Molibdènum: Béda antara owahan

{{Elementbox_isotopes_stable | mn=92 | sym=Mo | na=14.84% | n=50 }}

{{Elementbox_isotopes_decay | mn=93 | sym=Mo

| dm=[[electron capture|ε]] | de=- | pn=93 | ps=[[niobium|Nb]] }}

{{Elementbox_isotopes_stable | mn=94 | sym=Mo | na=9.25% | n=52 }}

| dm2=[[gamma ray|γ]] | de2=0.74, 0.36,<br />0.14| pn2= | ps2=- }}

{{Elementbox_isotopes_decay | mn=100 | sym=Mo

| dm=[[double beta decay|β^-β^-]] | de=3.04 | pn=100 | ps=[[ruthenium|Ru]] }}

{{Elementbox_isotopes_end}}

Though molybdenum is found in such [[mineral]]s as [[wulfenite]] ([[lead|Pb]]Mo[[oxygen|O]]₄) and [[powellite]] ([[calcium|Ca]]Mo[[oxygen|O]]₄), the main commercial source of molybdenum is [[molybdenite]] (Mo[[sulfur|S]]₂). Molybdenum is mined as a principal ore, and is also recovered as a byproduct of copper and tungsten mining.<ref name="CRCdescription" /> Large mines in [[Colorado]] ([[Climax, Colorado|Climax]]) and in [[British Columbia]] yield [[molybdenite]], while many [[porphyry copper]] deposits such as the [[Chuquicamata]] mine in northern [[Chile]] produce molybdenum as a byproduct of copper mining. The Knaben mine in southern Norway was opened in 1885, making it the first molybdenum mine. It remained open until 1973.

 

 

A side product of molybdenum mining is [[rhenium]]. As it is always present in small varying quantities in molybdenite, the only commercial source for rhenium is molybdenum mines.

{{Commons|Molybdenum}}

{{wiktionary|molybdenum}}

 

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[[af:Molibdeen]]

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[[el:Μολυβδένιο]]

[[en:Molybdenum]]