Isolation
of high-level radioactive waste (HLW) in deep geological
repositories (DGR) through a multibarrier concept is the most accepted
approach to ensure long-term safety. Clay minerals are one of the
most promising materials to be used as engineered barriers. In particular,
high charge micas, as components of the engineered barrier, show superselectivity
for some radioactive isotopes and a large adsorption capacity, which
is almost twice that of the other low charge aluminosilicates. In
addition, high charge micas are optimum candidates for decontamination
of nuclear waste through two different mechanisms; namely an ion exchange
reaction and a nonreversible mechanism involving the formation of
new stable crystalline phases under hydrothermal conditions. In this
work, we report a new in situ optical sensor based on the incorporation
of Eu3+ in these high charge micas for tracking the long-term
physical-chemical behavior of HLW contaminants in DRG under mild hydrothermal
conditions. The incorporation of Eu3+ into the interlayer
space of the mica originates a well resolved green and red luminescence,
from both the 5D1 and 5D0 excited states, respectively. The formation of new crystalline phases
under hydrothermal conditions involves important changes in the Eu3+ emission spectra and lifetime. The most interesting features
of Eu3+ luminescence to be used as an optical sensor are
(1) the presence or absence of the Eu3+ green emission
from the 5D1 excited state, (2) the energy shift
of the 5D0 → 7F0 transition, (3) the crystal-field splitting of the 7F1 Eu3+ level, and (4) the observed luminescence
lifetimes, which are directly related to the interaction mechanisms
between the lanthanide ions and the silicate network.