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Organohalide Perovskites are Fast Ionic Conductors

机译:有机卤化物钙钛矿是快速离子导体

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Fast ionic conductors constitute a family of materials exhibiting high values of the ionic conductivity while their crystal structure remains rather rigid. Perovskite-like compounds are known to be good ionic conductors with applications as solid electrolytes. In hybrid halide perovskites both intrinsic (native) and extrinsic defect migration are regarded to occur. Ion diffusivity analysis is inherently ambiguous in all-solid-state configurations because of the multicomponent environment. Here, a liquid electrolyte in contact to the perovskite material forms a reservoir of Li+ that is forced to intercalate and migrate within the perovskite electrode. This approach decouples different contributions to transport in such a way that ion diffusion kinetics is easily accessible by means of impedance methods. The room-temperature chemical diffusion coefficient of lithium ion within the perovskite lattice exhibits values as high as D-mu approximate to 10(-7) cm(2) s(-1), which implies conductivities within the range of 10(-3) Omega(-1) cm(-1) for highly lithiated electrodes. This confirms the superionic intrinsic property of organohalide perovskites from a direct and unambiguous measurement that does not rely upon simulation tools.
机译:快速离子导体构成一族材料,这些材料表现出很高的离子电导率,而它们的晶体结构仍然相当坚硬。已知钙钛矿状化合物是良好的离子导体,可作为固体电解质使用。在杂化卤化物钙钛矿中,固有的(天然)缺陷和外部的缺陷迁移都被认为发生了。由于存在多组分环境,因此离子扩散率分析在全固态配置中固有地模棱两可。在此,与钙钛矿材料接触的液体电解质形成Li +的储层,被迫在钙钛矿电极内插入和迁移。该方法以通过阻抗方法容易获得离子扩散动力学的方式解耦了对运输的不同贡献。钙钛矿晶格中锂离子的室温化学扩散系数显示出高达D-mu的值,近似于10(-7)cm(2)s(-1),这意味着电导率在10(-3)范围内)高度锂化的电极的Omega(-1)cm(-1)。通过不依赖模拟工具的直接且明确的测量结果,可以确认有机卤化物钙钛矿的超离子固有特性。

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