Radon
Radon is a colorless, odorless, radioactive noble gas that forms naturally as certain rocks and soils slowly release it during the radioactive decay of uranium and radium. Because it's completely undetectable by human senses yet radioactive, it's taken seriously today as an indoor air quality hazard, especially when it seeps into basements and accumulates in poorly ventilated buildings.
- Group · Period
- 18 · 6
- At room temp
- gas
- Melts at
- 202 K
- Density
- 0.00973 g/cm³
- Discovered
- 1900
Uses
Radon has very few practical uses today, largely because its radioactivity makes it more of a hazard to manage than a resource to exploit. In the early-to-mid 20th century, small sealed capsules of radon gas, called radon seeds, were occasionally used in a form of radiotherapy to treat tumors, since the radiation it emits can damage cancerous tissue; this practice has almost entirely been replaced by safer, more precisely controlled radiation sources. Radon is also occasionally used in scientific research, for instance as a natural tracer that helps geologists study fault lines, groundwater movement, or soil permeability, since its concentration in air or water reflects underlying geological activity.
By far radon’s most significant modern relevance is as something to be monitored and reduced rather than used — building codes and health agencies in many countries recommend testing homes for radon and installing ventilation systems to keep indoor concentrations low.
History
Radon was discovered in 1900 by German physicist Friedrich Ernst Dorn, who noticed that samples of radium continually released a radioactive gas as part of their natural decay process. He referred to it as “radium emanation,” and other researchers around the same period identified similar emanations from thorium and actinium, which were later understood to be different isotopes of the same element. It eventually took the name radon to reflect its connection to radium and its place as a member of the noble gas group, once chemists confirmed that all these “emanations” were really the same chemical element.
Fun facts
- Radon is the only naturally occurring element that is a gas at room temperature and also radioactive.
- Radon exposure in homes is considered a leading cause of lung cancer in non-smokers, which is why many countries recommend testing basements and ground-floor rooms for it.
- Being a noble gas, radon barely reacts chemically with anything, so it simply seeps up through soil and rock and diffuses into the air rather than binding into stable compounds.
Frequently asked questions
Why is radon dangerous if it's chemically unreactive like other noble gases?
Radon's danger has nothing to do with chemical reactivity — it comes from radioactivity. When inhaled, radon and the radioactive particles it decays into can damage lung tissue over time, which is why long-term exposure, especially in enclosed spaces like basements, is linked to an increased risk of lung cancer.
How does radon get into homes if it comes from rock and soil?
Radon gas seeps up naturally from uranium- and radium-bearing rock and soil beneath and around buildings, and it can enter through cracks in foundations, gaps around pipes, or sump pits. It tends to build up most in basements and ground-floor spaces with limited airflow, which is why testing and ventilation matter most there.
Who discovered radon and how?
German scientist Friedrich Ernst Dorn discovered radon in 1900 while studying radium, noticing that radium samples continuously gave off a radioactive gas as they decayed. He initially called it "radium emanation," and it was only later given the name radon, tying it to its place among the other noble gases.
Compounds
1 notable compound containing Rn
- RnF2halide
Radon difluoride
A compound inferred from radiotracer experiments in which radon gas reacts with fluorine to form a nonvolatile solid; because radon decays so quickly, it has never been produced or observed in a visible, weighable amount, so its properties remain only partly established.
Used for: No practical use — studied only to probe the chemistry of a normally 'inert' gas
Isotopes
39 known isotopes
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| Isotope | Natural abundance | Half-life | Decay mode | Mass excess | Binding energy / nucleon | Decay width |
|---|---|---|---|---|---|---|
| Rn-210 | — | 2.4 h | Alpha decay (96%), Electron capture / beta-plus decay (4%) | -9,604.76 keV | 7,796.67 keV | 5.28 × 10-20 eV |
| Rn-211 | — | 14.6 h | Electron capture (72.6%), Alpha decay (27.4%) | -8,755.33 keV | 7,793.94 keV | 8.68 × 10-21 eV |
| Rn-222 | — | 3.8235 d | Alpha decay (100%) | 16,371.96 keV | 7,694.5 keV | 1.38 × 10-21 eV |
Show all 39 isotopes
| Rn-193 | — | 1.15 ms | Alpha decay (100%) | 9,042.92 keV | 7,675.85 keV | 3.97 × 10-13 eV |
| Rn-194 | — | 0.78 ms | Alpha decay (100%) | 5,724.62 keV | 7,695 keV | 5.85 × 10-13 eV |
| Rn-195 | — | 6 ms | Alpha decay (100%) | 5,050.29 keV | 7,700.38 keV | 7.60 × 10-14 eV |
| Rn-196 | — | 4.4 ms | Alpha decay (99.9%), Electron capture / beta-plus decay (0.06%) | 1,975.17 keV | 7,717.97 keV | 1.04 × 10-13 eV |
| Rn-197 | — | 65 ms | Alpha decay (100%) | 1,510.37 keV | 7,722.12 keV | 7.02 × 10-15 eV |
| Rn-198 | — | 65 ms | Electron capture / beta-plus decay, Alpha decay | -1,230.32 keV | 7,737.72 keV | 7.02 × 10-15 eV |
| Rn-199 | — | 0.59 s | Alpha decay (94%), Electron capture / beta-plus decay (6%) | -1,559.85 keV | 7,741.06 keV | 7.73 × 10-16 eV |
| Rn-200 | — | 1.03 s | Alpha decay (86%), Electron capture / beta-plus decay (14%) | -4,000.45 keV | 7,754.91 keV | 4.43 × 10-16 eV |
| Rn-201 | — | 7.0 s | Electron capture / beta-plus decay, Alpha decay | -4,107.41 keV | 7,757.02 keV | 6.52 × 10-17 eV |
| Rn-202 | — | 9.7 s | Alpha decay (78%), Electron capture / beta-plus decay (22%) | -6,274.56 keV | 7,769.3 keV | 4.70 × 10-17 eV |
| Rn-203 | — | 44.2 s | Alpha decay (66%), Electron capture / beta-plus decay (34%) | -6,184.05 keV | 7,770.34 keV | 1.03 × 10-17 eV |
| Rn-204 | — | 74.5 s | Alpha decay (72.4%), Electron capture / beta-plus decay (27.6%) | -7,970.12 keV | 7,780.57 keV | 6.12 × 10-18 eV |
| Rn-205 | — | 170 s | Electron capture / beta-plus decay (75.4%), Alpha decay (24.6%) | -7,709.76 keV | 7,780.72 keV | 2.68 × 10-18 eV |
| Rn-206 | — | 5.67 m | Alpha decay (62%), Electron capture / beta-plus decay (38%) | -9,132.92 keV | 7,789.04 keV | 1.34 × 10-18 eV |
| Rn-207 | — | 9.25 m | Electron capture / beta-plus decay (79%), Alpha decay (21%) | -8,634.74 keV | 7,788 keV | 8.22 × 10-19 eV |
| Rn-208 | — | 24.35 m | Alpha decay (62%), Electron capture / beta-plus decay (38%) | -9,655.39 keV | 7,794.27 keV | 3.12 × 10-19 eV |
| Rn-209 | — | 28.8 m | Electron capture / beta-plus decay (83%), Alpha decay (17%) | -8,941.05 keV | 7,792.18 keV | 2.64 × 10-19 eV |
| Rn-212 | — | 23.9 m | Alpha decay (100%) | -8,659.22 keV | 7,794.8 keV | 3.18 × 10-19 eV |
| Rn-213 | — | 19.4 ms | Alpha decay (100%) | -5,695.95 keV | 7,782.18 keV | 2.35 × 10-14 eV |
| Rn-214 | — | 259 ns | Alpha decay (100%) | -4,319.66 keV | 7,777.1 keV | 1.76 × 10-9 eV |
| Rn-215 | — | 2.30 us | Alpha decay (100%) | -1,168.99 keV | 7,763.82 keV | 1.98 × 10-10 eV |
| Rn-216 | — | 45 us | Alpha decay (100%) | 253.31 keV | 7,758.66 keV | 1.01 × 10-11 eV |
| Rn-217 | — | 0.54 ms | Alpha decay (100%) | 3,658.57 keV | 7,744.4 keV | 8.45 × 10-13 eV |
| Rn-218 | — | 33.75 ms | Alpha decay (100%) | 5,217.41 keV | 7,738.75 keV | 1.35 × 10-14 eV |
| Rn-219 | — | 3.96 s | Alpha decay (100%) | 8,829.34 keV | 7,723.78 keV | 1.15 × 10-16 eV |
| Rn-220 | — | 55.6 s | Alpha decay (100%) | 10,611.99 keV | 7,717.26 keV | 8.21 × 10-18 eV |
| Rn-221 | — | 25 m | Beta-minus decay (78%), Alpha decay (22%) | 14,471.35 keV | 7,701.39 keV | 3.04 × 10-19 eV |
| Rn-223 | — | 24.3 m | Beta-minus decay (100%) | 20,389.74 keV | 7,678.17 keV | 3.13 × 10-19 eV |
| Rn-224 | — | 107 m | Beta-minus decay (100%) | 22,445.1 keV | 7,670.75 keV | 7.11 × 10-20 eV |
| Rn-225 | — | 4.66 m | Beta-minus decay (100%) | 26,534.14 keV | 7,654.36 keV | 1.63 × 10-18 eV |
| Rn-226 | — | 7.4 m | Beta-minus decay (100%) | 28,747.19 keV | 7,646.41 keV | 1.03 × 10-18 eV |
| Rn-227 | — | 20.2 s | Beta-minus decay (100%) | 32,885.84 keV | 7,630.05 keV | 2.26 × 10-17 eV |
| Rn-228 | — | 65 s | Beta-minus decay (100%) | 35,243.47 keV | 7,621.65 keV | 7.02 × 10-18 eV |
| Rn-229 | — | 12.0 s | Beta-minus decay (100%) | 39,362.4 keV | 7,605.62 keV | 3.80 × 10-17 eV |
| Rn-230 | — | — | Unknown | 42,170 keV | 7,595 keV | — |
| Rn-231 | — | — | Beta-minus decay (100%) | 46,550 keV | 7,579 keV | — |