Pressure-composition isotherm and X-ray diffraction studies of ErFe2-H
system have been carried out to resolve the reported controversies re
garding the composition limits of various hydride phases. Further, the
existence of a new plateau in ErFe2Hx for x values between 4 and 5 ha
s been established and the structure of the new hydride phase with x s
imilar or equal to 5 is found to be orthorhombic.