Group 4 phosphides, which are typically prepared at high temperatures (>800
degrees C) over several days, are synthesized in self-propagating metathes
is (exchange) reactions in seconds. These reactions produce cubic forms of
zirconium phosphide (ZrP) and hafnium phosphide (HfP) which are normally ma
de at temperatures greater than 1425 degrees C and 1600 degrees C, respecti
vely. To test whether the high temperatures reached in the metathesis react
ions are responsible for the formation of the cubic phases, inert salts are
added to lower the maximum reaction temperatures. The lower temperature re
actions still result in cubic phosphides, although smaller crystallites for
m. Further experiments with phosphorus addition indicate that the phosphoru
s content is not responsible for cubic phase formation. Templating is ruled
out using lattice mismatched KCl and hexagonal ZnS as additives. Therefore
, the direct synthesis of the high-temperature cubic phase in metathesis re
actions appears to be caused by nucleation of the metastable cubic form tha
t is then trapped by rapid cooling. Heating the cubic phase of either ZrP o
r HfP to 1000 degrees C for 18 h, or carrying out metathesis reactions in s
ealed ampules at 1000 degrees C, results only in the hexagonal phase.