Krypton is characterized by several sharp emission lines (
spectral signatures) the strongest being green and yellow. Krypton is one of the products of
uranium fission. Solid krypton is white and has a face-centered
cubic crystal structure, which is a common property of all noble gases (except
helium, which has a hexagonal close-packed crystal structure).
Isotopes Naturally occurring krypton in Earth's atmosphere is composed of five
stable isotopes, plus one isotope (78Kr) with such a long
half-life (9.2×1021 years) that it can be considered stable. (This isotope has the third-longest known half-life among all isotopes for which decay has been observed; it undergoes
double electron capture to 78
Se). In addition, about thirty unstable isotopes and
isomers are known. Traces of 81Kr, a
cosmogenic nuclide produced by the
cosmic ray irradiation of 80Kr, also occur in nature: this
isotope is
radioactive with a half-life of 230,000 years. Krypton is highly volatile and does not stay in solution in near-surface water, but 81Kr has been used for
dating old (50,000–800,000 years)
groundwater.
85Kr is an inert radioactive noble gas with a half-life of 10.76 years. It is produced by the
fission of
uranium and
plutonium, such as in
nuclear bomb testing and
nuclear reactors. 85Kr is released during the reprocessing of
fuel rods from nuclear reactors. Concentrations at the
North Pole are 30% higher than at the
South Pole due to convective mixing.
Chemistry Like the other noble gases, krypton is chemically highly unreactive. The rather restricted chemistry of krypton in the +2 oxidation state parallels that of the neighboring element
bromine in the +1 oxidation state; due to the
scandide contraction it is difficult to oxidize the 4p elements to their group oxidation states. Until the 1960s no noble gas compounds had been synthesized. Following the first successful synthesis of
xenon compounds in 1962, synthesis of
krypton difluoride () was reported in 1963. In the same year, was reported by Grosse,
et al., but was subsequently shown to be a mistaken identification. Under extreme conditions, krypton reacts with fluorine to form KrF2 according to the following equation: : Krypton gas in a
krypton fluoride laser absorbs energy from a source, causing the krypton to react with fluorine gas, producing the exciplex krypton fluoride, a temporary
complex in an excited energy state: : The complex can undergo spontaneous or stimulated emission, reducing its energy state to a metastable, but highly
repulsive ground state. The ground state complex quickly dissociates into unbound atoms: : The result is an
exciplex laser which radiates energy at 248 nm, near the
ultraviolet portion of the
spectrum, corresponding with the energy difference between the ground state and the excited state of the complex.
ArKr+ and Kr
H+
polyatomic ions have been investigated and there is evidence for Kr
Xe or KrXe+. The reaction of with produces an unstable compound, , that contains a krypton-
oxygen bond. A krypton-
nitrogen bond is found in the
cation [HC≡N–Kr–F], produced by the reaction of with [HC≡NH][AsF] below −50 °C. The kryptonium ion, KrH+, is an
onium ion, consisting of protonated krypton. Kryptonium is known in dilute gas phase. Although salts of the fluorokryptonium ion, KrF+, are known to exist, the existence of the kryptonium salts have not been proven. In 1989,
Bergman,
Moore,
Pimentel and coworkers photolyzed a
rhodium(I) complex, Cp*Rh(CO)2 (Cp* =
pentamethylcyclopentadienyl), using a pulsed
XeCl laser (308 nm) in pressurized liquid Kr as a solvent at a temperature between −80 and −120 °C and observed the formation of Cp*Rh(CO)(Kr), which was identified by
infrared spectroscopy by its metal–carbonyl stretch at 1946 cm−1. This species decayed with a rate constant of
k = 5 × 103 s−1 at −80 °C. The analogous Xe complex, with an infrared signal at 1943 cm−1, was more stable and could be observed at −30 °C in pressurized liquid Xe. The highly reactive and transient Cp*Rh(CO) species believed to form upon photolysis also coordinates to and inserts into the C–H bonds of cyclohexane and other alkanes (R–H) under these conditions to give alkane
σ-complexes Cp*Rh(CO)(R–H) and rhodium(III) alkyl complexes Cp*Rh(CO)(R)(H) upon
oxidative addition.
Natural occurrence Earth has retained all of the noble gases that were present at its formation except
helium. Krypton's concentration in the
atmosphere is about 1
ppm. It can be extracted from liquid air by
fractional distillation. The amount of krypton in space is uncertain, because measurement is derived from meteoric activity and solar winds. The first measurements suggest an abundance of krypton in space. ==Applications==