The aim of this work is to investigate the origin of the piezochromism and
thermochromism exhibited by the copper oxide CuMoO4. These optical phenomen
a are associated with structural phase transition (PT) from the triclinic a
lpha (green) modification to the gamma (brownish-red) modification. The var
iation of the optical-absorption spectrum with pressure and temperature ind
icates that the piezochromic and thermochromic transitions can be leached f
rom ambient conditions either by applying pressure at 2.5 kbar or by coolin
g at T = 200 K. We show that the change of color at the alpha --> gamma PT
is due to the broadening of the first O2- --> Cu2+ charge-transfer band, an
d the disappearance of an intense peak at 1.49 eV, related to the presence
of pyramidal CuO5 complexes in alpha-CuMoO4. The measured oscillator streng
th suggests that this peak corresponds to the e-->b(1) crystal-field transi
tion within CuO5 rather than to an O2---> Cu2+ charge-transfer band. The co
rrelation between optical and structural properties performed in this work
confirms this interpretation, and also explains the strong dichroism exhibi
ted by the crystal in the high-pressure gamma- CuMoO4 modification.