用于高效太阳能水分解的赤铁矿纳米结构

J. Deng, A. Pu, M. Li, J. Gao, H. Zhang, J. Zhong, X. Sun
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引用次数: 5

摘要

赤铁矿具有良好的光学带隙(2.1 ~ 2.2 eV)、氧化环境中优异的化学稳定性、丰富度和低廉的成本,是一种高效的太阳能水分解光催化剂。根据理论预测,赤铁矿的太阳能制氢效率可达16.8%,水分解光电流可达12.6 mA cm-2。然而,赤铁矿在太阳能分解水中的实际性能远未达到理想状态,这主要受到电导率差、激发态载流子寿命短(10-12s)、析氧反应动力学差、空穴扩散长度短(2-4nm)以及非辅助分解水中能带位置不合适等因素的限制。近年来,我们对赤铁矿纳米结构光电极的性能进行了大量的研究。通过控制赤铁矿的形貌、元素掺杂和改善赤铁矿的电荷输运等方法,提高了赤铁矿光电极在太阳能水分解中的性能。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hematite nanostructures for high efficient solar water splitting
Hematite has emerged as a good photocatalyst for efficient solar water splitting due to its favorable optical band gap (2.1-2.2 eV), extraordinary chemical stability in oxidative environment, abundance, and low cost. According to theoretical prediction, the solar-to-hydrogen efficiency of hematite can be 16.8% and the water splitting photocurrent can be 12.6 mA cm-2. However, the practical performance of hematite for solar water splitting is far from the ideal case which has been limited by several factors such as poor conductivity, short lifetime of the excited-state carrier (10-12s), poor oxygen evolution reaction (OER) kinetics, short hole diffusion length (2-4nm), and improper band position for unassisted water splitting. In our recent work, enormous efforts have been focused on improving the performance of hematite nanostructure photoelectrode. Different methods such as morphology control, elemental doping, and improvement of the charge transport of hematite have been developed to improve the performance of hematite photoelectrode in solar water splitting.
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