C₃⁺

C3 ion
Flags: RATE12
Empirical: C₃⁺
Mass: 36 amu
Heat of formation: 2004.0 kJ mol^-1
Added to system: 2003-05-06 06:43:21

22 C₃⁺ formation reactions

	Reaction	α	β	T_l - T_u (K)
1	H⁺ + C₃ → C₃⁺ + H	4.00e-9	0.00	10 - 41000
2	C⁺ + C₂H → C₃⁺ + H	1.00e-9	0.00	10 - 41000
3	C⁺ + C₂S → C₃⁺ + S	5.00e-10	-0.50	10 - 41000
4	C⁺ + C₃O → C₃⁺ + CO	3.33e-10	-0.50	10 - 41000
5	C⁺ + HC₃N → C₃⁺ + HCN	2.50e-10	-0.50	10 - 41000
6	C₂⁺ + C₂ → C₃⁺ + C	8.70e-10	0.00	10 - 41000
7	C + C₂H⁺ → C₃⁺ + H	1.10e-9	0.00	10 - 41000
8	CH⁺ + C₂ → C₃⁺ + H	1.00e-9	0.00	10 - 41000
9	CH⁺ + C₂H → C₃⁺ + H₂	9.80e-10	0.00	10 - 41000
10	CH + C₂⁺ → C₃⁺ + H	3.20e-10	-0.50	10 - 41000
11	H⁺ + C₃H → C₃⁺ + H₂	2.00e-9	-0.50	10 - 41000
12	HNC₃ + C⁺ → C₃⁺ + HNC	1.55e-9	-0.50	10 - 41000
13	HNC₃ + He⁺ → C₃⁺ + NH + He	2.00e-9	-0.50	10 - 41000
14	He⁺ + C₃H → C₃⁺ + He + H	2.00e-9	-0.50	10 - 41000
15	He⁺ + C₃O → C₃⁺ + O + He	1.00e-9	-0.50	10 - 41000
16	He⁺ + C₃P → C₃⁺ + P + He	5.00e-10	-0.50	10 - 41000
17	He⁺ + C₄ → C₃⁺ + C + He	6.70e-10	0.00	10 - 41000
18	He⁺ + C₄S → CS + C₃⁺ + He	5.00e-10	-0.50	10 - 41000
19	He⁺ + C₅ → C₃⁺ + C₂ + He	1.00e-9	0.00	10 - 41000
20	He⁺ + CH₂CCH → C₃⁺ + He + H₂ + H	6.70e-10	-0.50	10 - 41000
21	He⁺ + CH₃CCH → C₃⁺ + He + H₂ + H₂	5.00e-10	0.00	10 - 41000
22	He⁺ + H₂CCC → C₃⁺ + He + H₂	1.00e-9	-0.50	10 - 41000

	Reaction	α	β	T_l - T_u (K)
1	C₂H₄ + C₃⁺ → C₂H₄⁺ + C₃	3.96e-10	0.00	10 - 41000
2	C₃⁺ + e^- → C₂ + C	3.00e-7	-0.50	10 - 300
3	C₂H₂ + C₃⁺ → C₅H⁺ + H	1.70e-9	0.00	10 - 41000
4	C₂H₄ + C₃⁺ → C₃H₂⁺ + C₂H₂	1.35e-10	0.00	10 - 41000
5	C₂H₄ + C₃⁺ → C₅H₂⁺ + H₂	2.34e-10	0.00	10 - 41000
6	C₂H₄ + C₃⁺ → C₅H₃⁺ + H	1.35e-10	0.00	10 - 41000
7	C₃⁺ + HC₃N → C₅H⁺ + CN	3.20e-9	-0.50	10 - 41000
8	CH₄ + C₃⁺ → C₃H⁺ + CH₃	2.38e-10	0.00	10 - 41000
9	CH₄ + C₃⁺ → C₄H₂⁺ + H₂	3.61e-10	0.00	10 - 41000
10	CH₄ + C₃⁺ → C₄H₃⁺ + H	3.52e-10	0.00	10 - 41000
11	H₂ + C₃⁺ → C₃H⁺ + H	2.40e-10	0.00	10 - 41000
12	HCN + C₃⁺ → C₃H⁺ + CN	2.60e-10	-0.50	10 - 41000
13	HCN + C₃⁺ → C₄N⁺ + H	1.04e-9	-0.50	10 - 41000
14	O₂ + C₃⁺ → C₃O⁺ + O	1.75e-10	0.00	10 - 41000

Variation of log fractional abundance (relative to H₂) with log time (years) in a dark cloud model. Ref. RATE12 paper.

C3+