Argon (Ar)
Stable isotopes of argon available from ISOFLEX
Isotope | Z(p) | N(n) | Atomic Mass | Natural Abundance | Enrichment Level | Physical Form |
Ar-36 | 18 | 18 | 35.9675462 | 0.34% | ≥99.90% | Gas |
Ar-38 | 18 | 20 | 37.9627322 | 0.06% | 99.90% | Gas |
Ar-40 | 18 | 22 | 39.96238312 | 99.60% | 99.99% | Gas |
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Argon was discovered in 1894 by Sir William Ramsay and Lord Rayleigh. Its name derives from the Greek word argos, meaning “inactive.” Today the chemical symbol for argon is Ar, but until 1957 its symbol was simply A.
Argon is a colorless and odorless gas that is present to a very small extent in the atmosphere. It is practically insoluble in water. It makes a good atmosphere for working with air-sensitive materials since it is heavier than air and less reactive than N2. It is an effective “blanket” for the production of titanium and other reactive elements. It provides a protective atmosphere for growing silicon and germanium crystals.
Commercial applications for argon include its use in electric light bulbs and in fluorescent tubes. It is also used as an inert gas shield for arc welding and cutting.
Properties of Argon
Name | Argon |
Symbol | Ar |
Atomic number | 18 |
Atomic weight | 39.948 |
Standard state | Gas at 298 ºK |
CAS Registry ID | 7440-37-1 |
Group in periodic table | 18 |
Group name | Noble gas |
Period in periodic table | 3 |
Block in periodic table | p-block |
Color | Colorless |
Classification | Nonmetallic |
Melting point | -189.3 ºC |
Boiling point | -185.8 ºC |
Thermal conductivity | 0.01772 W/(m-K) |
Heat of vaporization | 6.5 kJ·mol-1 |
Heat of fusion | 1.18 kJ·mol-1 |
Density | 1.784 g/cm3 |
Electron configuration | [Ne]3s23p6 |
Oxidation state | 0 |
Research
- Volatile element isotopes of submarine hydrothermal mineral deposits in the western Pacific
- New 40Ar/39Ar ages from the Kalatag district in the Eastern Tianshan, NW China: Constraints on the timing of Cu mineralization and stratigraphy
- B isotopes of Carboniferous-Permian volcanic rocks in the Tuha basin mirror a transition from subduction to intraplate setting in Central Asian Orogenic Belt