Argon

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Argon was also a codename used for the KH-5 reconnaissance satellite. The Eye of Argon is an infamous fantasy novella.
18 chlorineargon-
Ne

Ar

Kr
General
Name, Symbol, Number argon, Ar, 18
Chemical series noble gases
Group, Period, Block 18, 3, p
Appearance colorless
Atomic mass 39.948(1) g/mol
Electron configuration [Ne] 3s2 3p6
Electrons per shell 2, 8, 8
Physical properties
Phase gas
Melting point 83.80 K
(-189.35 °C, -308.83 °F)
Boiling point 87.30 K
(-185.85 °C, -302.53 °F)
Heat of fusion 1.18 kJ/mol
Heat of vaporization 6.43 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   47 53 61 71 87
Atomic properties
Crystal structure cubic face centered
Oxidation states 0
Electronegativity no data (Pauling scale)
Ionization energies
(more)
1st: 1520.6 kJ/mol
2nd: 2665.8 kJ/mol
3rd: 3931 kJ/mol
Atomic radius 71 pm
Atomic radius (calc.) 71 pm
Covalent radius 97 pm
Van der Waals radius 188 pm
Miscellaneous
Magnetic ordering nonmagnetic
Thermal conductivity (300 K) 17.72 mW/(m·K)
Speed of sound (gas, 27 °C) 323 m/s
CAS registry number 7440-37-1
Notable isotopes
Main article: Isotopes of argon
iso NA half-life DM DE (MeV) DP
36Ar 0.337% Ar is stable with 18 neutrons
37Ar syn 35 d ε  ? 37Cl
38Ar 0.063% Ar is stable with 20 neutrons
39Ar syn 269 y β- 0.565 39K
40Ar 99.600% Ar is stable with 22 neutrons
42Ar syn 32.9 y β- 0.600 42K
References

Argon is the chemical element in the periodic table that has the symbol Ar and atomic number 18. The third noble gas, in group 18, argon makes up about 1% of the Earth's atmosphere.

Contents

Notable characteristics

Argon is 2.5 times as soluble in water as nitrogen which is approximately the same solubility as oxygen. This highly stable chemical element is colorless and odorless in both its liquid and gaseous forms. There are no known true chemical compounds that contain argon, one of the reasons it was formerly called an inert gas. The creation of argon hydrofluoride (HArF), a highly unstable compound of argon with fluorine, was reported by researchers at the University of Helsinki in 2000, but has not been confirmed.

Although no chemical compounds of argon are presently confirmed, argon can form clathrates with water when atoms of it are trapped in a lattice of the water molecules. Theoretical calculations on computers have shown several Argon compounds that should be stable but for which no synthesis routes are currently known.

Applications

It is used in lighting since it will not react with the filament in a lightbulb even under high temperatures and other cases where diatomic nitrogen is an unsuitable (semi-)inert gas. Other uses;

Argon is also used in technical SCUBA diving to inflate the dry suit, due to its nonreactive, heat isolating effect.

History

Argon (Greek argos meaning "inactive") was suspected to be present in air by Henry Cavendish in 1785 but was not discovered until 1894 by Lord Rayleigh and Sir William Ramsay.

Occurrence

This gas is isolated through liquid air fractionation since the atmosphere contains only 0.934% volume of argon (1.29% mass). The Martian atmosphere in contrast contains 1.6% of Ar-40 and 5 ppm Ar-36. In 2005, the Huygens probe also discoverd the presence of Ar-40 on Titan, the largest moon of Saturn [1] (http://www.esa.int/esaCP/SEMHB881Y3E_index_0.html).

Compounds

Before 1962, argon and the other noble gases were generally considered to be chemically inert and not able to form compounds. However, since then, scientists have been able to force the heavier noble gases to form compounds. In 2000, the first argon compounds were formed by researchers at the University of Helsinki. By shining ultraviolet light onto frozen argon containing a small amount of hydrogen fluoride, they were able to form argon hydrofluoride (HArF).

Isotopes

The main isotopes of argon found on Earth are Ar-40, Ar-36, and Ar-38. Naturally occurring K-40 with a half-life of 1.250 x 109 years, decays to stable Ar-40 (11.2%) by electron capture and by positron emission, and also transforms to stable Ca-40 (88.8%) via beta decay. These properties and ratios are used to determine the age of rocks.

In the Earth's atmosphere, Ar-39 is made by cosmic ray activity, primarily with Ar-40. In the subsurface environment, it is also produced through neutron capture by K-39 or alpha emission by calcium. Argon-37 is created from the decay of calcium-40 as a result of subsurface nuclear explosions. It has a half-life of 35 days.

References

External links

ar:أرغون (عنصر) bg:Аргон ca:Argó cs:Argon cy:Argon da:Argon de:Argon eo:Argono es:Argón et:Argoon fi:Argon fr:Argon he:ארגון (יסוד) hr:Argon hu:Argon id:Argon io:Argono is:Argon it:Argon ja:アルゴン ko:아르곤 mi:Argon ms:Argon nl:Argon nn:Argon no:Argon pl:Argon pt:Argon ru:Аргон simple:Argon sl:Argon sr:Неон sv:Argon uk:Аргон zh:氩

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