14 research outputs found
Complex Alloy and Heterostructure Nanoparticles Derived from Perovskite Oxide Precursors for Catalytic Dry Methane Reforming
We have developed a general route for combining Ni, Fe,
Co, Cu,
and Pd in a nanoparticle using the exsolution mechanism from LaFe0.7Ni0.1Co0.1Cu0.05Pd0.05O3 perovskite oxide precursors. The strong adherence
of the nanoparticles to the support yields attractive catalytic properties
for dry methane reforming, such as coke resistance and thermal sintering
suppression. The reduction of the precursors at 700 and 900 °C
yielded NiCoCuPd or NiFeCoCuPd nanoparticles with a size-dependent
phase transition from a complex concentrated alloy to phase-separated
heterostructures. Our findings indicate that smaller concentrated
alloy nanoparticles (∼10 nm) are more effective for methane
activation than larger (>20 nm) phase-separated nanoparticles
Pt<sub>3</sub>Co/Co Composite Catalysts on Porous N‑Doped Carbon Support Derived from ZIF-67 with Enhanced HER and ORR Activities
The primary challenge for efficient H2 evolution
and
hydrogen energy conversion is to develop highly active and stable
catalysts with simple and reliable preparation processes. In this
regard, we have designed and synthesized a porous carbon-supported
low-Pt alloy catalyst (Pt3Co/Co@C composite) using ZIF-67
as a template. It showed uniformly dispersed Pt3Co/Co on
the porous carbon layer due to the confinement effect of the porous
carbon layer. Pt3Co/Co@C demonstrated excellent activity
for the hydrogen evolution reaction in the full pH range, with an
overpotential of 187 mV in 0.5 M H2SO4 to attain
100 mA/cm2 as well as long-term stability. It also displayed
superior mass activity for the oxygen reduction reaction (ORR) at
0.85 V (vs RHE) compared to the commercial Pt/C. Furthermore, the
Pt3Co/Co@C catalyst exclusively enabled a four-electron
reaction process under ORR conditions without the competitive pathway
to H2O2. The current work provides guidance
for the design and facile synthesis of Pt-based catalysts with enhanced
performance
Dynamical Observation and Detailed Description of Catalysts under Strong Metal–Support Interaction
Understanding
the structures of catalysts under realistic conditions with atomic
precision is crucial to design better materials for challenging transformations.
Under reducing conditions, certain reducible supports migrate onto
supported metallic particles and create strong metal–support
states that drastically change the reactivity of the systems. The
details of this process are still unclear and preclude its thorough
exploitation. Here, we report an atomic description of a palladium/titania
(Pd/TiO<sub>2</sub>) system by combining state-of-the-art in situ
transmission electron microscopy and density functional theory (DFT)
calculations with structurally defined materials, in which we visualize
the formation of the overlayers at the atomic scale under atmospheric
pressure and high temperature. We show that an amorphous reduced titania
layer is formed at low temperatures, and that crystallization of the
layer into either mono- or bilayer structures is dictated by the reaction
environment and predicted by theory. Furthermore, it occurs in combination
with a dramatic reshaping of the metallic surface facets
Cumulative ET for each year of 2003–2010 respectively (panel a); cumulative ET averaged over the observation periods and its standard deviation (black line) and monthly variations in standard deviation (red line and the axis on right) (panel b).
<p>Cumulative ET for each year of 2003–2010 respectively (panel a); cumulative ET averaged over the observation periods and its standard deviation (black line) and monthly variations in standard deviation (red line and the axis on right) (panel b).</p
Coefficient of variation (CV) of ET at flux sites with over 3 years' observations.
<p>Coefficient of variation (CV) of ET at flux sites with over 3 years' observations.</p
Cumulative precipitation versus average air temperature of the whole year and the growing season (April–October) during the period 1989–2010.
<p>For the period of 2003–2010, the size of black dot is approximately proportional to the ET amount. The two-digit numbers (YY) denote the years from 2003 to 2010 (20YY). Dotted lines represent the averages over the 20 year period.</p
Yearly values of cumulative ET calculated through different approaches: V<sub>cli-eco</sub> (for variable climate and variable ecosystem responses); V<sub>cli</sub> (for variable climate); V<sub>eco</sub> (for variable ecosystem responses).
<p>The correlation coefficients of the cumulative values calculated with the three approaches are also reported.</p
Annual accumulated ET, R<sub>n</sub>, P and annual averaged T<sub>a</sub> during 2003–2010.
<p>Annual accumulated ET, R<sub>n</sub>, P and annual averaged T<sub>a</sub> during 2003–2010.</p
Air temperature (T<sub>a</sub> °C) and growing season length (GSL, in days T<sub>a</sub>≥5°C) during 2003–2010.
<p>Air temperature (T<sub>a</sub> °C) and growing season length (GSL, in days T<sub>a</sub>≥5°C) during 2003–2010.</p
Correlation coefficients (R) between ET and some of the climatic drivers (R<sub>n</sub>, T<sub>a</sub> and VPD) at monthly and annual scale (p represents the probability-value).
<p>Correlation coefficients (R) between ET and some of the climatic drivers (R<sub>n</sub>, T<sub>a</sub> and VPD) at monthly and annual scale (p represents the probability-value).</p