Geology
Isotopes, minerals or decay products are used to trace geological processes and the history of rocks.
Radon is element 86 (Rn), located in period 6, group 18 and the p block. At room temperature its reference phase is gas. Its electron configuration is [Xe] 4f14 5d10 6s2 6p6.
The outer electron shell is filled, which strongly reduces the tendency to gain, lose or share electrons. This is the central reason noble gases are much less reactive than neighbouring groups.
The heavier noble gases are not completely inert: under suitable conditions some form compounds, especially with highly electronegative elements. The group trend is therefore low reactivity, not an absolute prohibition on chemistry.
Radon is monatomic under ordinary conditions. Noble-gas compounds are unusual, but the heavier members can form compounds under strongly oxidising conditions; xenon chemistry in particular includes well-characterised fluorides and oxides.
The reference phase at room temperature is gas. The listed density is 9.73 g/L. The melting point is 202 K (-71.15 °C). The boiling point is 211.5 K (-61.65 °C). Pressure, purity and crystal structure can shift measured physical properties.
In practice, radon is encountered in geology, health and scientific research.
Isotopes, minerals or decay products are used to trace geological processes and the history of rocks.
Radon is important mainly because exposure, radioactivity or biological effects must be measured and controlled.
Radon is produced, isolated or measured mainly to test atomic, nuclear and periodic trends rather than for bulk commercial use.
Radon is in period 6 and group 18. In the neighbourhood shown here, astatine is immediately to its left in the same period; xenon is above it and oganesson below it in the same group. These positions make it possible to compare atomic size, ionisation energy and bonding behaviour with nearby elements.
Values describe the element or neutral atom where applicable. Physical data can depend on allotrope, pressure and measurement conditions.
The discovery of radon is associated with Friedrich Ernst Dorn. Recognition of the element, isolation of a pure sample and assignment of its modern atomic number did not necessarily occur at the same time.
Radon has no standard atomic weight. There is no characteristic terrestrial isotopic mixture from which a stable abundance-weighted average can be assigned.
Radon has no stable isotope. Its isotopes are radioactive, and their half-lives and decay modes become important whenever the element is measured, handled or used.
Radon is radioactive. Work with it requires radiological controls appropriate to the isotope, activity, radiation type and chemical form.