The crystallization process of Fe80P20-xSix amorphous alloys has been
studied by electrical resistivity, X-ray diffraction, neutron diffract
ion, and transmission electron microscopy. This process is classified
into two different patterns with a boundary of 6 at%Si. In the alloys
containing less than 6 at%Si, alpha-Fe and Fe3P, both of which are sta
ble phases, precipitate from the amorphous matrix directly. In the cry
stallization of the amorphous alloys containing over 6 at%Si, two comp
lex phases are observed in the early stages. We found that these two p
hases are isostructural with the alpha-Mn type and beta-Mn type phase.
After these two metastable phases disappear, another metastable phase
which is probably Fe2P appears. In the final stage of the crystalliza
tion, however, existing crystalline phases are stable alpha-Fe (or ord
ered Fe3Si) and Fe3P. In the isothermal crystallization process of the
Fe80P14Si6 amorphous alloy, only the alpha-Mn type phase is observed
as the metastable phase at high temperatures such as 683, 703 and 723
K; however, at a lower temperature such as 668 K, no metastable phase
is observed. The precipitation of the metastable alpha-Mn type and/or
beta-Mn type phases, which consist of the Frank-Kasper coordination po
lyhedra, can be closely related to the local structure in these amorph
ous alloys.