论文标题

对e $ _g $占用的批评视图作为氧气进化催化活动的描述$ _2 $ o $ $ _4 $纳米颗粒

A criticial view on e$_g$ occupancy as a descriptor for oxygen evolution catalytic activity in LiMn$_2$O$_4$ nanoparticles

论文作者

Schönewald, Florian, Eckhoff, Marco, Baumung, Max, Risch, Marcel, Blöchl, Peter E., Behler, Jörg, Volkert, Cynthia A.

论文摘要

我们研究了limn $ _2 $ o $ _4 $纳米颗粒对电催化氧演化反应(OER)的表面电子结构和组成的影响。扫描透射电子显微镜(Stem)电子能量损失光谱(EEL)研究结合了基于密度功能理论(DFT)的鳗鱼光谱的模拟,在原始纳米颗粒中揭示了4 nm厚的表面层,平均MN氧化态降低,并增加了MN浓度。这归因于Mn $^{2+} $在尖晶石晶格的四面体位点部分替换了li $^+$,并伴随着八面体协调的Mn的Mn 3D-State填充。在电催化OER循环过程中,该近地表四面体MN被浸出,从而增加了八面体配位Mn的氧化态。使用基于旋转的环盘电极(RRDE)检测OER期间O和MN的检测,我们表明氧气的进化保持恒定,而Mn $^{2+} $被删除,表明近距离四面体配位的MN对Limn $ _2 $ o _2 $ o $ $ $ $ _4 $ $ _4 $ _4 $ $ _4 $ $ _4 $ _4 $ _4 $ _4 $ _4 $ _4 $ _4 $。这是令人惊讶的,因为在八面体部位中Mn的E $ _g $占用率(广泛用作OER活动的描述符)在循环过程中的表面层中发生了显着变化。 e $ _g $排空没有与OER活动相关的事实表明,八面体阳离子价不是对活动的基本衡量,因为主动表面状态不受四面体MN的影响,或者因为带结构或金属氧键的其他细节,这一事实更强烈地调节了oer oer的价格限制步骤。

We investigate the effect of the surface electronic structure and composition of LiMn$_2$O$_4$ nanoparticles on the electrocatalytic oxygen evolution reaction (OER). Scanning transmission electron microscopy (STEM) electron energy loss spectroscopy (EELS) studies combined with density functional theory (DFT) based simulations of the EEL spectra reveal in pristine nanoparticles a 4 nm thick surface layer with reduced average Mn oxidation state and increased Mn concentration. This is attributed to Mn$^{2+}$ partially replacing Li$^+$ at the tetrahedral sites of the spinel lattice accompanied by Mn 3d-state filling of octahedrally coordinated Mn. During electrocatalytic OER cycling, this near-surface tetrahedral Mn is leached out, thereby increasing the oxidation state of octahedrally coordinated Mn. Using rotating ring-disc electrode (RRDE) based detection of O and Mn during the OER, we show that the oxygen evolution remains constant while the Mn$^{2+}$ is removed, revealing that near-surface tetrahedrally coordinated Mn has no effect on the OER activity of LiMn$_2$O$_4$. This is surprising since the e$_g$ occupancy of Mn in octahedral sites, which is widely used as a descriptor of OER activity, changes significantly in the surface layer during cycling. The fact that e$_g$ emptying fails to correlate with OER activity here indicates that octahedral cation valence is not a fundamental measure of activity, either because the active surface state is not affected by tetrahedral Mn or because other details of the band structure or metal-oxygen bonding character, more strongly regulate the rate-limiting steps for OER.

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