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The
Material that changes its dimension in the magntic field, as first
discovered in 1842 by James Joule, is called magnetostrictive effect.
The traditional magnetostrictive material such as iron, nickel, ferrite
piezoceramic etc. are of low magnetostriction. In the early 1970s, A.E
Clark and coworkers discovered that rare earth binary alloys TbFe2,
DyFe2, SmFe2 etc. have very large
magnetostriction above room temperatures however with high anisotropy
which means very large field will be needed to get suturation, and this
causes great difficulty in practical applications. In solving this
problem, pseodobinary alloys were studied which led to the discovery of
TbxDy1-xFe2-y material possessing
giant magnetostriction with low anisotropy. Grain-oriented TbxDy1-xFe2-y
single crystal or multicrystal materials exhibit "jump
effect" which means that the magnetostriction increases
drastically in the presence of prestress. From then on, the practical
application of this material became possible, therefore attracting
widespread attention from industry.
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By
alloying the two compounds it was found that the magnetic field
required to produce saturated strains were considerably reduced. The
resulting alloy Tb0.27Dy 0.73 Fe1.95
(commercially known as Terfenol-D) is at present
the most widely used magnetostrictive material. Terfenol is capable of
strains as high as 1500ppm and, since the 1980's, has been a
commercially available material for application in a great many fields.
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