Radon
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For other uses, see Radon (disambiguation).
86 astatine ← radon → francium
Xe
↑
Rn
↓
Uuo
Periodic Table - Extended Periodic Table
General
Name, Symbol, Number radon, Rn, 86
Chemical series noble gases
Group, Period, Block 18, 6, p
Appearance colorless
Standard atomic weight (222) g·mol−1
Electron configuration [Xe] 4f14 5d10 6s2 6p6
Electrons per shell 2, 8, 18, 32, 18, 8
Physical properties
Phase gas
Density (0 °C, 101.325 kPa)
9.73 g/L
Melting point 202 K
(-71.15 °C, -96 °F)
Boiling point 211.3 K
(-61.85 °C, -79.1 °F)
Critical point 377 K, 6.28 MPa
Heat of fusion 3.247 kJ·mol−1
Heat of vaporization 18.10 kJ·mol−1
Heat capacity (25 °C) 20.786 J·mol−1·K−1
Vapor pressure P(Pa) 1 10 100 1 k 10 k 100 k
at T(K) 110 121 134 152 176 211
Atomic properties
Crystal structure cubic face centered
Oxidation states 0
Electronegativity no data (scale Pauling)
Ionization energies 1st: 1037 kJ/mol
Atomic radius (calc.) 120 pm
Covalent radius 145 pm
Miscellaneous
Magnetic ordering non-magnetic
Thermal conductivity (300 K) 3.61 m W·m−1·K−1
CAS registry number 10043-92-2
Selected isotopes
Main article: Isotopes of radon iso NA half-life DM DE (MeV) DP
211Rn syn 14.6 h Epsilon 2.892 211At
Alpha 5.965 207Po
222Rn 100% 3.824 d Alpha 5.590 218Po
References
Radon (IPA: /ˈreɪdɒn/) is a chemical element that has the symbol Rn and atomic number 86. A radioactive noble gas that is formed by the decay of radium, radon is one of the heaviest gases and is considered to be a health hazard. The most stable isotope is 222Rn which has a half-life of 3.8 days and is used in radiotherapy. Radon is a significant contaminant that affects indoor air quality worldwide. Radon gas from natural sources can accumulate in buildings and reportedly causes 21,000 lung cancer deaths per year in the United States alone[2].
Contents [hide]
1 Notable characteristics
2 Applications
2.1 Radon therapy
2.2 Hydrologic studies
2.3 Geologic studies
2.4 Atmospheric studies
3 History
4 Occurrence
5 Compounds
6 Isotopes
7 Health Effects and Epidemiology
8 Testing and mitigation
9 Radon therapy
10 References
10.1 Other references
11 Notable Radon Researchers and Scientists
12 External links
[edit] Notable characteristics
Essentially chemically inert, but radioactive, radon is the heaviest noble gas and one of the heaviest gases at room temperature. At standard temperature and pressure radon is a colorless gas, but when it is cooled below its freezing point (202 K ; -71 °C ; -96 °F) it has a brilliant phosphorescence which turns yellow as the temperature is lowered, and becomes orange-red at the temperatures air liquefies (below 93 K ; -180 °C).
Natural radon concentrations in Earth's atmosphere are so low that radon-rich water in contact with the atmosphere will continually lose radon by volatilization. Hence, ground water has a higher concentration of 222Rn than surface water, because it is continuously produced by radiocative decay of 226Ra present in rocks. Likewise, the saturated zone of a soil frequently has a higher radon content than the unsaturated zone due to diffusional losses to the atmosphere.
[edit] Applications
[edit] Radon therapy
In the United States and Europe there are a few "radon spas," where people sit for minutes or hours in a high-radon atmosphere in the belief that airborne radiation will invigorate or energize them. The same applies to the hot water spas of Misasa, Tottori, Japan, where water is naturally rich in radium and exhales radon. However, there is no scientific evidence for this belief, nor any known biological mechanism by which such an effect could occur. In addition, it conflicts with the internationally recognized standard that there is no safe threshold for radiation exposure (see Linear no-threshold model) and that exposure should be limited to that "as low as reasonably acheivable" (ALARA).
Radon accumulates in underground mines and caves. Good ventilation should therefore be maintained in mines, and in some countries, guides in tourist caves are classified as "radiation workers", whose time of exposure is monitored. Tourism of caves is not generally considered a significant hazard for the relatively brief visits by members of the general public.
Although some physicians once believed that radon can be used therapeutically, there is no evidence for this belief and radon is not currently in medical use, at least in the developed world.
[edit] Hydrologic studies
Because of radon's rapid loss to air and comparatively rapid decay, radon is used in hydrologic research that studies the interaction between ground water, streams and rivers. Any significant concentration of radon in a stream or river is a good indicator that there are local inputs of ground water.
[edit] Geologic studies
Some researchers have looked at elevated soil-gas radon concentrations, or rapid changes in soil radon concentrations, as a predictor for earthquakes. Results have been generally unconvincing but may ultimately prove to have some limited use in specific locations.
Radon soil-concentration has been used in an experimental way to map close-subsurface geological faults, because concentrations are generally higher over the faults. Similarly it has found some limited use in geothermal prospecting.
[edit] Atmospheric studies
Radon emanation from the soil varies with soil type and with surface uranium content, so outdoor radon concentrations can be used to track air masses to a limited degree. This fact has been put to use by some atmospheric scientists.
Radon is a known pollutant emitted from geothermal power stations, though it disperses rapidly, and no radiological hazard has been demonstrated in various investigations. The trend in geothermal plants is to reinject all emissions by pumping deep underground, and this seems likely to ultimately decrease such radon hazards further.
[edit] History
Radon (named after radium) was discovered in 1900 by Friedrich Ernst Dorn, who called it radium emanation. In 1908 William Ramsay and Robert Whytlaw-Gray, who named it niton (Latin nitens meaning "shining"; symbol Nt), isolated it, determined its density and that it was the heaviest known gas. It has been called “radon” since 1923.
The first major studies of the health concern occurred in the context of uranium mining, first in the Joachimsthal region of Bohemia and then in the American Southwest during the early Cold War. Because radon is a daughter-product of uranium, uranium mines have high concentrations of radon and its highly radioactive daughter products. Many Native Americans, Mormons, and other miners in the Four Corners region would later contract lung cancer and other pathologies as a result of high levels of exposure to radon gas while mining uranium for the Atomic Energy Commission in the mid-1950s. Safety standards instituted required expensive ventilation and as such were not widely implemented or policed.
The danger of radon exposure in dwellings was discovered in 1984 with the case of Stanley Watras, an employee at the Limerick nuclear power plant in Pennsylvania. Watras set off the radiation alarms (see Geiger counter) on his way into work for two weeks straight while authorities searched for the source of the contamination. They were shocked to find that the source was astonishingly high levels of radon, around 100,000 Bq.m-3, in his house's basement and it was not related to the nuclear plant. The risks associated with living in his house were estimated to be equivalent to smoking 135 packs of cigarettes every day.[1] Following this event, which was highly publicized, national radon safety standards were set and radon detection and ventilation became a standard homeowner concern.
Radon is the second most frequent cause of lung cancer, after cigarette smoking, and radon-induced lung cancer is thought to be the 6th leading cause of cancer death overall.[2] [3]
[edit] Occurrence
On average, there is one atom of radon in 1 x 1021 molecules of air. Radon can be found in some spring waters and hot springs.[3] The towns of Boulder, Montana, Misasa, Japan, and Bad Kreuznach, Germany boast radium-rich springs which emit radon.
Radon emanates naturally from the ground, particularly in certain regions, especially (but not only) regions with granitic soils. However, not all granitic regions are prone to high emissions of radon. Depending on how houses are built and ventilated, radon may accumulate in basements and dwellings. The highest average radon concentrations in counties in the US are found in Iowa and in the Appalachian Mountains areas in south-eastern Pennsylvania. [4]
Radon, along with other noble gases krypton and xenon, is also produced during the operation of nuclear power plants. A small fraction of it leaks out of the fuel, through the cladding and into the cooling water, from which it is scavenged. It is then routed to a holdup tank where it remains for a large number of half-lives. It is finally purged to the open air through a tall stack which is carefully monitored for radiation level.
The European Union recommends that action should be taken starting from concentrations of 400 Bq/m3 for old houses and 200 Bq/m3 for new ones. After publication of the North American and European Pooling Studies, Health Canada has proposed a new guideline that lowers their action level from 800 to 200 Bq/m3.[5] The United States Environmental Protection Agency (EPA) strongly recommends action for any house with a concentration higher than 148 Bq/m3 (given as 4 pCi/L)[6], and encourages action starting at 74 Bq/m3 (given as 2 pCi/L). EPA radon risk level tables including comparisons to other risks encountered in life are available in their citizen's guide.[7] Nearly one in 15 homes in the U.S. has a high level of indoor radon according to their statistics. The U.S. Surgeon General and EPA recommend all homes be tested for radon. Since 1985, millions of homes have been tested for radon in the U.S.
Radon emitted from the ground has been shown to accumulate in the air if there is a meteorological inversion and little wind.[8]
[edit] Compounds
Some experiments indicate that fluorine can react with radon and form radon fluoride. Radon clathrates have also been reported.
[edit] Isotopes
Main article: isotopes of radon
There are twenty known isotopes of radon. The most stable isotope is 222Rn, which is a decay product (daughter product) of 226Ra, has a half-life of 3.823 days and emits alpha particles. 220Rn is a natural decay product of thorium and is called “thoron.” It has a half-life of 55.6 seconds and also emits alpha radiation. 219Rn is derived from actinium, is called “actinon,” is an alpha emitter and has a half-life of 3.96 seconds.
The full decay series of 238U which produces natural radon is as follows (with half-lives):
238U (4.5 x 109 yr), 234Th (24.1 days), 234Pa (1.18 min), 234U (250,000 yr), 230Th (75,000 yr), 226Ra (1,600 yr), 222Rn (3.82 days), 218Po (3.1 min), 214Pb (26.8 min), 214Bi (19.7 min), 214Po (164 µs), 210Pb (22.3 yr), 210Bi (5.01 days), 210Po (138 days), 206Pb (stable).
[edit] Health Effects and Epidemiology
The general effects of radon to the human body are due to its radioactivity and consequent risk of radiation-induced cancer. As an inert gas, "radon has a low solubility in body fluids which lead to a uniform distribution of the gas throughout the body" (Lindgren, 1989). Radon gas and its solid decay products are carcinogens. The greatest health risks come from exposure to the inhaled solid radon gas decay products that are produced during the radioactive decay of radon gas. Two of these decay products, polonium-218 and 214, present a significant radiologic hazard [4]. Once the radioactive decay products are inhaled into the lung, they undergo further radioactive decay releasing small bursts of energy in the form of alpha particles that can either cause double-strand DNA breaks or create free radicals that can damage the DNA [5].
Based on studies carried out by the National Academy of Sciences in the United States, radon is the second most common cause of lung cancer after cigarette smoking, accounting for 15,000 to 22,000 cancer deaths per year in the US alone according to the National Cancer Institute.[9] (Radon decay products are also present in tobacco smoke.) These estimates were based on extrapolations from radon-exposed underground miners. On January 13, 2005, the Surgeon General of the United States reported that over 20,000 Americans die each year of radon-related lung cancer.[10] The USEPA recommends homes be fixed if an occupant's long-term exposure will average 4 picocuries per liter (pCi/L) (148 Bq m-3) or higher.[11]
Risk estimates no longer need to be based on extrapolations from miners, but rather can be taken from direct evidence from residential studies. One of the most comprehensive case-control epidemiologic radon studies, performed by R. William Field and colleagues at the University of Iowa and College of Saint Benedict/Saint John's University,[12] demonstrated a 50% increased lung cancer risk with prolonged radon exposure at the EPA's action level of 4 pCi/L.[13][14] Iowa has the highest average radon concentrations in the nation and a very stable population which added to the strength of the study. Recent pooled epidemiologic radon studies by Dan Krewski et al. (2005; 2006)[15][16] and Sarah Darby et al. (2005) have also shown an increased lung cancer risk from radon below the U.S. EPA's action level of 4 pCi/L.
It is unknown whether radon causes other types of cancer, but recent studies suggest that more research is needed to assess whether or not radon exposure is associated with other cancers (i.e. leukemia, breast cancer) and non cancer outcomes (i.e. MS) [6], [7]
[edit] Testing and mitigation
ASTM E-2121 is a standard for reducing radon in homes as far as practicable below 4 picocuries per liter (pCi/L) in indoor air.[17][18] In the U.S., about one in every 15 homes has a radon level above this standard.[19]
Radon test kits are commercially available. In the U.S., single test kits can cost about $10.[20] The kit includes a collector that the user hangs in the basement for 2 to 7 days. The user then sends the collector to a laboratory for analysis. The National Environmental Health Association provides a list of radon measurement professionals.[21] Long term kits, taking collections for up to one year, are also available. An open land test kit can test radon emissions from the land before construction begins. The USEPA and the National Environmental Health Association, have identified 15 types of radon testing.[22] A Lucas cell is one type of device.
Radon levels fluctuate naturally. An initial test might not be an accurate assessment of your home's average radon level. Transient weather can affect short term measurements.[23] Therefore, a high result (over 4 pc/l) justifies repeating the test before undertaking more expensive abatement projects. Measurements between 4 and 10 pc/l warrant a long term radon test. Measurements over 10 pc/l warrant only another short term test so that abatement measures are not unduly delayed. Purchasers of real estate are advised to delay or decline a purchase if the seller has not successfully abated radon to 4 pc/l or less.
The National Environmental Health Association (NEHA) administers a voluntary National Radon Proficiency Program (NRPP) for radon professionals consisting of individuals and companies wanting to take training courses and examinations to demonstrate their competency.[24] A list of mitigation service providers is available.[25] Indoor radon can be mitigated by sealing basement foundations, water drainage, or by sub-slab de-pressurization. In severe cases, mitigation can use air pipes and fans to exhaust sub-slab air to the outside. Indoor ventilation systems are more effective, but exterior ventilation can be cost-effective in some cases. Modern construction that conserves energy by making homes air tight exacerbates the risks of radon exposure, if radon is present in the home. Older homes with more porous construction are more likely to vent radon naturally. Ventilation systems can be combined with a heat exchanger to recover energy in the process of exchanging air with the outside. Homes built on a crawl space can benefit from a radon collector installed under a radon barrier (a sheet of plastic that covers the crawl space).
[edit] Radon therapy
Radon therapy has been historically used in some spa resorts around the world. Beneficial health effects of radon therapy have never been clinically proven.
Radioactive water baths have been applied since 1906 in Joachimsthal, Czech Republic, but even before radon discovery they were used in Bad Gastein, Austria. Hot radium-rich spring releasing radon is also used in traditional Japanese onsen in Misasa, Tottori prefecture. Drinking therapy is applied in Bad Brambach, Germany. Inhalation therapy is carried out in Gasteiner-Heilstollen, Austria, in Kowary, Poland and in Boulder, Montana, United States.
[edit] References
^ The Radon Story, University of Bradford, UK
^ S. Darby, D. Hill, R. Doll (2001). "Radon: A likely carcinogen at all exposures". Annals of Oncology 12 (10): 27. DOI:10.1023/A:1012518223463.
^ Radon Occurrence and Health Risk, R. William Field, Department of Occupational and Environmental Health, University of Iowa.
^ [1]
^ It's Your Health - Radon, Health Canada
^ Radiation information: radon. United States Environmental Protection Agency (Oct 2006). Retrieved on 2007-05-25.
^ A Citizen's Guide to Radon: The Guide to Protecting Yourself and Your Family from Radon, United States Environmental Protection Agency.
^ Daniel J. Steck, R. William Field, and Charles F. Lynch, "Exposure to Atmospheric Radon", Environmental Health Perspectives, Volume 107, Number 2, February 1999. Online version
^ http://www.cancer.gov/cancertopics/factsheet/Risk/radon
^ http://www.surgeongeneral.gov/pressreleases/sg01132005.html
^ http://www.epa.gov/radon/
^ http://www.csbsju.edu/MNradon/
^ http://www.epa.gov/iaq/radon/iowastudy.html
^ http://aje.oxfordjournals.org/cgi/content/abstract/151/11/1091?ijkey=8382ae3c72b5d0496d6436b37843689b6963e046&keytype2=tf_ipsecsha
^ http://www.public-health.uiowa.edu/newsletter/rd.asp?rlsId=254
^ http://www.radonnews.org/RadonRiskStudies/NorthAmericanPooling.pdf
^ http://www.epa.gov/iaq/radon/pubs/mitstds.html
^ http://www.astm.org/cgi-bin/SoftCart.exe/DATABASE.CART/REDLINE_PAGES/E2121.htm?L+mystore+xyan5063
^ http://www.nsc.org/library/facts/radon.htm
^ http://www.radon.com/cgi-bin/oo.cgi
^ http://www.radongas.org/Description_of_Radon_Measurement_Service.html
^ http://www.radongas.org/device.htm
^ http://www.radon.com/radon/mitigation.html
^ http://www.radongas.org/
^ http://www.radongas.org/Description_of_Radon_Mitigation_Services.html
[edit] Other references
Los Alamos National Laboratory - Radon
USGS Periodic Table - Radon
EPA Iowa Radon Study
World Health Organization International Radon Project
Decay chains of some elements including Radon
[8]Radon Occurrence and Health Risks
[edit] Notable Radon Researchers and Scientists
Sarah Darby
R. William Field
Dan Krewski
Daniel J. Steck
[edit] External links
Wikimedia Commons has media related to:
RadonLook up radon in
Wiktionary, the free dictionary.Iowa Radon Lung Cancer Study FREE Reprint [9]*Iowa RadonLung Cancer Study
WebElements.com - Radon
U.S. Environmental Protection Agency — Indoor Air Radon
Agency for Toxic Substances and Disease Registry — Radon Toxicity Case Study
(U.S.) National Safety Council info
U.K. Health Protection Agency Information
Ask TreeHugger: What Do Radon Tests Mean?
Retrieved from "http://en.wikipedia.org/wiki/Radon"
Categories: Chemical elements | Building biology | Health risks | Noble gases | Soil contamination
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