Radon resides in group 18 of the periodic table of elements. It is continuously formed by the natural radioactive decay of the element radium. Radium itself is a decay product of uranium and thorium naturally found in global soils and rocks.
Being a noble gas, radon is remarkably chemically inert under standard environmental conditions. This means it almost never reacts with other elements in nature. However, it can form a few simple chemical compounds under extreme laboratory conditions.
For example, scientists have successfully forced it to react and form radon difluoride (RnF2). Radon gas easily diffuses out of the ground and escapes upward into the atmosphere. It can accumulate and concentrate heavily in building basements, underground mines, and poorly sealed houses.
The most stable natural isotope is radon-222, which possesses a half-life of about 3.8 days. This radioactive isotope predictably decays into heavy, solid radioactive elements that can be deeply inhaled. Prolonged exposure to concentrated radon and its radioactive decay products is extremely dangerous. Medical experts widely recognize this exposure as a leading global cause of severe lung cancer.

![Radon element card: symbol Rn, atomic number 86, atomic mass [222], electron configuration [Xe] 4f¹⁴ 5d¹⁰ 6s² 6p⁶, Noble gas, group 18, period 6, gas at room temperature.](https://stage.chemistry-dictionary.com/wp-content/uploads/2026/09/radon-chemical-element.webp)