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| Name, Symbol, Number | argon, Ar, 18 | ||||||||||||||||||||||||||||||||||||||||||||||||
| Chemical series | noble gases | ||||||||||||||||||||||||||||||||||||||||||||||||
| Group, Period, Block | 18, 3, p | ||||||||||||||||||||||||||||||||||||||||||||||||
| Appearance | colorless![]() |
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| Atomic mass | 39.948(1) g/mol | ||||||||||||||||||||||||||||||||||||||||||||||||
| Electron configuration | [Ne] 3s2 3p6 | ||||||||||||||||||||||||||||||||||||||||||||||||
| Electrons per shell | 2, 8, 8 | ||||||||||||||||||||||||||||||||||||||||||||||||
| Physical properties | |||||||||||||||||||||||||||||||||||||||||||||||||
| Phase | gas (At room temperature) | ||||||||||||||||||||||||||||||||||||||||||||||||
| Density | (0 °C, 101.325 kPa) 1.784 g/L |
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| Melting point | 83.80 K (-189.35 °C, -308.83 °F) |
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| Boiling point | 87.30 K (-185.85 °C, -302.53 °F) |
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| Critical point | 150.87 K, 4.898 MPa | ||||||||||||||||||||||||||||||||||||||||||||||||
| Heat of fusion | 1.18 kJ·mol−1 | ||||||||||||||||||||||||||||||||||||||||||||||||
| Heat of vaporization | 6.43 kJ·mol−1 | ||||||||||||||||||||||||||||||||||||||||||||||||
| Heat capacity | (25 °C) 20.786 J·mol−1·K−1 | ||||||||||||||||||||||||||||||||||||||||||||||||
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| Atomic properties | |||||||||||||||||||||||||||||||||||||||||||||||||
| Crystal structure | cubic face centered | ||||||||||||||||||||||||||||||||||||||||||||||||
| Oxidation states | 0 | ||||||||||||||||||||||||||||||||||||||||||||||||
| Electronegativity | no data (Pauling scale) | ||||||||||||||||||||||||||||||||||||||||||||||||
| Ionization energies (more) |
1st: 1520.6 kJ·mol−1 | ||||||||||||||||||||||||||||||||||||||||||||||||
| 2nd: 2665.8 kJ·mol−1 | |||||||||||||||||||||||||||||||||||||||||||||||||
| 3rd: 3931 kJ·mol−1 | |||||||||||||||||||||||||||||||||||||||||||||||||
| 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−1·K−1 | ||||||||||||||||||||||||||||||||||||||||||||||||
| Speed of sound | (gas, 27 °C) 323 m/s | ||||||||||||||||||||||||||||||||||||||||||||||||
| CAS registry number | 7440-37-1 | ||||||||||||||||||||||||||||||||||||||||||||||||
| Selected isotopes | |||||||||||||||||||||||||||||||||||||||||||||||||
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| References | |||||||||||||||||||||||||||||||||||||||||||||||||
Argon (IPA: /ˈɑːgɒn/) is a chemical element designated by the symbol Ar. Argon has atomic number 18 and is the third element in group 18 of the periodic table (noble gases). Argon is present in the Earth's atmosphere at slightly less than 1%, making it the most common noble gas on Earth.
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Argon has approximately the same solubility in water as oxygen gas and is 2.5 times more soluble in water than nitrogen gas.[1] This highly stable chemical element is colorless, odorless, tasteless and nontoxic in both its liquid and gaseous forms. Argon is inert under most conditions and forms no confirmed stable compounds at room temperature. The creation of argon hydrofluoride (HArF), a metastable compound of argon with fluorine and hydrogen, was first reported by researchers at the University of Helsinki in 2000.
Although the neutral ground-state chemical compounds of argon are presently limited to HArF, argon can form clathrates with water when atoms of it are trapped in a lattice of the water molecules. Also argon-containing ions e.g. ArH+ and excited state complexes e.g. ArF are well known. Theoretical calculations on computers have shown several argon compounds that should be stable but for which no synthesis routes are currently known.
Argon is used in incandescent lighting and other applications in which diatomic nitrogen is not sufficiently inert. Argon will not react with the filament of light bulbs even at high temperatures. Other uses:
Argon (Greek αργός 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 in an experiment in which they removed all of the oxygen and nitrogen from the air. Argon was also encountered in 1882 through independent research of H.F. Newall and W.N. Hartley. Each observed new lines in the color spectrum of air but were unable to identify the element responsible for the lines. Argon became the first member of the noble gases to be discovered.
The symbol for Argon is now Ar, but up until 1957 it was A.[2]
Argon constitutes 0.934% by volume and 1.29% by mass of the Earth's atmosphere, and air is the primary raw material used by industry to produce purified argon products. Argon is isolated from air by fractionation, most commonly by cryogenic fractional distillation, a process that also produces purified nitrogen, oxygen, neon, krypton and xenon.
The Martian atmosphere in contrast contains 1.6% of argon-40 and 5 ppm of argon-36. The Mariner spaceprobe fly-by of the planet Mercury in 1973 found that Mercury has a very thin atmosphere with 70% argon, believed to result from releases of the gas as a decay product from radioactive materials on the planet. In 2005, the Huygens probe also discovered the presence of argon-40 on Titan, the largest moon of Saturn.[3]
Argon’s complete octet of electrons indicates full s and p subshells. This full outer energy level makes argon very stable and extremely resistant to bonding with other elements. Before 1962, argon and the other noble gases were considered to be chemically inert and unable to form compounds; however, compounds of the heavier noble gases have since been synthesized. 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, argon hydrofluoride (HArF) was formed.[4] It is stable up to 40 kelvins (−233 °C).
The main isotopes of argon found on Earth are 40Ar, 36Ar, and 38Ar. Naturally occurring 40K with a half-life of 1.250×109 years, decays to stable 40Ar (11.2%) by electron capture and by positron emission, and also transforms to stable 40Ca (88.8%) via beta decay. These properties and ratios are used to determine the age of rocks.
In the Earth's atmosphere, 39Ar is made by cosmic ray activity, primarily with 40Ar. In the subsurface environment, it is also produced through neutron capture by 39K or alpha emission by calcium. 37Ar is created from the decay of 40Ca as a result of subsurface nuclear explosions. It has a half-life of 35 days.
| E numbers | ||
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| Colours (E100-199) • Preservatives (E200-299) • Antioxidants & Acidity regulators (E300-399) • Thickeners, stabilisers & emulsifiers (E400-499) • pH regulators & anti-caking agents (E500-599) • Flavour enhancers (E600-699) • Miscellaneous (E900-999) • Additional chemicals (E1100-1599) | ||
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| Waxes (E900-909) • Synthetic glazes (E910-919) • Improving agents (E920-929) • Packaging gases (E930-949) • Sweeteners (E950-969) • Foaming agents (E990-999) | ||
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| Argon (E938) • Helium (E939) • Dichlorodifluoromethane (E940) • Nitrogen (E941) • Nitrous oxide (E942) • Butane (E943a) • Isobutane (E943b) • Propane (E944) • Oxygen (E948) • Hydrogen (E949) | ||
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