CNO cycle
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The CNO cycle (for carbon–nitrogen–oxygen) is one of the two (known) sets of fusion reactions by which stars convert hydrogen to helium, the other being the proton–proton chain reaction. Unlike the latter, the CNO cycle is a catalytic cycle. Theoretical models[which?] show that the CNO cycle is the dominant source of energy in stars more massive than about 1.3 times the mass of the Sun.[1] The proton–proton chain is more important in stars the mass of the Sun or less. This difference stems from temperature dependency differences between the two reactions; pp-chain reactions start occurring at temperatures around 4×106 K[2] (4 megakelvins), making it the dominant energy source in smaller stars. A self-maintaining CNO chain starts occurring at approximately 15 MK, but its energy output rises much more rapidly with increasing temperatures.[1] At approximately 17 MK, the CNO cycle starts becoming the dominant source of energy.[3] The Sun has a core temperature of around 15.7 MK, and only 1.7% of 4He nuclei being produced in the Sun are born in the CNO cycle. The CNO-I process was independently proposed by Carl von Weizsäcker[4] and Hans Bethe[5] in 1938 and 1939, respectively.
In the CNO cycle, four protons fuse, using carbon, nitrogen and oxygen isotopes as a catalyst, to produce one alpha particle, two positrons and two electron neutrinos. Although there are various paths and catalysts involved in the CNO cycles, simply speaking all these cycles have the same net result:
- 4 1
1H + 2 e− → 4
2He + 2 e+ + 2 e− + 2 ν
e + 3 γ + 24.7 MeV → 4
2He + 2 ν
e + 3 γ + 26.7 MeV
Cold CNO cycles
Under typical conditions found in stellar plasmas, catalytic hydrogen burning by the CNO cycles is limited by proton captures. Specifically, the timescale for beta decay of radioactive nuclei produced is faster than the timescale for fusion. Because of the long timescales involved, the cold CNO cycles convert hydrogen to helium slowly, allowing them to power stars in quiescent equilibrium for many years.CNO-I
The first proposed catalytic cycle for the conversion of hydrogen into helium was at first simply called the carbon–nitrogen cycle (CN cycle), also honorarily referred to as the Bethe–Weizsäcker cycle, because it does not involve a stable isotope of oxygen. Bethe's original calculations suggested the CN-cycle was the Sun's primary source of energy, owing to the belief at the time that the Sun's composition was 10% nitrogen;[5] the solar abundance of nitrogen is now known to be less than half a percent. This cycle is now recognized as the first part of the larger CNO nuclear burning network.The main reactions of the CNO-I cycle are 12
6C→13
7N→13
6C→14
7N→15
8O→15
7N→12
6C:[6]
-
12
6C+ 1
1H→ 13
7N+ γ + 1.95 MeV 13
7N→ 13
6C+ e+ + ν
e+ 1.20 MeV (half-life of 9.965 minutes[7]) 13
6C+ 1
1H→ 14
7N+ γ + 7.54 MeV 14
7N+ 1
1H→ 15
8O+ γ + 7.35 MeV 15
8O→ 15
7N+ e+ + ν
e+ 1.73 MeV (half-life of 122.24 seconds[7]) 15
7N+ 1
1H→ 12
6C+ 4
2He+ 4.96 MeV
The limiting (slowest) reaction in the CNO-I cycle is the proton capture on 14
7N; it was recently experimentally measured down to stellar energies, revising the calculated age of globular clusters by around 1 billion years.[9]
The neutrinos emitted in beta decay will have a spectrum of energy ranges, because although momentum is conserved, the momentum can be shared in any way between the positron and neutrino, with either being emitted at rest and the other taking away the full energy, or anything in between, so long as all the energy from the Q-value is used. All momentum which get the electron and the neutrino together is not great enough to cause a significant recoil of the much heavier daughter nucleus and hence, its contribution to kinetic energy of the products, for the precision of values given here, can be neglected. Thus the neutrino emitted during the decay of nitrogen-13 can have an energy from zero up to 1.20 MeV, and the neutrino emitted during the decay of oxygen-15 can have an energy from zero up to 1.73 MeV. On average, about 1.7 MeV of the total energy output is taken away by neutrinos for each loop of the cycle, leaving about 25 MeV available for producing luminosity.[10]
CNO-II
In a minor branch of the reaction, occurring in the Sun's inner part, the core, just 0.04% of the time, the final reaction shown above does not produce carbon-12 and an alpha particle, but instead produces oxygen-16 and a photon and continues 157N→16
8O→17
9F→17
8O→14
7N→15
8O→15
7N:
-
15
7N+ 1
1H→ 16
8O+ γ + 12.13 MeV 16
8O+ 1
1H→ 17
9F+ γ + 0.60 MeV 17
9F→ 17
8O+ e+ + ν
e+ 2.76 MeV (half-life of 64.49 seconds) 17
8O+ 1
1H→ 14
7N+ 4
2He+ 1.19 MeV 14
7N+ 1
1H→ 15
8O+ γ + 7.35 MeV 15
8O→ 15
7N+ e+ + ν
e+ 2.75 MeV (half-life of 122.24 seconds)
CNO-III
This subdominant branch is significant only for massive stars. The reactions are started when one of the reactions in CNO-II results in fluorine-18 and gamma instead of nitrogen-14 and alpha, and continues 178O→18
9F→18
8O→15
7N→16
8O→17
9F→17
8O:
-
17
8O+ 1
1H→ 18
9F+ γ + 5.61 MeV 18
9F→ 18
8O+ e+ + ν
e+ 1.656 MeV (half-life of 109.771 minutes) 18
8O+ 1
1H→ 15
7N+ 4
2He+ 3.98 MeV 15
7N+ 1
1H→ 16
8O+ γ + 12.13 MeV 16
8O+ 1
1H→ 17
9F+ γ + 0.60 MeV 17
9F→ 17
8O+ e+ + ν
e+ 2.76 MeV (half-life of 64.49 seconds)
CNO-IV
Like the CNO-III, this branch is also only significant in massive stars. The reactions are started when one of the reactions in CNO-III results in fluorine-19 and gamma instead of nitrogen-15 and alpha, and continues 19
9F→16
8O→17
9F→17
8O→18
9F→18
8O→19
9F:
-
19
9F+ 1
1H→ 16
8O+ 4
2He+ 8.114 MeV 16
8O+ 1
1H→ 17
9F+ γ + 0.60 MeV 17
9F→ 17
8O+ e+ + ν
e+ 2.76 MeV (half-life of 64.49 seconds) 17
8O+ 1
1H→ 18
9F+ γ + 5.61 MeV 18
9F→ 18
8O+ e+ + ν
e+ 1.656 MeV (half-life of 109.771 minutes) 18
8O+ 1
1H→ 19
9F+ γ + 7.994 MeV
Hot CNO cycles
Under conditions of higher temperature and pressure, such as those found in novae and x-ray bursts, the rate of proton captures exceeds the rate of beta-decay, pushing the burning to the proton drip line. The essential idea is that a radioactive species will capture a proton more quickly than it can beta decay, opening new nuclear burning pathways that are otherwise inaccessible. Because of the higher temperatures involved, these catalytic cycles are typically referred to as the hot CNO cycles; because the timescales are limited by beta decays instead of proton captures, they are also called the beta-limited CNO cycles.HCNO-I
The difference between the CNO-I cycle and the HCNO-I cycle is that 137N captures a proton instead of decaying, leading to the total sequence 12
6C→13
7N→14
8O→14
7N→15
8O→15
7N→12
6C:
-
12
6C+ 1
1H→ 13
7N+ γ + 1.95 MeV 13
7N+ 1
1H→ 14
8O+ γ + 4.63 MeV 14
8O→ 14
7N+ e+ + ν
e+ 5.14 MeV (half-life of 70.641 seconds) 14
7N+ 1
1H→ 15
8O+ γ + 7.35 MeV 15
8O→ 15
7N+ e+ + ν
e+ 2.75 MeV (half-life of 122.24 seconds) 15
7N+ 1
1H→ 12
6C+ 4
2He+ 4.96 MeV
HCNO-II
The notable difference between the CNO-II cycle and the HCNO-II cycle is that 179F captures a proton instead of decaying, and helium is produced in a subsequent reaction on 18
9F, leading to the total sequence 15
7N→16
8O→17
9F→18
10Ne→18
9F→15
8O→15
7N:
-
15
7N+ 1
1H→ 16
8O+ γ + 12.13 MeV 16
8O+ 1
1H→ 17
9F+ γ + 0.60 MeV 17
9F+ 1
1H→ 18
10Ne+ γ + 3.92 MeV 18
10Ne→ 18
9F+ e+ + ν
e+ 4.44 MeV (half-life of 1.672 seconds) 18
9F+ 1
1H→ 15
8O+ 4
2He+ 2.88 MeV 15
8O→ 15
7N+ e+ + ν
e+ 2.75 MeV (half-life of 122.24 seconds)
HCNO-III
An alternative to the HCNO-II cycle is that 189F captures a proton moving towards higher mass and using the same helium production mechanism as the CNO-IV cycle as 18
9F→19
10Ne→19
9F→16
8O→17
9F→18
10Ne→18
9F:
-
18
9F+ 1
1H→ 19
10Ne+ γ + 6.41 MeV 19
10Ne→ 19
9F+ e+ + ν
e+ 3.32 MeV (half-life of 17.22 seconds) 19
9F+ 1
1H→ 16
8O+ 4
2He+ 8.11 MeV 16
8O+ 1
1H→ 17
9F+ γ + 0.60 MeV 17
9F+ 1
1H→ 18
10Ne+ γ + 3.92 MeV 18
10Ne→ 18
9F+ e+ + ν
e+ 4.44 MeV (half-life of 1.672 seconds)
Use in astronomy
While the total number of "catalytic" CNO nuclei are conserved in the cycle, in stellar evolution the relative proportions of the nuclei are altered. When the cycle is run to equilibrium, the ratio of the carbon-12/carbon-13 nuclei is driven to 3.5, and nitrogen-14 becomes the most numerous nucleus, regardless of initial composition. During a star's evolution, convective mixing episodes bring material in which the CNO cycle has operated from the star's interior to the surface, altering the observed composition of the star. Red giant stars are observed to have lower carbon-12/carbon-13 and carbon-12/nitrogen-14 ratios than main sequence stars, which is considered to be convincing evidence for the operation of the CNO cycle.[citation needed]The presence of the heavier elements carbon, nitrogen and oxygen places an upper bound of approximately 150 solar masses on the maximum size of massive stars.[citation needed] It is thought[by whom?] that the "metal-poor" early universe could have had stars, called Population III stars, up to 250 solar masses without interference from the CNO cycle at the beginning of their lifetime.