Radon (Rn)

Radon is a heavy, colorless, odorless, radioactive noble gas produced by the decay of uranium and thorium in rocks and soil. It is the densest gas at standard conditions and a significant inhalation hazard linked to lung cancer.

Atomic Number
86
Atomic Mass
222
Category
Noble Gases
Phase (STP)
Gas
Block
P
Electronegativity (Pauling)

Bohr Atomic Model

Protons
86
Neutrons
136
Electrons
86
Identity
Atomic Number86
SymbolRn
NameRadon
Group18
Period6
Position
Period6
Group Label18
Grid X18
Grid Y6
Physical Properties
Atomic Mass (u)222
Density (g/cm³)0.009074
Melting Point (K)202 K -71.15 °C
Boiling Point211.5 K -61.7 °C
Phase at STPGas
CategoryNoble Gases
Liquid Density (g/cm³)
Molar Volume (cm³/mol)
Emission Spectrum (nm)
Discovery
English NameRadon
English Pronunciationˈreɪdɒn
Latin NameRadon
Latin PronunciationRA-don
Year1900
DiscovererFriedrich Ernst Dorn
CountryGermany
CAS Number10043-92-2
CID Number
RTECS Number
Atomic Properties
Electron ShellK2
Electron Configuration[Xe] 4f^1^45d^1^06s^26p^6
Oxidation States0 +2
Ion Charge
Ionization Potential (eV)10.749
Electronegativity (Pauling)
Electron Affinity (kJ/mol)
Electrons86
Protons86
Neutrons136
ValenceVIII
BlockP
Atomic Radius (pm)
Covalent Radius (pm)146
van der Waals Radius (pm)220
Thermodynamic Properties
PhaseGAS
Heat of Fusion (kJ/mol)
Specific Heat (J/g·K)0.094
Thermal Expansion (1/K)
Heat of Vaporization (kJ/mol)
Mechanical Properties
Brinell Hardness
Mohs Hardness
Vickers Hardness
Bulk Modulus (GPa)
Young's Modulus (GPa)
Shear Modulus (GPa)
Poisson Ratio
Sound Speed (m/s)
Refractive Index
Thermal Conductivity (W/m·K)
Electromagnetic Properties
Electrical Conductivity (S/m)
Electrical TypeINSULATOR
Magnetic TypeDIAMAGNETIC
Volume Magnetic Susceptibility
Mass Magnetic Susceptibility
Molar Magnetic Susceptibility
Resistivity (Ω·m)
Superconducting Point (K)
Crystal Properties
StructureFace-centered cubic (fcc) — solid
SystemCUBIC
Space Group
a (Å)
b (Å)
c (Å)
α (°)
β (°)
γ (°)
Debye Temperature (K)
Nuclear Properties
RadioactiveNo
Half-lifeRn-222: 3.82 days
Lifetime
Neutron Cross-section (barn)
Safety Information
Health HazardKnown human carcinogen (lung cancer risk)
Reactivity HazardChemically inert; forms few compounds
Specific HazardRadioactive; asphyxiant at high concentrations
Prevalence
Universe
Sun
Oceans
Human Body
Earth Crust
Meteorites


FAQs about Radon

Radon is a naturally occurring radioactive noble gas produced by the decay of uranium (U) and thorium (Th) present in the Earth’s crust. It is part of the uranium-238 decay chain:

\(\mathrm{^{238}U \rightarrow ^{226}Ra \rightarrow ^{222}Rn + \alpha}\)

The isotope radon-222 is the most stable and common form, with a half-life of 3.8 days.

Radon is dangerous because it emits alpha radiation during radioactive decay. When inhaled, it can damage lung tissue, increasing the risk of lung cancer. Prolonged exposure to high levels of radon gas, especially indoors, is a leading cause of lung cancer after smoking.

Radon has several isotopes, all radioactive. The most important ones are:

  • Rn-222: Half-life 3.8 days, from the uranium-238 series.
  • Rn-220 (Thoron): Half-life 55.6 seconds, from the thorium-232 series.
  • Rn-219 (Actinon): Half-life 3.96 seconds, from the actinium series.

Among them, Rn-222 is the most significant in environmental and health contexts.

Radon gas is found everywhere in small amounts. It seeps naturally from soil, rocks, and groundwater. It tends to accumulate in enclosed spaces such as basements and underground buildings where ventilation is poor.

Radon is a colorless, odorless, and tasteless gas at room temperature. It condenses into a colorless liquid below −61.8 °C and freezes into a yellow solid below −71 °C. It is the densest noble gas and slightly soluble in water and organic solvents.

As a noble gas, radon is chemically inert under most conditions. However, under extreme conditions, it can form compounds such as radon difluoride (RnF2) and possibly oxides of radon. These compounds are unstable and only observed in laboratory conditions.

\(\mathrm{Rn + F_2 \rightarrow RnF_2}\)

Radon is a major source of natural background radiation. When radon gas decays, it produces radioactive radon daughters (like polonium-218 and lead-214) that attach to dust particles. Inhalation of these particles leads to alpha radiation exposure inside the lungs.

Radon exposure can be reduced by:

  • Improving ventilation in basements and crawl spaces.
  • Sealing cracks in floors and walls to prevent gas entry.
  • Installing radon mitigation systems that vent gas outside the building.
  • Regularly testing indoor air using radon test kits.

Radon has limited but specialized applications:

  • Medical therapy: Historically used in radiation therapy for cancer (now mostly replaced).
  • Scientific research: As a tracer gas to study air movement and groundwater flow.
  • Geological surveys: Used in detecting uranium deposits and studying seismic activity.

Radon is part of the noble gases (Group 18) because it has a complete outer electron shell (6s26p6), making it chemically inert under normal conditions, similar to helium, neon, and argon.

Long-term exposure to radon and its decay products is the second leading cause of lung cancer after smoking. According to the World Health Organization (WHO), safe indoor radon levels should be below 100 Bq/m³ to minimize risk.