|Name, Symbol, Number||Argon, Ar, 18|
|Chemical series||Noble gases|
|Group, Period, Block||18 (VIIIA), 3 , p|
|Density, Hardness||1.784 kg/m3 (273 K), NA|
|Atomic weight||39.948 amu|
|Atomic radius (calc.)||no data (71) pm|
|Covalent radius||97 pm|
|van der Waals radius||188 pm|
|Electron configuration||[Ne]33s2 3p6|
|e- 's per energy level||2, 8, 8|
|Oxidation states (Oxide)||0 (unknown)|
|Crystal structure||Cubic face centered|
|State of matter||gas (nonmagnetic)|
|Melting point||83.8 K (-308.7 °F)|
|Boiling point||87.3 K (-302.4 °F)|
|Molar volume||22.56 ×1010-3 m3/mol|
|Heat of vaporization||6.447 kJ/mol|
|Heat of fusion||1.188 kJ/mol|
|Speed of sound||319 m/s at 293.15 K|
|Electronegativity||no data (Pauling scale)|
|Specific heat capacity||520 J/(kg*K)|
|Electrical conductivity||no data|
|Thermal conductivity||0.01772 W/(m*K)|
|1st ionization potential||1520.6 kJ/mol|
|2nd ionization potential||2665.8 kJ/mol|
|3rd ionization potential||3931 kJ/mol|
|4th ionization potential||5771 kJ/mol|
|5th ionization potential||7238 kJ/mol|
|6th ionization potential||8781 kJ/mol|
|7th ionization potential||11995 kJ/mol|
|8th ionization potential||13842 kJ/mol|
|Most Stable Isotopes|
|SI units & STP are used except where noted.|
|Table of contents|
6 External Links
Argon is 2.5 times as soluble in water as nitrogen which is approximately the same solubility as oxygen. This chemically inert element is colorless and odorless in both its liquid and gaseous forms. There are no known true chemical compounds that contain argon.
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;
- Used as an inert gas shield in arc welding and cutting,
- as a non-reactive blanket in the manufacture of titanium and other reactive elements,
- as a protective atmosphere for growing silicon and germanium crystals.
- Argon-39 has been used for a number of applications, primarily ice coring. It has also been used for ground water dating
HistoryArgon (Greek argos meaning "lazy") was suspected to be present in air by Henry Cavendish in 1785 but wasn't discovered until 1894 by Lord Rayleigh and Sir William Ramsay.
OccurrenceThis gas is isolated through liquid air fractionation since the atmosphere contains only 0.94% argon. The Martian atmosphere in contrast contains 1.6% of Ar-40 and 5 ppm Ar-36.
IsotopesThe 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 decays to stable Ca-40 (88.8%) by negatron emission. These properties and ratios are used to determine the age of rockss.
In 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 produced from the decay of calcium-40, the result of subsurface nuclear explosions. It has a half-life of 35 days.