This work investigates the photoluminescence (PL) properties of the cubic chloroperovskite NH4MnCl3.
Like in most concentrated materials, the Mn2+
PL which is located at 2.10 eV at T = 10 K
strongly depends on the temperature. Optical absorption (OA), emission, and
excitation spectroscopy, as well as lifetime measurements, performed on NH4MnCl3
indicate that the PL is mainly intrinsic at T = 10 K
and consists of a broad band located at 2.10 eV. Above this temperature, the PL
gradually transforms to extrinsic PL due to exciton migration and subsequent
trapping. Further temperature increase above 100 K yields transfer to killers of
excitation which are responsible for the PL quenching, and hence the absence of PL
at ambient conditions. The exciton traps are identified with perturbed Mn2+
sites with the effective activation energy of 52 meV, whilst the activation
energy for energy transfer is 47 meV. The existence of these traps has
been directly revealed by time-resolved spectroscopy. The detected
intrinsic and extrinsic PL bands are displaced by 6 meV, which
coincides with the activation energy difference between pure Mn2+ and trap
Mn2+,
as derived from temperature dependence studies of the lifetime τ(T).
Interestingly, a PL band at 1.82 eV is observed above 60 K. This band, which was initially
associated with deeper excitation traps, actually corresponds to precipitates of MnCl2 inside NH4MnCl3.
The correlation analysis performed on NH4MnCl3
using OA, PL, and lifetime data provides an estimate of the precipitate concentration of 0.3 mol%.
The presence of two separated Mn2+
PL bands at different temperatures is a rather common
phenomenon in concentrated materials such as AMnX3 (A = NH4, Rb;
X = Cl,
F), and has been interpreted in terms of exciton transfer to deeper traps. The
present finding stresses the relevance of an adequate structural characterization in
dealing with PL in concentrated materials.