Actinides in the environment

The actinide series is a group of chemical elements with atomic numbers ranging from 89 to 102,[note 1] including notable elements such as uranium and plutonium. The nuclides (or isotopes) thorium-232, uranium-235, and uranium-238 occur primordially, while trace quantities of actinium, protactinium, neptunium, and plutonium exist as a result of radioactive decay and (in the case of neptunium and plutonium) neutron capture of uranium.[note 2] These elements are far more radioactive than the naturally occurring thorium and uranium, and thus have much shorter half-lives. Elements with atomic numbers greater than 94 do not exist naturally on Earth, and must be produced in a nuclear reactor.[2] However, certain isotopes of elements up to californium (atomic number 98) still have practical applications which take advantage of their radioactive properties.[3][4]

While all actinides are radioactive, actinides and actinide compounds comprise a significant portion of the Earth's crust.[5] There is enough thorium and uranium to be commercially mined, with thorium having a concentration in the Earth's crust about four times that of uranium.[6] The global production of uranium in 2021 was over six million tons, with Australia having been the leading supplier.[7] Thorium is extracted as a byproduct of titanium, zirconium, tin, and rare earths from monazite, from which thorium is often a waste product. Despite its greater abundance in the Earth's crust, the low demand for thorium in comparison to other metals extracted alongside thorium has led to a global surplus.[8]

The primary hazard associated with actinides is their radioactivity, though they may also cause heavy metal poisoning if absorbed into the bloodstream.[9] Generally, ingested insoluble actinide compounds, such as uranium dioxide and mixed oxide (MOX) fuel, will pass through the digestive tract with little effect since they have long half-lives, and cannot dissolve and be absorbed into the bloodstream.[10] Inhaled actinide compounds, however, will be more damaging as they remain in the lungs and irradiate lung tissue.


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  1. ^ Wu, Yang; Dai, Xiongxin; Xing, Shan; Luo, Maoyi; Christl, Marcus; Synal, Hans-Arno; Hou, Shaochun (2022). "Direct search for primordial 244Pu in Bayan Obo bastnaesite". Chinese Chemical Letters. 33 (7): 3522–3526. doi:10.1016/j.cclet.2022.03.036. Retrieved 29 January 2024.
  2. ^ Seaborg, Glenn T.; Segrè, Emilio (June 1947). "THE TRANS-URANIUM ELEMENTS". Nature. 159 (4052): 863–865. doi:10.1038/159863a0.
  3. ^ "Americium in Ionization Smoke Detectors". www.epa.gov. Environmental Protection Agency. 27 November 2018.
  4. ^ Ellis, Jason K. "ORNL's californium-252 will play pivotal role in new reactor startups | ORNL". www.ornl.gov. Oak Ridge National Laboratory.
  5. ^ Herring, J. Stephen (2012). Encyclopedia of sustainability science and technology. New York: Springer. p. 11202. ISBN 978-0-387-89469-0.
  6. ^ Herring, p. 11203
  7. ^ "Uranium Mining Overview - World Nuclear Association". world-nuclear.org. World Nuclear Association.
  8. ^ Herring, pp. 11204-11205
  9. ^ Briner, Wayne (25 January 2010). "The Toxicity of Depleted Uranium". International Journal of Environmental Research and Public Health. 7 (1): 303–313. doi:10.3390/ijerph7010303.{{cite journal}}: CS1 maint: unflagged free DOI (link)
  10. ^ Keith, S; Faroon, O; Roney, N; Scinicariello, F; Wilbur, S; Ingerman, L; Llados, F; Plewak, D; Wohlers, D; Diamond, G (February 2013). "Toxicological Profile for Uranium". National Library of Medicine. PMID 24049861.

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