Neutron flux

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The neutron flux, is a scalar quantity used in nuclear physics and nuclear reactor physics. It is the total distance travelled by all free neutrons per unit time and volume. [1] Equivalently, it can be defined as the number of neutrons travelling through a small sphere of radius in a time interval, divided by a maximal cross section of the sphere (the great disk area, ) and by the duration of the time interval. [2] : 82-83 The dimension of neutron flux is and the usual unit is cm−2s−1 (reciprocal square centimetre times reciprocal second).

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The neutron fluence is defined as the neutron flux integrated over a certain time period. So its dimension is and its usual unit is cm−2 (reciprocal square centimetre). An older term used instead of cm−2 was "n.v.t." (neutrons, velocity, time). [3]

Natural neutron flux

Neutron flux in asymptotic giant branch stars and in supernovae is responsible for most of the natural nucleosynthesis producing elements heavier than iron. In stars there is a relatively low neutron flux on the order of 105 to 1011 cm−2 s−1, resulting in nucleosynthesis by the s-process (slow neutron-capture process). By contrast, after a core-collapse supernova, there is an extremely high neutron flux, on the order of 1032 cm−2 s−1, [4] resulting in nucleosynthesis by the r-process (rapid neutron-capture process).

Earth atmospheric neutron flux, apparently from thunderstorms, can reach levels of 3·10−2 to 9·10+1 cm−2 s−1. [5] [6] However, recent results [7] (considered invalid by the original investigators [8] ) obtained with unshielded scintillation neutron detectors show a decrease in the neutron flux during thunderstorms. Recent research appears to support lightning generating 1013–1015 neutrons per discharge via photonuclear processes. [9]

Artificial neutron flux

Artificial neutron flux refers to neutron flux which is man-made, either as byproducts from weapons or nuclear energy production or for a specific application such as from a research reactor or by spallation. A flow of neutrons is often used to initiate the fission of unstable large nuclei. The additional neutron(s) may cause the nucleus to become unstable, causing it to decay (split) to form more stable products. This effect is essential in fission reactors and nuclear weapons.

Within a nuclear fission reactor, the neutron flux is the primary quantity measured to control the reaction inside. The flux shape is the term applied to the density or relative strength of the flux as it moves around the reactor. Typically the strongest neutron flux occurs in the middle of the reactor core, becoming lower toward the edges. The higher the neutron flux the greater the chance of a nuclear reaction occurring as there are more neutrons going through an area per unit time.

Reactor vessel wall neutron fluence

A reactor vessel of a typical nuclear power plant (PWR) endures in 40 years (32 full reactor years) of operation approximately 6.5×1019 cm−2 (E > 1 MeV) of neutron fluence. [10] Neutron flux causes reactor vessels to suffer from neutron embrittlement.

See also

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References

  1. Stamm'ler, Rudi J. J.; Abbate, Máximo Julio (1 July 1983). Methods of Steady-State Reactor Physics in Nuclear Design (1st ed.). Academic Press. ISBN   978-0126633207. LCCN   82072342. OCLC   9915614. OL   3512075M.
  2. Beckurts, Karl-Heinrich; Wirtz, Karl (1964). "5.1.1 Neutron Flux, Neutron Density, and Neutron Current" . Neutron Physics . Translated by Dresner, L. (1st ed.). Springer-Verlang. ISBN   978-3540030966. LCCN   64025646. OCLC   569910840. OL   27986790M via Internet Archive.
  3. M. F. Kaplan (August 1983). Nuclear Radiation and the Properties of Concrete (PDF). University of Cape Town. p. 2. Retrieved 14 September 2022.
  4. Burbidge, E. Margaret; Burbidge, G. R.; Fowler, William A.; Hoyle, F. (October 1957). "Synthesis of the Elements in Stars". Reviews of Modern Physics. 29 (4): 548–650. Bibcode:1957RvMP...29..547B. doi: 10.1103/RevModPhys.29.547 .
  5. Gurevich, A. V.; Antonova, V. P. (2012). "Strong Flux of Low-Energy Neutrons Produced by Thunderstorms". Physical Review Letters. American Physical Society. 108 (12): 125001. Bibcode:2012PhRvL.108l5001G. doi:10.1103/PhysRevLett.108.125001. PMID   22540588.
  6. Gurevich, A. V.; Almenova, A. M. (2016). "Observations of high-energy radiation during thunderstorms at Tien-Shan". Physical Review D. American Physical Society. 94 (2): 023003. Bibcode:2016PhRvD..94b3003G. doi:10.1103/PhysRevD.94.023003.
  7. Alekseenko, V.; Arneodo, F.; Bruno, G.; Di Giovanni, A.; Fulgion, W.; Gromushkin, D.; Shchegolev, O.; Stenkin, Yu.; Stepanov, V.; Sulakov, V.; Yashin, I. (2015). "Decrease of Atmospheric Neutron Counts Observed during Thunderstorms". Physical Review Letters. American Physical Society. 114 (12): 125003. Bibcode:2015PhRvL.114l5003A. doi:10.1103/PhysRevLett.114.125003. PMID   25860750.
  8. Gurevich, A. V.; Ptitsyn, M. O. (2015). "Comment on "Decrease of Atmospheric Neutron Counts Observed during Thunderstorms"". Physical Review Letters. American Physical Society. 115 (12): 179501. Bibcode:2015PhRvL.115q9501G. doi:10.1103/PhysRevLett.115.179501. PMID   26551144.
  9. Köhn, Christoph; Diniz, Gabriel; Harakeh, GMushin (2017). "Production mechanisms of leptons, photons, and hadrons and their possible feedback close to lightning leaders". Journal of Geophysical Research: Atmospheres. American Geophysical Union. 122 (2): 1366. Bibcode:2017JGRD..122.1365K. doi:10.1002/2016JD025445. PMC   5349290 . PMID   28357174.
  10. Nuclear Power Plant Borssele Reactor Pressure Vessel Safety Assessment, p. 29, 5.6 Neutron Fluence Calculation.