Krypton: a noble gas element (atomic number 36)
Krypton is a colorless, odorless noble gas (Kr, Z=36) used in lighting, lasers and standards. It occurs in trace amounts in air and has a small number of stable isotopes and some radioisotopes.
Krypton is a chemical element in the group of inert gases known as the noble gases. Its chemical symbol is Kr and its atomic number is 36. At ordinary temperatures and pressures it is a colorless, odorless, monatomic gas with very low chemical reactivity. The element's name derives from the Greek word kryptos, meaning "hidden", a reference to its rarity and the difficulty of isolating it.
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7 ImagesCharacteristics and physical properties
Krypton is distinguished by its low reactivity, typical of the noble gases, but under extreme laboratory conditions it can form a few compounds—most notably krypton difluoride (KrF2). It exists naturally as several isotopes, some stable and others radioactive. Commercially, krypton is separated from air by cryogenic fractional distillation of liquefied air and recovered in small quantities because it is present only as a trace constituent.
- Symbol: Kr; atomic number: 36.
- Appearance: colorless, odorless monatomic gas at standard conditions.
- Chemical behavior: largely inert; forms only a few rare, highly oxidized species under special conditions.
- Isotopes: multiple stable isotopes exist; certain radioisotopes (e.g., Kr-85) are produced by nuclear fission.
History and naming
Krypton was discovered in 1898 by Sir William Ramsay and Morris Travers during the study of liquefied air. They detected it as a faintly luminous component left after removing oxygen, nitrogen and argon. The choice of the name reflects the element's initially "hidden" presence in the atmosphere and the challenge of its isolation.
Uses and applications
Krypton has several practical and scientific uses that exploit its spectral and thermal properties. It is used in certain types of lighting, in high-speed photography and in some lasers. Because of well-defined emission lines, krypton has also been employed as a reference in optical measurements and standards.
- Lighting: additives in fluorescent and discharge lamps, photographic flash tubes and some high-intensity lamps.
- Lasers and optics: components in excimer and gas lasers; used where specific ultraviolet or visible wavelengths are required.
- Windows and insulation: filling between panes in energy-efficient glazing to reduce heat transfer.
- Standards and measurement: a specific spectral line of the isotope krypton-86 was once used as a wavelength standard for defining the metre, and krypton emission lines continue to be important in spectroscopy.
Krypton also finds specialized roles in research laboratories and certain industrial processes. Its scarcity and cost limit widespread use, so it is reserved for applications that specifically benefit from its unique physical or spectral characteristics.
Notable facts and distinctions
Krypton belongs to the same column of the periodic table as neon, argon and xenon, sharing many traits of chemical inertness. Unlike heavier xenon, which forms a wider range of compounds, krypton's chemistry is considerably more limited. Though present only in trace amounts in Earth's atmosphere, its distinct spectral lines make it valuable for precise optical work. For general reference the element is often described simply as a noble gas.
For further general reading on noble gases and related techniques see introductory resources and spectral databases: fluorescent lamp technology and manufacturer or standards organization pages for measurement history and practice.
History
In 1894 argon had been discovered as the first noble gas by John William Strutt, 3rd Baron Rayleigh and William Ramsay, one year later helium, known so far only from the solar spectrum, was isolated by Ramsay from uranium ores. From the laws of the periodic table, Ramsay realized that there must be other such elements. Therefore, starting in 1896, he first investigated various minerals and meteorites and the gases they emitted when heated or dissolved. However, he and his colleague Morris William Travers were not successful, only helium and, more rarely, argon were found. The investigation of hot gases from Cauterets in France and from Iceland also brought no results.
Finally, they examined 15 litres of liquefied crude argon and separated it by fractional distillation. In the residue they found hitherto unknown yellow and green spectral lines, i.e. a new element. It was named krypton after the ancient Greek κρυπτός kryptós ("hidden"). After purification by further distillation, Ramsay and Travers were also able to determine its molar mass of about 80 g/mol. After this discovery, they found the element neon in another, lower-boiling fraction, and finally, by separating the crude krypton, the element xenon.
In 1924, Andreas von Antropoff claimed to have synthesized a first krypton compound in the form of a red stable solid of krypton and chlorine. However, it later turned out that this compound did not contain krypton, but nitrogen monoxide and hydrogen chloride. Greater efforts in the synthesis of krypton compounds were made after the discovery of the first xenon compounds in 1962. Aristid von Grosse was the first to present a krypton compound. He initially thought it was krypton tetrafluoride; however, it was identified as krypton difluoride after further experiments.
The wavelength of an electromagnetic radiation emitted by the krypton isotope 86Kr was chosen as the basis for the definition of the metre in 1960. It thus replaced the too imprecise definition via the primal meter made of a platinum-iridium alloy. A metre was defined as 1,650,763.73 times the wavelength of the radiation emitted by the nuclide 86Kr during the transition from the 5d5 to the 2pl0 state and propagating in vacuum. In 1983, this definition was finally replaced by one based on the distance light travels in vacuum in a given fraction of a second.
Occurrence
Krypton is one of the rarest elements on earth. Rarer are only xenon and radioactive elements, which either have already decayed for the most part like plutonium or only occur as a short-lived intermediate product of decay series. The proportion of krypton in the Earth's atmosphere is 1.9 - 10-5 ppm, the largest part of the gas is in the atmosphere, which consists of 1.14 ppm krypton.
In the rest of the universe, krypton occurs in higher proportions, comparable to those of lithium, gallium, and scandium. The ratio of krypton to hydrogen is largely constant in the universe. It can be concluded that interstellar matter is rich in krypton. Krypton could also be detected in a white dwarf. Compared to the Sun, 450 times the amount was measured, but the reason for this high krypton content is still unknown.
Related articles
Author
AlegsaOnline.com Krypton: a noble gas element (atomic number 36) Leandro Alegsa
URL: https://en.alegsaonline.com/art/54519
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