Krypton is a chemical element and a rare noble gas in Group 18 of the periodic table, with the atomic number 36 and symbol "Kr." It is nearly three times heavier than air and is colourless, tasteless, monoatomic, and odourless. Krypton is more abundant in Earth's atmosphere than other places, with traces found in minerals and meteorites. Earth's atmosphere contains approximately 1.14 parts per million of krypton by volume.
Krypton was discovered in 1898 by Sir William Ramsay and Morris Travers during the fractional distillation of liquid air. Like other noble gases, krypton’s full outer electron shell makes it resistant to forming compounds with most other elements, contributing to its reputation as an inert gas.
Krypton is found in trace amounts in Earth's atmosphere, making up approximately 1.14 parts per million by volume. It can also be found in minerals and meteorites.
Krypton is a colourless, odourless, tasteless, monoatomic gas about three times heavier than air.
In its solid state, krypton forms a face-centred cubic crystalline structure, similar to other noble gases. At high temperatures, krypton behaves similarly to neon but emits a purple glow instead of red. When mixed with other gases, krypton produces a greenish-yellow light.
Interestingly, krypton is more concentrated at the North Pole than at the South Pole due to convective mixing, a process where solid particles disperse within one another.
Although krypton is rare on Earth, it is relatively common in stars, including the sun.
Although traditionally considered unreactive, krypton can form compounds with highly electronegative elements, such as fluorine, under specific conditions. In its +2 oxidation state, krypton reacts with fluorine at extremely low temperatures (-196°C) in the presence of an electrical discharge to form krypton difluoride (KrF2). This compound is unstable and decomposes at higher temperatures. Importantly, krypton reacts exclusively with fluorine and does not form compounds with other halogens.
(Session 2025 - 26)