Krypton

From New World Encyclopedia
For other uses, see Krypton (disambiguation).
36 brominekryptonrubidium
Ar

Kr

Xe
Kr-TableImage.png
periodic table
General
Name, Symbol, Number krypton, Kr, 36
Chemical series noble gases
Group, Period, Block 18, 4, p
Appearance colorless
Kr,36.jpg
Atomic mass 83.798(2) g/mol
Electron configuration [Ar] 3d10 4s2 4p6
Electrons per shell 2, 8, 18, 8
Physical properties
Phase gas
Density (0 °C, 101.325 kPa)
3.749 g/L
Melting point 115.79 K
(-157.36 °C, -251.25 °F)
Boiling point 119.93 K
(-153.22 °C, -243.8 °F)
Critical point 209.41 K, 5.50 MPa
Heat of fusion 1.64 kJ/mol
Heat of vaporization 9.08 kJ/mol
Heat capacity (25 °C) 20.786 J/(mol·K)
Vapor pressure
P/Pa 1 10 100 1 k 10 k 100 k
at T/K 59 65 74 84 99 120
Atomic properties
Crystal structure cubic face centered
Oxidation states 2
Electronegativity 3.00 (Pauling scale)
Ionization energies
(more)
1st: 1350.8 kJ/mol
2nd: 2350.4 kJ/mol
3rd: 3565 kJ/mol
Atomic radius (calc.) 88 pm
Covalent radius 110 pm
Van der Waals radius 202 pm
Miscellaneous
Magnetic ordering nonmagnetic
Thermal conductivity (300 K) 9.43 mW/(m·K)
Speed of sound (gas, 23 °C) 220 m/s
Speed of sound (liquid) 1120 m/s
CAS registry number 7439-90-9
Notable isotopes
Main article: Isotopes of krypton
iso NA half-life DM DE (MeV) DP
78Kr 0.35% 2.3×1020 y ε ε - 78Se
79Kr syn 35.04 h ε - 79Br
β+ 0.604 79Br
γ 0.26, 0.39,
0.60
-
80Kr 2.25% Kr is stable with 44 neutrons
81Kr syn 2.29×105 y ε - 81Br
γ 0.281 -
82Kr 11.6% Kr is stable with 46 neutrons
83Kr 11.5% Kr is stable with 47 neutrons
84Kr 57% Kr is stable with 48 neutrons
85Kr syn 10.756 y β- 0.687 85Rb
86Kr 17.3% Kr is stable with 50 neutrons

Krypton (chemical symbol Kr, atomic number 36) is a colorless, odorless, tasteless noble gas. It occurs in trace amounts in the atmosphere and is isolated by fractionating liquefied air. Krypton is inert for most practical purposes, but it is known to form compounds with fluorine. Krypton can also form clathrates with water when atoms of it are trapped in a lattice of the water molecules. It is often used with other rare gases in fluorescent lamps.

Occurrence

The concentration of krypton in earth's atmosphere is about 1 part per million (ppm). It can be extracted from liquid air by the technique known as fractional distillation.[1]

History

Krypton (Greek κρυπτός, meaning "hidden") was discovered in Great Britain in 1898 by Sir William Ramsay and Morris Travers. They found it in the residue that remained after evaporating nearly all components of liquid air.

Metric role

In 1960, an international agreement defined the meter in terms of light emitted from a krypton isotope. This agreement replaced the longstanding standard meter located in Paris, which was a metal bar made of platinum-iridium alloy. (The bar was originally estimated to be one ten-millionth of a quadrant of the Earth's polar circumference.) Just 23 years later, the krypton-based standard was replaced by a measure of the speed of light—the most reliable constant in the universe. In October 1983, the Bureau International des Poids et Mesures (International Bureau of Weights and Measures) defined the meter as the distance that light travels in a vacuum during 1/299,792,458 seconds.

Notable characteristics

Image of a krypton-filled discharge tube shaped like the element's atomic symbol.

Its melting point is 156.6 degrees celcius, and its boiling point is 152.3 degrees celcius. The density of krypton is 3.73 grams per liter at STP.

Krypton, a noble gas due to its very low chemical reactivity, is characterized by a brilliant green and orange spectral signature. It is one of the products of uranium fission. Solidified krypton is white and crystalline with a face-centered cubic crystal structure, which is a common property of all "rare gases."

Isotopes

Naturally occurring krypton is made of five stable and one slightly radioactive isotope. Krypton's spectral signature is easily produced with some very sharp lines. Kr-81 is the product of atmospheric reactions with the other naturally occurring isotopes of krypton. It is radioactive with a half-life of 250,000 years. Like xenon, krypton is highly volatile when it is near surface waters and Kr-81 has therefore been used for dating old (50,000 - 800,000 year) groundwater.

Kr-85 is an inert, radioactive noble gas with a half-life of 10.76 years, that is produced by fission of uranium and plutonium. Sources have included nuclear bomb testing, nuclear reactors, and the release of Kr-85 during the reprocessing of fuel rods from nuclear reactors. A strong gradient exists between the northern and southern hemispheres where concentrations at the North Pole are approximately 30% higher than the South Pole due to the fact that most Kr-85 is produced in the northern hemisphere, and north-south atmospheric mixing is relatively slow.

Compounds

Like the other noble gases, krypton is widely considered to be chemically inert. Following the first successful synthesis of xenon compounds in 1962, synthesis of krypton difluoride was reported in 1963. [2] Other fluorides and a salt of a krypton oxoacid have also been found. ArKr+ and KrH+ molecule-ions have been investigated and there is evidence for KrXe or KrXe+.

At the University of Helsinki in Finland, HKrCN and HKrCCH (krypton hydride-cyanide and hydrokryptoacetylene) were synthesized and determined to be stable up to 40K(M. Räsänen et al.). See http://pubs.acs.org/cen/80th/noblegases.html in its paragraph starting "Many recent findings".

Krypton fluoride laser

One major use of krypton is the krypton fluoride laser. Certain amounts of energy are added to force krypton gas to react with fluorine gas to become KrF excited state complex.

The compound will decompose once the energy supply stops. During the decomposition process, the excess energy stored in the excited state complex will be emitted in the form of strong ultraviolet laser radiation.

References
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External links

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