In chemistry, oxypnictides are a class of materials composed of oxygen, a pnictogen (group-V, especially phosphorus and arsenic) and one or more other elements. Although this group of compounds has been recognized since 1995, interest in these compounds increased dramatically after the publication of the superconducting properties of LaOFeP and LaOFeAs which were discovered in 2006 and 2008. In these experiments the oxide was partly replaced by fluoride.
These and related compounds (e.g. the 122 iron arsenides) form a new group of iron-based superconductors known as iron pnictides or ferropnictides since the oxygen is not essential but the iron seems to be.
Oxypnictides have been patented as magnetic in early 2006.H. Hosono et al. (2006) Magnetic semiconductor material European Patent Application EP1868215
The different subclasses of oxypnictides are , oxyphosphides, oxyarsenides, oxyantimonides, and oxybismuthides.
The superconductivity of the oxypnictides seems to depend on the iron-pnictogen layers.
Some found in 2008 to be high-temperature superconductors (up to 55 K) of composition ReOTmPn, where Re is a rare earth, Tm is a transition metal and Pn is from group V e.g. As.
+ oxypnictides !Material ! Tc (K) | |
LaO0.89F0.11FeAs | 26 |
LaO0.9F0.2FeAs | 28.5 |
CeFeAsO0.84F0.16 | 41 |
SmFeAsO0.9F0.1 | 43 |
La0.5Y0.5FeAsO0.6 | 43.1 |
NdFeAsO0.89F0.11 | 52 |
PrFeAsO0.89F0.11 | 52 |
GdFeAsO0.85 | 53.5 |
SmFeAsO~0.85 | 55 |
Tests in magnetic fields up to 45 teslas suggest the upper critical field of LaFeAsO0.89F0.11 may be around 64 T. A different lanthanum-based material tested at 6 K predicts an upper critical field of 122 T in La0.8K0.2FeAsO0.8F0.2.
Practical use
See also
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