003)- Cazaux et al., Journal of Physics: Conference Series, Volume 6, Issue 1, pp. 155-160 (2005)