Al1–x
Gd
x
N is one of a series of novel heterostructural alloys
involving
rare earth cations with potentially interesting properties for (opto)electronic,
magnetic, and neutron detector applications. Using alloy models in
conjunction with density functional theory, we explored the full composition
range for Al1–x
Gd
x
N and found that wurtzite is the ground-state structure up
to a critical composition of x
c = 0.82.
The calculated temperature-composition phase diagram reveals a large
miscibility gap inducing spinodal decomposition at equilibrium conditions,
with higher Gd substitution (meta)stabilized at higher temperatures.
By depositing combinatorial thin films at high effective temperatures
using radio-frequency cosputtering, we have achieved the highest Gd3+ incorporation into the wurtzite phase reported to date,
with single-phase compositions at least up to x ≈
0.25 confirmed by high-resolution synchrotron grazing incidence wide-angle
X-ray scattering. High-resolution transmission electron microscopy
on material with x ≈ 0.13 and x ≈ 0.24 confirmed a uniform composition polycrystalline film
with uniform columnar grains having the wurtzite structure. Spectroscopic
ellipsometry and cathodoluminescence spectroscopy measurements are
employed to probe the optoelectronic properties, showing that the
band gap decreases with increasing Gd content x and
that this effect causes the ideal Gd substitution level for cathodoluminescence
applications to be low. Expanding our calculations to other rare earth
cations (Pr3+ and Tb3+) reveals similar thermodynamic
stability and solubility behavior to Gd. From this and previous studies
on Al1–x
Sc
x
N, we elucidate that both smaller ionic radius and higher bond
ionicity promote increased incorporation of group IIIB cations into
wurtzite AlN. This work furthers the development of design rules for
new alloys in this material family.