Actinides in the environment
Actinides in the environment refer to the sources, environmental behaviour and effects of actinides in Earth's environment. Environmental radioactivity is not limited solely to actinides; non-actinides such as radon and radium are of note.
- 1 Inhalation versus ingestion
- 2 Thorium in the environment
- 3 Uranium in the environment
- 4 Neptunium in the environment
- 5 Plutonium in the environment
- 6 Americium in the environment
- 7 See also
- 8 References
- 9 Further reading
- 10 External links
Inhalation versus ingestion
Generally, ingested insoluble actinide compounds such as high-fired uranium dioxide and mixed oxide (MOX) fuel will pass through the digestive system with little effect since they cannot dissolve and be absorbed by the body. Inhaled actinide compounds, however, will be more damaging as they remain in the lungs and irradiate the lung tissue.
Ingested Low-fired oxides and soluble salts such as nitrate can be absorbed into the blood stream. If they are inhaled then it is possible for the solid to dissolve and leave the lungs. Hence the dose to the lungs will be lower for the soluble form.
Thorium in the environment
In India, a large amount of thorium ore can be found in the form of monazite in placer deposits of the Western and Eastern coastal dune sands, particularly in the Tamil Nadu coastal areas. The residents of this area are exposed to a naturally occurring radiation dose ten times higher than the worldwide average.
Thorium is found at low levels in most rocks and soils, where it is about three times more abundant than uranium, and is about as common as lead. Soil commonly contains an average of around 6 parts per million (ppm) of thorium. Thorium occurs in several minerals, the most common being the rare earth-thorium-phosphate mineral, monazite, which contains up to about 12% thorium oxide. There are substantial deposits in several countries. 232Th decays very slowly (its half-life is about three times the age of the earth) but other thorium isotopes occur in the thorium and uranium decay chains. Most of these are short-lived and hence much more radioactive than 232Th, though on a mass basis they are negligible.
Effects in humans
Thorium has been linked to liver cancer. In the past thoria (thorium dioxide) was used as a contrast agent for medical X-ray radiography but its use has been discontinued. It was sold under the name Thorotrast.
Uranium in the environment
Uranium is a natural metal which is widely found. It is present in almost all soils and it is more plentiful than antimony, beryllium, cadmium, gold, mercury, silver, or tungsten and is about as abundant as arsenic or molybdenum. Significant concentrations of uranium occur in some substances such as phosphate rock deposits, and minerals such as lignite, and monazite sands in uranium-rich ores (it is recovered commercially from these sources).
Seawater contains about 3.3 parts per billion of uranium by weight as uranium(VI) forms soluble carbonate complexes. The extraction of uranium from seawater has been considered as a means of obtaining the element. Because of the very low specific activity of uranium the chemical effects of it upon living things can often outweigh the effects of its radioactivity. Additional uranium has been added to the environment in some locations as a result of the nuclear fuel cycle and the use of depleted uranium in munitions.
Neptunium in the environment
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Like plutonium, neptunium has a high affinity for soil. However, it is relatively mobile over the long term, and diffusion of neptunium-237 in groundwater is a major issue in designing a deep geological repository for permanent storage of spent nuclear fuel. 237Np has a halflife of 2.144 million years, so it is a long-term problem; but its halflife is still much shorter than those of uranium-238, uranium-235, or uranium-236, and 237Np therefore has higher specific activity than those nuclides.
Plutonium in the environment
Plutonium in the environment has several sources. These include:
- Atomic batteries
- In space
- In pacemakers
- Bomb detonations
- Bomb safety trials
- Nuclear accidents (such as Chernobyl)
- Nuclear crime
- Nuclear fuel cycle
Plutonium, like other actinides, readily forms a plutonium dioxide (plutonyl) core (PuO2). In the environment, this plutonyl core readily complexes with carbonate as well as other oxygen moieties (OH−, NO2−, NO3−, and SO42−) to form charged complexes which can be readily mobile with low affinities to soil.
PuO2 formed from neutralizing highly acidic nitric acid solutions tends to form polymeric PuO2 which is resistant to complexation. Plutonium also readily shifts valences between the +3, +4, +5 and +6 states. It is common for some fraction of plutonium in solution to exist in all of these states in equilibrium.
Plutonium is known to bind to soil particles very strongly, see above for a X-ray spectroscopic study of plutonium in soil and concrete. While caesium has very different chemistry to the actinides, it is well known that both caesium and many of the actinides bind strongly to the minerals in soil. Hence it has been possible to use 134Cs labeled soil to study the migration of Pu and Cs is soils. It has been shown that colloidal transport processes control the migration of Cs (and will control the migration of Pu) in the soil at the Waste Isolation Pilot Plant.
Americium in the environment
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In France a truck transporting 900 smoke detectors had been reported to have caught fire, it is claimed that this led to a release of americium into the environment. In the U.S., the "Radioactive Boy Scout" David Hahn was able to buy thousands of smoke detectors at remainder prices and concentrate the americium from them.
There have been cases of humans being contaminated with americium, the worst case being that of Harold McCluskey. It is interesting to note that Harold McCluskey did not die of cancer but of heart disease (which he had before the accident). It is likely that the medical care which he was given saved his life; because of the difference in the chemistry of americium (the +3 oxidation state is very stable) to plutonium (where the +4 state can form in the human body) the americium has very different biochemistry to plutonium.
The most common isotope americium-241 decays (half-life of 431 years) to neptunium-237 which has a much longer half-life, so in the long term, the issues discussed above for neptunium apply.
B.E. Burakov, M.I Ojovan,W.E. Lee. Crystalline Materials for Actinide Immobilisation, Imperial College Press, London, 198 pp. (2010). http://www.icpress.co.uk/engineering/p652.html
- "Compendium Of Policy And Statutory Provisions Relating To Exploitation Of Beach Sand Minerals". Government Of India. Archived from the original on 4 December 2008. Retrieved 2008-12-19.
- THORIUM Agency for Toxic Substances and Disease Registry. July 1999.
- "Uranium: the essentials". WebElements. Retrieved 2008-12-19.
- "Neptunium" (PDF). Argonne National Laboratory, EVS. August 2005. Archived (PDF) from the original on 19 December 2008. Retrieved 2008-12-19.
- Whicker, R.D.; S.A. Ibrahim (2006). "Vertical migration of 134Cs bearing soil particles in arid soils: implications for plutonium redistribution.". Journal of Environmental Radioactivity 88 (2): 171–188. PMID 16564117. doi:10.1016/j.jenvrad.2006.01.010.
- "Radiological Agent: Americium-241". CBWInfo.com. Archived from the original on 8 January 2009. Retrieved 2008-12-19.
- Hala, Jiri, and James D. Navratil. Radioactivity, Ionizing Radiation and Nuclear Energy. Konvoj: Brno, Czech Republic, 2003. ISBN 80-7302-053-X.
- Royal Society for Chemistry - Why do mechanisms matter in radioactive waste management?
- Federation of American Scientists - Spectroscopies for Environmental Studies of Actinide Species