History
(Gr. molybdos, lead) Before Scheele recognized molybdenite as a distinct ore
of a new element in 1778, it was confused with graphite and lead ore. The metal
was prepared as an impure form in 1782 by Hjelm. Molybdenum does not occur
native, but is obtained principally from molybdenite. Wulfenite, and Powellite
are also minor commercial ores.
Sources
Molybdenum is also recovered as a by-product of copper and tungsten mining
operations. The metal is prepared from the powder made by the hydrogen reduction
of purified molybdic trioxide or ammonium molybdate.
Properties
The metal is silvery white, very hard, but is softer and more ductile than
tungsten. It has a high elastic modulus, and only tungsten and tantalum, of the
more readily available metals, have higher melting points. It is a valuable
alloying agent, as it contributes to the hardenability and toughness of quenched
and tempered steels. It also improves the strength of steel at high
temperatures.
Uses
It is used in certain nickel-based alloys, such as the "Hastelloys(R)" which
are heat-resistant and corrosion-resistant to chemical solutions. Molybdenum
oxidizes at elevated temperatures. The metal has found recent application as
electrodes for electrically heated glass furnaces and foreheaths. The metal is
also used in nuclear energy applications and for missile and aircraft parts.
Molybdenum is valuable as a catalyst in the refining of petroleum. It has found
applications as a filament material in electronic and electrical applications.
Molybdenum is an essential trace element in plant nutrition. Some lands are
barren for lack of this element in the soil. Molybdenum sulfide is useful as a
lubricant, especially at high temperatures where oils would decompose. Almost
all ultra-high strength steels with minimum yield points up to 300,000
psi(lb/in.2)
contain molybdenum in amounts from 0.25 to 8%.
Page Source: Los Alamos National Laboratory
Last Updated: 12/19/97, CST Information Services Team
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