Variation in Mg content lit the pyrochlore phase of composition Pb1.83
Mg0.29+xNb1.71-xO6.39-1.5x, where 0.1 less than or equal to x less tha
n or equal to 0.522, resulted in the formation of PMN perovskite and w
hen x=0.522, near pure perovskite phase was obtained. Sintering temper
ature also played an effective role in the formation of perovskite in
the pyrochlore. For small amounts of excess Mg, the perovskite general
ly existed as inter- and intragranular inclusion particles with occasi
onal clusters of perovskite grains, and when x greater than or equal t
o 0.4, pyrochlore became the minor phase and perovskite formed the mat
rix. Invariably, Mg rich phases were also observed in the microstructu
re. Dielectric measurements sheaved that the relative permittivity of
the mixtures increased with Mg concentration as a result of a decrease
in the pyrochlore content. (C) 1997 The Institute of Materials.