Zirconolite
is considered to be a suitable wasteform material for
the immobilization of Pu and other minor actinide species produced
through advanced nuclear separations. Here, we present a comprehensive
investigation of Dy
3+
incorporation within the self-charge
balancing zirconolite Ca
1–
x
Zr
1–
x
Dy
2
x
Ti
2
O
7
solid solution, with the view to simulate
trivalent minor actinide immobilization. Compositions in the substitution
range 0.10 ≤
x
≤ 1.00 (Δ
x
= 0.10) were fabricated by a conventional mixed oxide
synthesis, with a two-step sintering regime at 1400 °C in air
for 48 h. Three distinct coexisting phase fields were identified,
with single-phase zirconolite-2M identified only for
x
= 0.10. A structural transformation from zirconolite-2M to zirconolite-4M
occurred in the range 0.20 ≤
x
≤ 0.30,
while a mixed-phase assemblage of zirconolite-4M and cubic pyrochlore
was evident at Dy concentrations 0.40 ≤
x
≤
0.50. Compositions for which
x
≥ 0.60 were
consistent with single-phase pyrochlore. The formation of zirconolite-4M
and pyrochlore polytype phases, with increasing Dy content, was confirmed
by high-resolution transmission electron microscopy, coupled with
selected area electron diffraction. Analysis of the Dy L
3
-edge XANES region confirmed that Dy was present uniformly as Dy
3+
, remaining analogous to Am
3+
. Fitting of the
EXAFS region was consistent with Dy
3+
cations distributed
across both Ca
2+
and Zr
4+
sites in both zirconolite-2M
and 4M, in agreement with the targeted self-compensating substitution
scheme, whereas Dy
3+
was 8-fold coordinated in the pyrochlore
structure. The observed phase fields were contextualized within the
existing literature, demonstrating that phase transitions in CaZrTi
2
O
7
–REE
3+
Ti
2
O
7
binary solid solutions are fundamentally controlled by the ratio
of ionic radius of REE
3+
cations.