Fe–N–C materials exhibit excellent activity and stability for oxygen reduction reaction (ORR), as one of the most promising candidates to replace commercial Pt/C catalysts. However, it is challenging to unravel features of the superior ORR activity originating from Fe–N–C materials. In this work, the electronic and geometric structures of the isolated Fe–N–C sites and their correlations with the ORR performance are investigated by varying the secondary thermal activation temperature of a rationally designed NC‐supported Fe single‐atom catalyst (SAC). The systematic analyses demonstrate the significant role of coordinated atoms of SA and metallic Fe nanoparticles (NPs) in altering the electronic structure of isolated Fe–N–C sites. Meanwhile, strong interaction between isolated Fe–N–C sites and adjacent Fe NPs can change the geometric structure of isolated Fe–N–C sites. Theoretical calculations reveal that optimal regulation of the electronic and geometric structure of isolated Fe–N–C sites by the co‐existence of Fe NPs narrows the energy barriers of the rate‐limiting steps of ORR, resulting in outstanding ORR performance. This work not only provides the fundamental understanding of the underlying structure–activity relationship, but also sheds light on designing efficient Fe–N–C catalysts.
This study focuses on the chemical composition, and the factors controlling it, of the high mountain-rivers in the source region of the Yangtze River on the Tibetan Plateau. By comprehensive and systematic analysis, the chemical signatures, spatial variations of water quality, as well as the factors controlling them are studied. The value of the average total dissolved solids (TDS) is 778 mg/l, ranging from 117 to 5496 mg/l. In order of decreasing concentration, the main cations are Na try of the river water is controlled by lithogenic weathering processes. The Na-normalized ratio end-member diagram indicates that the weathering of silicates and carbonates is relatively significant, on the whole. There exists pronounced regional heterogeneity in the water chemistry and the factors affecting it. The northern rivers, including Chumaer He, Beilu He, and Ranchiqu, are mainly affected by evaporation and crystallization processes, while the southern rivers (Tuotuo He, Gaerqu, and Buqu) show effects from the weathering of carbonates and silicates.
As
a two-dimensional direct band gap semiconductor with unique
electronic and magnetic properties, monolayer chromium triiodide (CrI3) has
a great potential for spintronic applications. Under the guidance
of the defect theory, we adopt first-principles calculation to determine
the structural, thermodynamic, electronic, and magnetic properties
of point defects of monolayer CrI3. Twenty kinds of point
defects, including vacancies, interstitial, substitution, and bond-rotation
defects have been investigated. Either the metalloid or metallic single
atom vacancies is energetically stable depends on the chemical potential
of iodide, leading to the intrinsic n-type and p-type dopings, respectively.
More interestingly, a ferromagnetic to antiferromagnetic transition
of the magnetic phase can be induced for most type of point defects,
which can be explained by a simple Heisenberg model. The content of
present investigation contributes to the atomic-scale understanding
of the electric and magnetic properties of monolayer CrI3.
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