Sb. Rice et al., Empirical identification of uranium oxides and fluorides using electron energy-loss spectroscopy in the transmission electron microscope, MICROS MICR, 5(6), 1999, pp. 437-444
A set of uranium compound particles relevant to contaminated soils and othe
r environmental concerns surrounding uranium bioavailability were studied b
y electron energy-loss spectroscopy (EELS). Core-loss EELS results suggest
that uranium 4(+) compounds have an energy loss resolvable from 6(+) compou
nds. Shoulders on the uranium O-4,O-5 edge further distinguish UO2 from UF4
. Low-loss characteristics distinguish carbon-free uranium oxide specimens
on holey substrates. In the presence of carbon, correction techniques must
be applied. Uranium oxides, fluorides, and minerals show a tendency toward
reduction of uranium toward 4(+) under the beam. The electron dose required
to achieve the transformation from 6(+) to 4(+) is more severe than that u
sually required to obtain satisfactory spectra, but the possibility for red
uction should be considered. The conditions for low-loss analysis need not
be as vigorous as those for core losses, and can be done without altering t
he valence of most oxides.