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原位同步辐射散射研究钙钛矿薄膜从溶液到晶相的形成机制和控制。

Formation Mechanism and Control of Perovskite Films from Solution to Crystalline Phase Studied by in Situ Synchrotron Scattering.

机构信息

Department of Materials Science and Engineering, National Taiwan University , Taipei 10617, Taiwan.

Institute of Nuclear Energy Research , Taoyuan 32546, Taiwan.

出版信息

ACS Appl Mater Interfaces. 2016 Oct 12;8(40):26712-26721. doi: 10.1021/acsami.6b07468. Epub 2016 Sep 28.

Abstract

Controlling the crystallization and morphology of perovskite films is crucial for the fabrication of high-efficiency perovskite solar cells. For the first time, we investigate the formation mechanism of the drop-cast perovskite film from its precursor solution, PbCl and CHNHI in N,N-dimethylformamide, to a crystalline CHNHPbICl film at different substrate temperatures from 70 to 180 °C in ambient air and humidity. We employed an in situ grazing-incidence wide-angle X-ray scattering (GIWAXS) technique for this study. When the substrate temperature is at or below 100 °C, the perovskite film is formed in three stages: the initial solution stage, transition-to-solid film stage, and transformation stage from intermediates into a crystalline perovskite film. In each stage, the multiple routes for phase transformations are preceded concurrently. However, when the substrate temperature is increased from 100 to 180 °C, the formation mechanism of the perovskite film is changed from the "multistage formation mechanism" to the "direct formation mechanism". The proposed mechanism has been applied to understand the formation of a perovskite film containing an additive. The result of this study provides a fundamental understanding of the functions of the solvent and additive in the solution and transition states to the crystalline film. It provides useful knowledge to design and fabricate crystalline perovskite films for high-efficiency solar cells.

摘要

控制钙钛矿薄膜的结晶和形态对于制备高效钙钛矿太阳能电池至关重要。我们首次研究了从其前驱体溶液 PbCl 和 CHNHI 在 N,N-二甲基甲酰胺中到在环境空气和湿度下不同基底温度(70 至 180°C)的结晶 CHNHPbICl 薄膜的形成机制。我们为此研究采用了原位掠入射广角 X 射线散射(GIWAXS)技术。当基底温度为 100°C 或以下时,钙钛矿薄膜的形成经历三个阶段:初始溶液阶段、向固态薄膜转变阶段以及中间产物向结晶钙钛矿薄膜转变阶段。在每个阶段,多个相转变途径同时进行。然而,当基底温度从 100°C 升高到 180°C 时,钙钛矿薄膜的形成机制从“多阶段形成机制”转变为“直接形成机制”。所提出的机制已被应用于理解含添加剂的钙钛矿薄膜的形成。这项研究的结果提供了对溶剂和添加剂在溶液和过渡态到结晶薄膜中的作用的基本理解。它为设计和制备高效太阳能电池的结晶钙钛矿薄膜提供了有用的知识。

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