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carbon-nitrogen cycle

 
American Heritage Dictionary:

car·bon-ni·tro·gen cycle

(kär'bən-nī'trə-jən)
n.
A chain of thermonuclear reactions in which nitrogen isotopes are formed in intermediate stages and carbon acts essentially as a catalyst to convert four hydrogen atoms into one helium atom with the emission of two positrons. The entire sequence is thought to generate significant amounts of energy in the sun and certain other stars. Also called carbon cycle, nitrogen cycle.


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Circulation of nitrogen in various forms throughout nature. Nitrogen is essential to life, but in the atmosphere it is in a form (the diatomic molecule N2) unavailable to most organisms. Nitrogen fixation by microbes turns this nitrogen into nitrates and other compounds, which plants or algae assimilate into their tissues. Animals that eat plants in turn incorporate the compounds into their own tissues. Microbes decompose the remains and waste of all living things into ammonia (ammonification); the ammonia may leave the soil through vaporization into the air or leaching into water. Ammonia remaining in soil may be transformed by bacteria into nitrates (nitrification), which then can be reassimilated into living organisms, or into free nitrogen (denitrification), which reenters the atmosphere. Hence, once fixed from air, some nitrogen goes through the cycle repeatedly without returning to the gaseous state.

For more information on nitrogen cycle, visit Britannica.com.

Columbia Encyclopedia:

nitrogen cycle

Top
nitrogen cycle, the continuous flow of nitrogen through the biosphere by the processes of nitrogen fixation, ammonification (decay), nitrification, and denitrification. Nitrogen is vital to all living matter, both plant and animal; it is an essential constituent of amino acids, which form proteins of nucleic acids, and of many other organic materials.

Nitrogen Fixation

Although the earth's atmosphere is 78% nitrogen, free gaseous nitrogen cannot be utilized by animals or by higher plants. They depend instead on nitrogen that is present in the soil. To enter living systems, nitrogen must be "fixed" (combined with oxygen or hydrogen) into compounds that plants can utilize, such as nitrates or ammonia. A certain amount of atmospheric nitrogen is fixed by lightning and by some cyanobacteria (blue-green algae). But the great bulk of nitrogen fixation is performed by soil bacteria of two kinds: those that live free in the soil and those that live enclosed in nodules in the roots of certain leguminous plants (e.g., alfalfa, peas, beans, clover, soybeans, and peanuts). Among the free-living forms are species of Clostridium, discovered c.1893 by Sergei Winogradsky, and Azotobacter, discovered c.1901 by M. W. Beijerinck. Both Clostridium and Azotobacter are generally present in agricultural soils, and both are saprophytes, i.e., they use the energy from decaying organic matter in the soil to fuel soil processes, including nitrogen fixation.

Bacteria that live in the roots of legumes are of the genus Rhizobium, first isolated c.1888 by Beijerinck. These rod-shaped bacteria enter the roots chiefly through the root hairs and then work their way to the inner root tissues. There they stimulate the growth of tumorlike nodules. Within the nodules the bacteria develop into forms called bacteroids, which live in a symbiotic (mutually beneficial) relationship with the green plant. The bacteroids take carbohydrates from the plant for energy to fix nitrogen and synthesize amino acids; the plants take the amino acids elaborated in the nodule to build plant tissue. Animals in turn consume the plants and convert plant protein into animal protein. Rhizobia can be found free-living in the soil, but they cannot fix nitrogen in the free state, nor can the legume root fix nitrogen without Rhizobia.

The exact biochemistry of nitrogen fixation within the nodule is not yet understood. It is estimated that more than 300 lbs of nitrogen per acre (340 kg per hectare) can be fixed by fields of alfalfa and other legumes. After a harvest legume roots left in the soil decay, returning organic nitrogen compounds to the soil for uptake by the next generation of plants. For this reason crop rotation in which a leguminous crop is rotated with a nonleguminous one is a common practice for maintaining soil fertility.

Other Aspects of the Nitrogen Cycle

Decomposing animal remains and animal wastes also return organic nitrogen to the soil as ammonia. Many different kinds of decay microorganisms participate in ammonification. The nitrifying bacteria of the genus Nitrosomonas oxidize the ammonia to nitrites, and Nitrobacter oxidize the nitrites to nitrates. The nitrates can then be taken up again by the green plant. The cycle of fixation-decay-nitrification-fixation can proceed indefinitely without any nitrogen being returned to a gaseous state. But still another group of microorganisms, the denitrifying bacteria, can reduce nitrates all the way to molecular nitrogen. Denitrification occurs only in the absence of oxygen and is not common in well-cultivated soils.

Effects of Artificial Fixation

Nitrogen fixation can also be accomplished artificially by various methods (see nitrogen). Humans annually fix vast amounts of nitrogen for industrial purposes and for use as fertilizer. Unfortunately, large-scale legume cultivation and artificial fixation may be upsetting the natural nitrogen cycle in the biosphere. There is some question whether natural denitrification can keep pace with fixation. For one thing, run-off of nitrate fertilizer can cause eutrophication of lakes and streams (see water pollution) and can foul drinking supplies. Another environmental problem is that inorganic fertilizers tend to depress legume fixation. As a consequence, root tissue remaining after harvest is poorer, and thus more fertilizer must be applied the following year.



n.

A chain of thermonuclear reactions in which nitrogen isotopes are formed in intermediate stages and carbon acts essentially as a catalyst to convert four hydrogen atoms into one helium atom with the emission of two positrons. The entire sequence is thought to generate significant amounts of energy in the sun and certain other stars. Also called carbon cycle, nitrogen cycle.

Overview of the CNO-I Cycle

The CNO cycle (for carbonnitrogenoxygen) is one of two sets of fusion reactions by which stars convert hydrogen to helium, the other being the proton–proton chain. Unlike the proton–proton chain reaction, the CNO cycle is a catalytic cycle. Theoretical models 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. 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,[1] making it the dominant energy source in smaller stars. A self-maintaining CNO chain starts occurring at approximately 15×106 K, but its energy output rises much more rapidly with increasing temperatures.[2] At approximately 17×106 K, the CNO cycle starts becoming the dominant source of energy.[3] The Sun has a core temperature of around 15.7×106 K and only 1.7% of 4
He
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
1
H
 →  4
2
He
 +  2 e+
 +  2 ν
e
 +  3 γ  +  26.8 MeV

The positrons will almost instantly annihilate with electrons, releasing energy in the form of gamma rays. The neutrinos escape from the star carrying away some energy. The carbon, nitrogen, and oxygen isotopes are in effect one nucleus that goes through a number of transformations in an endless loop.

Contents

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 is 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
6
C
13
7
N
13
6
C
14
7
N
15
8
O
15
7
N
12
6
C
:[6]

12
6
C
 
1
1
H
 
→  13
7
N
 
γ      1.95 MeV
13
7
N
 
    →  13
6
C
 
e+
 
ν
e
 
1.20 MeV (half-life of 9.965 minutes)
13
6
C
 
1
1
H
 
→  14
7
N
 
γ      7.54 MeV
14
7
N
 
1
1
H
 
→  15
8
O
 
γ      7.35 MeV
15
8
O
 
    →  15
7
N
 
e+
 
ν
e
 
1.73 MeV (half-life of 122.24 seconds)
15
7
N
 
1
1
H
 
→  12
6
C
 
4
2
He
 
    4.96 MeV

where the Carbon-12 nucleus used in the first reaction is regenerated in the last reaction. After the two positrons emitted annihilate with two ambient electrons producing an additional 2.04 MeV, the total energy released in one cycle is 26.73 MeV; it should be noted that in some texts, authors are erroneously including the positron annihilation energy in with the beta-decay Q-value and then neglecting the equal amount of energy released by annihilation, leading to possible confusion. All values are calculated with reference to the Atomic Mass Evaluation 2003.[7]

The limiting (slowest) reaction in the CNO-I cycle is the proton capture on 14
7
N
; it was recently experimentally measured down to stellar energies, revising the calculated age of globular clusters by around 1 billion years.[8]

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. Because the mass of the electron and neutrino are much less than the mass of the daughter nucleus, for the precision of values given here, the recoil of the nucleus 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.[9]

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 15
7
N
16
8
O
17
9
F
17
8
O
14
7
N
15
8
O
15
7
N
:

15
7
N
 
1
1
H
 
→  16
8
O
 
γ      12.13 MeV
16
8
O
 
1
1
H
 
→  17
9
F
 
γ      0.60 MeV
17
9
F
 
    →  17
8
O
 
e+
 
ν
e
 
2.76 MeV (half-life of 64.49 seconds)
17
8
O
 
1
1
H
 
→  14
7
N
 
4
2
He
 
    1.19 MeV
14
7
N
 
1
1
H
 
→  15
8
O
 
γ      7.35 MeV
15
8
O
 
    →  15
7
N
 
e+
 
ν
e
 
2.75 MeV (half-life of 122.24 seconds)

Like the carbon, nitrogen, and oxygen involved in the main branch, the fluorine produced in the minor branch is merely catalytic and at steady state, does not accumulate in the star.

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 17
8
O
18
9
F
18
8
O
15
7
N
16
8
O
17
9
F
17
8
O
:

17
8
O
 
1
1
H
 
→  18
9
F
 
γ      5.61 MeV
18
9
F
 
    →  18
8
O
 
e+
 
ν
e
 
1.656 MeV (half-life of 109.771 minutes)
18
8
O
 
1
1
H
 
→  15
7
N
 
4
2
He
 
    3.98 MeV
15
7
N
 
1
1
H
 
→  16
8
O
 
γ      12.13 MeV
16
8
O
 
1
1
H
 
→  17
9
F
 
γ      0.60 MeV
17
9
F
 
    →  17
8
O
 
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
9
F
16
8
O
17
9
F
17
8
O
18
9
F
18
8
O
19
9
F
:

19
9
F
 
1
1
H
 
→  16
8
O
 
4
2
He
 
    8.114 MeV
16
8
O
 
1
1
H
 
→  17
9
F
 
γ      0.60 MeV
17
9
F
 
    →  17
8
O
 
e+
 
ν
e
 
2.76 MeV (half-life of 64.49 seconds)
17
8
O
 
1
1
H
 
→  18
9
F
 
γ      5.61 MeV
18
9
F
 
    →  18
8
O
 
e+
 
ν
e
 
1.656 MeV (half-life of 109.771 minutes)
18
8
O
 
1
1
H
 
→  19
9
F
 
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 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 13
7
N
captures a proton instead of decaying, leading to the total sequence 12
6
C
13
7
N
14
8
O
14
7
N
15
8
O
15
7
N
12
6
C
:

12
6
C
 
1
1
H
 
→  13
7
N
 
γ      1.95 MeV
13
7
N
 
1
1
H
 
→  14
8
O
 
γ      4.63 MeV
14
8
O
 
    →  14
7
N
 
e+
 
ν
e
 
5.14 MeV (half-life of 70.641 seconds)
14
7
N
 
1
1
H
 
→  15
8
O
 
γ      7.35 MeV
15
8
O
 
    →  15
7
N
 
e+
 
ν
e
 
2.75 MeV (half-life of 122.24 seconds)
15
7
N
 
1
1
H
 
→  12
6
C
 
4
2
He
 
    4.96 MeV

HCNO-II

The notable difference between the CNO-II cycle and the HCNO-II cycle is that 17
9
F
captures a proton instead of decaying, and helium is produced in a subsequent reaction on 18
9
F
, leading to the total sequence 15
7
N
16
8
O
17
9
F
18
10
Ne
18
9
F
15
8
O
15
7
N
:

15
7
N
 
1
1
H
 
→  16
8
O
 
γ      12.13 MeV
16
8
O
 
1
1
H
 
→  17
9
F
 
γ      0.60 MeV
17
9
F
 
1
1
H
 
→  18
10
Ne
 
γ      3.92 MeV
18
10
Ne
 
    →  18
9
F
 
e+
 
ν
e
 
4.44 MeV (half-life of 1.672 seconds)
18
9
F
 
1
1
H
 
→  15
8
O
 
4
2
He
 
    2.88 MeV
15
8
O
 
    →  15
7
N
 
e+
 
ν
e
 
2.75 MeV (half-life of 122.24 seconds)

HCNO-III

An alternative to the HCNO-II cycle is that 18
9
F
captures a proton moving towards higher mass and using the same helium production mechanism as the CNO-IV cycle as 18
9
F
19
10
Ne
19
9
F
16
8
O
17
9
F
18
10
Ne
18
9
F
:

18
9
F
 
1
1
H
 
→  19
10
Ne
 
γ      6.41 MeV
19
10
Ne
 
    →  19
9
F
 
e+
 
ν
e
 
17.22 MeV (half-life of 122.24 seconds)
19
9
F
 
1
1
H
 
→  16
8
O
 
4
2
He
 
    8.114 MeV
16
8
O
 
1
1
H
 
→  17
9
F
 
γ      0.60 MeV
17
9
F
 
1
1
H
 
→  18
10
Ne
 
γ      3.92 MeV
18
10
Ne
 
    →  18
9
F
 
e+
 
ν
e
 
4.44 MeV (half-life of 1.672 seconds)

Use in astronomy

While the total number of "catalytic" CNO nuclei is 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.

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[who?] 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.

See also

References

  1. ^ Reid, I. Neill; Suzanne L., Hawley (2005), New light on dark stars: red dwarfs, low-mass stars, brown dwarfs, Springer-Praxis books in astrophysics and astronomy (2nd ed.), Springer, p. 108, ISBN 3540251243, http://books.google.com/books?id=o7pe7Fp4JaAC&pg=PA108 
  2. ^ Salaris, Maurizio; Cassisi, Santi (2005), Evolution of stars and stellar populations, John Wiley and Sons, pp. 119–121, ISBN 0470092203, http://books.google.com/books?id=p4ojTNkcFx8C&pg=PA119 
  3. ^ Schuler, S. C.; King, J. R.; The, L.-S. (2009). "Stellar Nucleosynthesis in the Hyades Open Cluster". The Astrophysical Journal 701 (1): 837–849. arXiv:0906.4812. Bibcode 2009ApJ...701..837S. doi:10.1088/0004-637X/701/1/837. 
  4. ^ von Weizsäcker, C. F. (1938). "Über Elementumwandlungen in Innern der Sterne II". Physikalische Zeitschrift 39: 633–46. 
  5. ^ a b Bethe, H. A. (1939). "Energy Production in Stars". Physical Review 55 (5): 434–56. Bibcode 1939PhRv...55..434B. doi:10.1103/PhysRev.55.434. 
  6. ^ Krane, K. S. (1988). Introductory Nuclear Physics. John Wiley & Sons. p. 537. ISBN 0-471-80553-X. 
  7. ^ Wapstra, Aaldert; Audi, Georges (18 November 2003). "The 2003 Atomic Mass Evaluation". Atomic Mass Data Center. http://amdc.in2p3.fr/web/masseval.html. Retrieved 25 October 2011. 
  8. ^ LUNA Collaboration; Lemut, A.; Bemmerer, D.; Confortola, F.; Bonetti, R.; Broggini, C.; Corvisiero, P.; Costantini, H. et al. (2006). "First measurement of the 14N(p,gamma)15O cross section down to 70 keV". Physics Letters B 634: 483–487. arXiv:nucl-ex/0602012. Bibcode 2006PhLB..634..483L. doi:10.1016/j.physletb.2006.02.021. 
  9. ^ Scheffler, Helmut; Elsässer, Hans (1990). Die Physik der Sterne und der Sonne. Bibliographisches Institut (Mannheim, Wien, Zürich). ISBN 3-411-14172-7. 

Further reading


 
 

 

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