H3+ + O

Gaz phase reaction (type: Bimolecular reactions)  


     
 
Datasheet    T(K) = 10-300   
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Channels
H3+ + O → H2 + OH+
T(K): 10-300
Formula: Modified Arrhenius equation
Δ rH0 = -69.078
Δ rH298 = -62.852
2010-03-30
H3+ + O → H + H2O+
T(K): 10-300
Formula: Modified Arrhenius equation
Δ rH0 = -167.54
Δ rH298 = -162.261
2010-03-30
k( )
cm3s-1 		Details
1.18e-9 H3+ + O → H2 + OH+
T(K) = 10-300
α = 7.98E-10
β = -1.56E-1
γ = 1.41E+0
F 0 = 1.4
g = 0
Type uncert: lognormal
Method: Reviews and Evaluations
Description: The review from the ISSI team has been modified in order to take into account new theoretical results.
5.05e-10 H3+ + O → H + H2O+
T(K) = 10-300
α = 3.42E-10
β = -1.56E-1
γ = 1.41E+0
F 0 = 1.4
g = 0
Type uncert: lognormal
Method: Reviews and Evaluations
Description: The review from the ISSI team has been modified in order to take into account new theoretical results.
Reference
Origin: Datasheet
Authors:
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Year:
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Bettens, R. P. A. et al (1999)    T(K) = 0-70   
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Channels
H3+ + O → H2 + OH+
T(K): 0-70
Formula: Modified Arrhenius equation
Δ rH0 = -69.078
Δ rH298 = -62.852
2009-10-23
H3+ + O → H + H2O+
T(K): 0-70
Formula: Modified Arrhenius equation
Δ rH0 = -167.54
Δ rH298 = -162.261
2009-11-09
k( )
cm3s-1 		Details
1.83e-9 H3+ + O → H2 + OH+
T(K) = 0-70
α = 1.12E-9
β = -1.44E-1
γ = 0.00E+0
F 0 = 2
g = 0
Type uncert: lognormal
Method: Calculations
1.17e-10 H3+ + O → H + H2O+
T(K) = 0-70
α = 7.14E-11
β = -1.44E-1
γ = 0.00E+0
F 0 = 2
g = 0
Type uncert: lognormal
Method: Calculations
Reference
Origin: Bibliography
Authors: Bettens, R. P. A. et al
Volume,Page: 111, 6322
Year: 1999
DOI: -
Download citation: Bibtex RIS
 
Other database : OSU    T(K) = 10-800   
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Channels
H3+ + O → H2 + OH+
T(K): 10-800
Formula: Modified Arrhenius equation
Δ rH0 = -69.078
Δ rH298 = -62.852
2014-03-05
k( )
cm3s-1 		Details
8.00e-10 H3+ + O → H2 + OH+
T(K) = 10-800
α = 8.00E-10
β = 0.00E+0
γ = 0.00E+0
F 0 = 2
g = 0
Type uncert: lognormal
Method: Estimation
Description: Reactions used in the high temperature network for ISM applications by Harada et al. (2010)
Reference
Origin: Other database : OSU
Authors: Harada, N. et al
Volume,Page: 721,1570-1578
Year: 2010
DOI: DOI
Download citation: Bibtex RIS
 
Other database : OSU    T(K) = 10-280   
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Channels
H3+ + O → H2 + OH+
T(K): 10-280
Formula: Modified Arrhenius equation
Δ rH0 = -69.078
Δ rH298 = -62.852
2009-03-27
k( )
cm3s-1 		Details
8.00e-10 H3+ + O → H2 + OH+
T(K) = 10-280
α = 8.00E-10
β = 0.00E+0
γ = 0.00E+0
F 0 = 1.5
g = 0
Type uncert: lognormal
Method: Estimation
Reference
Origin: Other database : OSU
Authors:
Volume,Page:
Year:
DOI: -
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Datasheet    T(K) = 10-298   
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Channels
H3+ + O → H2 + OH+
T(K): 10-298
Formula: Modified Arrhenius equation
Δ rH0 = -69.078
Δ rH298 = -62.852
2009-10-16
H3+ + O → H + H2O+
T(K): 10-298
Formula: Modified Arrhenius equation
Δ rH0 = -167.54
Δ rH298 = -162.261
2009-10-16
k( )
cm3s-1 		Details
1.74e-9 H3+ + O → H2 + OH+
T(K) = 10-298
α = 8.54E-10
β = -2.10E-1
γ = 0.00E+0
F 0 = 1.4
g = 0
Type uncert: lognormal
Method: Reviews and Evaluations
Description: See datasheet - result of the ISSI review ---- THIS HAS BEEN UPDATED
7.48e-10 H3+ + O → H + H2O+
T(K) = 10-298
α = 3.66E-10
β = -2.10E-1
γ = 0.00E+0
F 0 = 1.4
g = 0
Type uncert: lognormal
Method: Reviews and Evaluations
Description: See datasheet - result of the ISSI review ---- THIS HAS BEEN UPDATED
Reference
Origin: Datasheet
Authors:
Volume,Page:
Year:
DOI: -
Download citation: