The phase transformation of zirconia from tetragonal to monoclinic is chara
cterized by UV Raman spectroscopy, visible Raman spectroscopy, and XRD. Ele
ctronic absorption Of ZrO2 in the UV region makes UV Raman spectroscopy mor
e sensitive at the surface region than XRD or visible Raman spectroscopy. Z
irconia changes from the tetragonal phase to the monoclinic phase with calc
ination temperatures elevated and monoclinic phase is always detected first
by UV Raman spectroscopy for the samples calcined at lower temperatures th
an that by XRD and visible Raman spectroscopy. When the phase of zirconia c
hanges from tetragonal to monoclinic, the slight changes of the phase at ve
ry beginning can be detected by UV Raman spectroscopy. UV Raman spectra cle
arly indicate that the phase transition takes place initially at the surfac
e regions. It is found that the phase change from tetragonal to monoclinic
is significantly retarded when amorphous Zr(OH)(4) was agglomerated to bigg
er particles and the particle agglomeration of amorphous zirconium hydroxid
e is beneficial to the stabilization of t-ZrO2 phase.