Time-of-flight
secondary ion mass spectrometry (TOF-SIMS) is one
of the few techniques that can specifically distinguish between organic
cations such as methylammonium and formamidinium. Distinguishing between
these two species can lead to specific insight into the origins and
evolution of compositional inhomogeneity and chemical gradients in
halide perovskite solar cells, which appears to be a key to advancing
the technology. TOF-SIMS can obtain chemical information from hybrid
organic–inorganic perovskite solar cells (PSCs) in up to three
dimensions, while not simply splitting the organic components into
their molecular constituents (C, H, and N for both methylammonium
and formamidinium), unlike other characterization methods. Here, we
report on the apparently ubiquitous A-site organic cation gradient
measured when doing TOF-SIMS depth-profiling of PSC films. Using thermomechanical
methods to cleave perovskite samples at the buried glass/transparent
conducting oxide interface enables depth profiling in a reverse direction
from normal depth profiling (backside depth profiling). When comparing
the backside depth profiles to the traditional front side profiled
devices, an identical slight gradient in the A-site organic cation
signal is observed in each case. This indicates that the apparent
A-site cation gradient is a measurement artifact due to beam damage
from the primary ion beam causing a continually decreasing ion yield
for secondary ions of methylammonium and formamidinium. This is due
to subsurface implantation and bond breaking from the 30 keV bismuth
primary ion beam impact when profiling with too high of a data density.
Here, we show that the beam-generated artifact associated with this
damage can mostly be mitigated by altering the measurement conditions.
We also report on a new method of depth profiling applied to PSC films
that enables enhanced sensitivity to halide ions in positive measurement
polarity, which can eliminate the need for a second measurement in
negative polarity in most cases.