10 research outputs found
Pressure-Induced Conductivity and Yellow-to-Black Piezochromism in a Layered Cu–Cl Hybrid Perovskite
Pressure-induced
changes in the electronic structure of two-dimensional
Cu-based materials have been a subject of intense study. In particular,
the possibility of suppressing the Jahn–Teller distortion of
d<sup>9</sup> Cu centers with applied pressure has been debated over
a number of decades. We studied the structural and electronic changes
resulting from the application of pressures up to ca. 60 GPa on a
two-dimensional copperÂ(II)–chloride perovskite using diamond
anvil cells (DACs), through a combination of in situ powder X-ray
diffraction, electronic absorption and vibrational spectroscopy, dc
resistivity measurements, and optical observations. Our measurements
show that compression of this charge-transfer insulator initially
yields a first-order structural phase transition at ca. 4 GPa similar
to previous reports on other Cu<sup>II</sup>–Cl perovskites,
during which the originally translucent yellow solid turns red. Further
compression induces a previously unreported phase transition at ca.
8 GPa and dramatic piezochromism from translucent red-orange to opaque
black. Two-probe dc resistivity measurements conducted within the
DAC show the first instance of appreciable conductivity in Cu<sup>II</sup>–Cl perovskites. The conductivity increases by 5 orders
of magnitude between 7 and 50 GPa, with a maximum measured conductivity
of 2.9 × 10<sup>–4</sup> S·cm<sup>–1</sup> at 51.4 GPa. Electronic absorption spectroscopy and variable-temperature
conductivity measurements indicate that the perovskite behaves as
a 1.0 eV band-gap semiconductor at 39.7 GPa and has an activation
energy for electronic conduction of 0.232(1) eV at 40.2 GPa. Remarkably,
all these changes are reversible: the material reverts to a translucent
yellow solid upon decompression, and ambient pressure powder X-ray
diffraction data taken before and after compression up to 60 GPa show
that the original structure is maintained with minimal hysteresis
Pressure-Induced Metallization of the Halide Perovskite (CH<sub>3</sub>NH<sub>3</sub>)PbI<sub>3</sub>
We report the metallization of the
hybrid perovskite semiconductor
(MA)ÂPbI<sub>3</sub> (MA = CH<sub>3</sub>NH<sub>3</sub><sup>+</sup>) with no apparent structural transition. We tracked its bandgap
evolution during compression in diamond-anvil cells using absorption
spectroscopy and observed strong absorption over both visible and
IR wavelengths at pressures above ca. 56 GPa, suggesting the imminent
closure of its optical bandgap. The metallic character of (MA)ÂPbI<sub>3</sub> above 60 GPa was confirmed using both IR reflectivity and
variable-temperature dc conductivity measurements. The impressive
semiconductor properties of halide perovskites have recently been
exploited in a multitude of optoelectronic applications. Meanwhile,
the study of metallic properties in oxide perovskites has revealed
diverse electronic phenomena. Importantly, the mild synthetic routes
to halide perovskites and the templating effects of the organic cations
allow for fine structural control of the inorganic lattice. Pressure-induced
closure of the 1.6 eV bandgap in (MA)ÂPbI<sub>3</sub> demonstrates
the promise of the continued study of halide perovskites under a range
of thermodynamic conditions, toward realizing wholly new electronic
properties
Hydrogen-Bond Symmetrization Breakdown and Dehydrogenation Mechanism of FeO<sub>2</sub>H at High Pressure
The cycling of hydrogen plays an
important role in the geochemical
evolution of our planet. Under high-pressure conditions, asymmetric
hydroxyl bonds tend to form a symmetric O–H–O configuration
in which H is positioned at the center of two O atoms. The symmetrization
of O–H bonds improves their thermal stability and as such,
water-bearing minerals can be present deeper in the Earth’s
lower mantle. However, how exactly H is recycled from the deep mantle
remains unclear. Here, we employ first-principles free-energy landscape
sampling methods together with high pressure-high temperature experiments
to reveal the dehydrogenation mechanism of a water-bearing mineral,
FeO<sub>2</sub>H, at deep mantle conditions. Experimentally, we show
that ∼50% H is released from symmetrically hydrogen-bonded
ε-FeO<sub>2</sub>H upon transforming to a pyrite-type phase
(Py-phase). By resolving the lowest-energy transition pathway from
ε-FeO<sub>2</sub>H to the Py-phase, we demonstrate that half
of the O–H bonds in the mineral rupture during the structural
transition, leading toward the breakdown of symmetrized hydrogen bonds
and eventual dehydrogenation. Our study sheds new light on the stability
of symmetric hydrogen bonds during structural transitions and provides
a dehydrogenation mechanism for hydrous minerals existing in the deep
mantle
High-Pressure Single-Crystal Structures of 3D Lead-Halide Hybrid Perovskites and Pressure Effects on their Electronic and Optical Properties
We report the first high-pressure single-crystal structures of
hybrid perovskites. The crystalline semiconductors (MA)ÂPbX<sub>3</sub> (MA = CH<sub>3</sub>NH<sub>3</sub><sup>+</sup>, X = Br<sup>–</sup> or I<sup>–</sup>) afford us the rare opportunity of understanding
how compression modulates their structures and thereby their optoelectronic
properties. Using atomic coordinates obtained from high-pressure single-crystal
X-ray diffraction we track the perovskites’ precise structural
evolution upon compression. These structural changes correlate well
with pressure-dependent single-crystal photoluminescence (PL) spectra
and high-pressure bandgaps derived from density functional theory.
We further observe dramatic piezochromism where the solids become
lighter in color and then transition to opaque black with compression.
Indeed, electronic conductivity measurements of (MA)ÂPbI<sub>3</sub> obtained within a diamond-anvil cell show that the material’s
resistivity decreases by 3 orders of magnitude between 0 and 51 GPa.
The activation energy for conduction at 51 GPa is only 13.2(3) meV,
suggesting that the perovskite is approaching a metallic state. Furthermore,
the pressure response of mixed-halide perovskites shows new luminescent
states that emerge at elevated pressures. We recently reported that
the perovskites (MA)ÂPbÂ(Br<sub><i>x</i></sub>I<sub>1–<i>x</i></sub>)<sub>3</sub> (0.2 < <i>x</i> < 1)
reversibly form light-induced trap states, which pin their PL to a
low energy. This may explain the low voltages obtained from solar
cells employing these absorbers. Our high-pressure PL data indicate
that compression can mitigate this PL redshift and may afford higher
steady-state voltages from these absorbers. These studies show that
pressure can significantly alter the transport and thermodynamic properties
of these technologically important semiconductors
Effects of Molecular Geometry on the Properties of Compressed Diamondoid Crystals
Diamondoids
are an intriguing group of carbon-based nanomaterials,
which combine desired properties of inorganic nanomaterials and small
hydrocarbon molecules with atomic-level uniformity. In this Letter,
we report the first comparative study on the effect of pressure on
a series of diamondoid crystals with systematically varying molecular
geometries and shapes, including zero-dimensional (0D) adamantane;
one-dimensional (1D) diamantane, [121]Âtetramantane, [123]Âtetramantane,
and [1212]Âpentamantane; two-dimensional (2D) [12312]Âhexamantane; and
three-dimensional (3D) triamantane and [1Â(2,3)Â4]Âpentamantane. We find
the bulk moduli of these diamondoid crystals are strongly dependent
on the diamondoids’ molecular geometry with 3D [1Â(2,3)Â4]Âpentamantane
being the least compressible and 0D adamantane being the most compressible.
These diamondoid crystals possess excellent structural rigidity and
are able to sustain large volume deformation without structural failure
even after repetitive pressure loading cycles. These properties are
desirable for constructing cushioning devices. We also demonstrate
that lower diamondoids outperform the conventional cushioning materials
in both the working pressure range and energy absorption density
Strain-Induced Modification of Optical Selection Rules in Lanthanide-Based Upconverting Nanoparticles
NaYF<sub>4</sub>:Yb<sup>3+</sup>,Er<sup>3+</sup> nanoparticle upconverters
are hindered by low quantum efficiencies arising in large part from
the parity-forbidden nature of their optical transitions and the nonoptimal
spatial separations between lanthanide ions. Here, we use pressure-induced
lattice distortion to systematically modify both parameters. Although
hexagonal-phase nanoparticles exhibit a monotonic decrease in upconversion
emission, cubic-phase particles experience a nearly 2-fold increase
in efficiency. In-situ X-ray diffraction indicates that these emission
changes require only a 1% reduction in lattice constant. Our work
highlights the intricate relationship between upconversion efficiency
and lattice geometry and provides a promising approach to modifying
the quantum efficiency of any lanthanide upconverter
Strain-Induced Modification of Optical Selection Rules in Lanthanide-Based Upconverting Nanoparticles
NaYF<sub>4</sub>:Yb<sup>3+</sup>,Er<sup>3+</sup> nanoparticle upconverters
are hindered by low quantum efficiencies arising in large part from
the parity-forbidden nature of their optical transitions and the nonoptimal
spatial separations between lanthanide ions. Here, we use pressure-induced
lattice distortion to systematically modify both parameters. Although
hexagonal-phase nanoparticles exhibit a monotonic decrease in upconversion
emission, cubic-phase particles experience a nearly 2-fold increase
in efficiency. In-situ X-ray diffraction indicates that these emission
changes require only a 1% reduction in lattice constant. Our work
highlights the intricate relationship between upconversion efficiency
and lattice geometry and provides a promising approach to modifying
the quantum efficiency of any lanthanide upconverter
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Bright, Mechanosensitive Upconversion with Cubic-Phase Heteroepitaxial Core–Shell Nanoparticles
Lanthanide-doped
nanoparticles are an emerging class of optical
sensors, exhibiting sharp emission peaks, high signal-to-noise ratio,
photostability, and a ratiometric color response to stress. The same
centrosymmetric crystal field environment that allows for high mechanosensitivity
in the cubic-phase (α), however, contributes to low upconversion
quantum yield (UCQY). In this work, we engineer brighter mechanosensitive
upconverters using a core–shell geometry. Sub-25 nm α-NaYF<sub>4</sub>:Yb,Er cores are shelled with an optically inert surface passivation
layer of ∼4.5 nm thickness. Using different shell materials,
including NaGdF<sub>4</sub>, NaYF<sub>4</sub>, and NaLuF<sub>4</sub>, we study how compressive to tensile strain influences the nanoparticles’
imaging and sensing properties. All core–shell nanoparticles
exhibit enhanced UCQY, up to 0.14% at 150 W/cm<sup>2</sup>, which
rivals the efficiency of unshelled hexagonal-phase (β) nanoparticles.
Additionally, strain at the core–shell interface can tune mechanosensitivity.
In particular, the compressive Gd shell results in the largest color
response from yellow-green to orange or, quantitatively, a change
in the red to green ratio of 12.2 ± 1.2% per GPa. For all samples,
the ratiometric readouts are consistent over three pressure cycles
from ambient to 5 GPa. Therefore, heteroepitaxial shelling significantly
improves signal brightness without compromising the core’s
mechano-sensing capabilities and further, promotes core–shell
cubic-phase nanoparticles as upcoming in vivo and in situ optical
sensors
Upconverting Nanoparticles as Optical Sensors of Nano- to Micro-Newton Forces
Mechanical forces affect a myriad
of processes, from bone growth
to material fracture to touch-responsive robotics. While nano- to
micro-Newton forces are prevalent at the microscopic scale, few methods
have the nanoscopic size and signal stability to measure them in vivo
or in situ. Here, we develop an optical force-sensing platform based
on sub-25 nm NaYF<sub>4</sub> nanoparticles (NPs) doped with Yb<sup>3+</sup>, Er<sup>3+</sup>, and Mn<sup>2+</sup>. The lanthanides Yb<sup>3+</sup> and Er<sup>3+</sup> enable both photoluminescence and upconversion,
while the energetically coupled <i>d</i>-metal Mn<sup>2+</sup> adds force tunability through its crystal field sensitivity. Using
a diamond anvil cell to exert up to 3.5 GPa pressure or ∼10
μN force per particle, we track stress-induced spectral responses.
The red (660 nm) to green (520, 540 nm) emission ratio varies linearly
with pressure, yielding an observed color change from orange to red
for α-NaYF<sub>4</sub> and from yellow–green to green
for <i>d</i>-metal optimized β-NaYF<sub>4</sub> when
illuminated in the near infrared. Consistent readouts are recorded
over multiple pressure cycles and hours of illumination. With the
nanoscopic size, a dynamic range of 100 nN to 10 μN, and photostability,
these nanoparticles lay the foundation for visualizing dynamic mechanical
processes, such as stress propagation in materials and force signaling
in organisms
A<sub>2</sub>TiO<sub>5</sub> (A = Dy, Gd, Er, Yb) at High Pressure
The
structural evolution of lanthanide A<sub>2</sub>TiO<sub>5</sub> (A
= Dy, Gd, Yb, Er) at high pressure is investigated using synchrotron
X-ray diffraction. The effects of A-site cation size and of the initial
structure are systematically examined by varying the composition of
the isostructural lanthanide titanates and the structure of dysprosium
titanate polymorphs (orthorhombic, hexagonal, and cubic), respectively.
All samples undergo irreversible high-pressure phase transformations,
but with different onset pressures depending on the initial structure.
While each individual phase exhibits different phase transformation
histories, all samples commonly experience a sluggish transformation
to a defect cotunnite-like (<i>Pnma</i>) phase for a certain
pressure range. Orthorhombic Dy<sub>2</sub>TiO<sub>5</sub> and Gd<sub>2</sub>TiO<sub>5</sub> form <i>P</i>2<sub>1</sub><i>am</i> at pressures below 9 GPa and <i>Pnma</i> above
13 GPa. Pyrochlore-type Dy<sub>2</sub>TiO<sub>5</sub> and Er<sub>2</sub>TiO<sub>5</sub> as well as defect-fluorite-type Yb<sub>2</sub>TiO<sub>5</sub> form <i>Pnma</i> at ∼21 GPa, followed by <i>Im</i>3<i>̅m</i>. Hexagonal Dy<sub>2</sub>TiO<sub>5</sub> forms <i>Pnma</i> directly, although a small amount
of remnants of hexagonal Dy<sub>2</sub>TiO<sub>5</sub> is observed
even at the highest pressure (∼55 GPa) reached, indicating
kinetic limitations in the hexagonal Dy<sub>2</sub>TiO<sub>5</sub> phase transformations at high pressure. Decompression of these materials
leads to different metastable phases. Most interestingly, a high-pressure
cubic X-type phase (<i>Im</i>3<i>Ì…m</i>)
is confirmed using high-resolution transmission electron microscopy
on recovered pyrochlore-type Er<sub>2</sub>TiO<sub>5</sub>. The kinetic
constraints on this metastable phase yield a mixture of both the X-type
phase and amorphous domains upon pressure release. This is the first
observation of an X-type phase for an A<sub>2</sub>BO<sub>5</sub> composition
at high pressure