同步辐射软X射线吸收谱与发射谱测定天然针铁矿能带结构
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  • 英文篇名:Electronic structure of natural goethite probed by soft X-ray emission and absorption spectroscopy
  • 作者:丁聪 ; 李艳 ; 李岩 ; 鲁安怀
  • 英文作者:DING Cong;LI Yan;LI Yan;LU An-huai;Key Laboratory of Orogenic Belts and Crustal Evolution, MOE, School of Earth and Space Sciences, Peking University;
  • 关键词:半导体矿物 ; 针铁矿 ; 同步辐射 ; 吸收谱 ; 发射谱 ; 光催化
  • 英文关键词:semiconductor mineral;;goethite;;synchrotron;;adsorption and emission spectroscopy;;photocatalysis
  • 中文刊名:YSKW
  • 英文刊名:Acta Petrologica Et Mineralogica
  • 机构:造山带与地壳演化教育部重点实验室北京大学地球与空间科学学院;
  • 出版日期:2016-03-25
  • 出版单位:岩石矿物学杂志
  • 年:2016
  • 期:v.35;No.160
  • 基金:国家重点基础研究发展计划(2014CB846001);; 国家自然科学基金重点项目(41230103);国家自然科学基金项目(41272003,41522201)~~
  • 语种:中文;
  • 页:YSKW201602015
  • 页数:6
  • CN:02
  • ISSN:11-1966/P
  • 分类号:175-180
摘要
天然半导体矿物由于成分、缺陷复杂,传统测试方法如紫外可见漫反射等难以准确测定其禁带宽度.本文以针铁矿为例,通过第一性原理计算得到纯针铁矿及掺Al针铁矿的电子结构.计算结果显示,纯针铁矿导带底与价带顶均由Fe3d与O2p轨道组成,而当含杂质Al时,Al2p与O2p发生杂化参与了价带组成.在此基础上,利用同步辐射X射线氧的K边吸收谱与发射谱对纯针铁矿及天然针铁矿的能带结构进行了测定.结果表明,天然含Al的针铁矿禁带宽度为2.30eV,小于纯针铁矿(2.57eV).本研究提供了一种测定天然氧化物矿物禁带宽度的新方法,为深入研究天然半导体可见光催化活性产生机制提供了理论依据.
        In this study, the authors investigated the electronic structures of natural goethite FeOOH by first principle theory and synchrotron soft X-ray emission and absorption spectroscopy. The results show that the band gap of natural goethite FeOOH is 2. 30 eV, smaller than the band gap of pure goethite FeOOH( 2. 57 eV). Due to the complex compositions and plenty of defects, the band structure of natural minerals is hard to measure by traditional methods, such as UV-Vis. The results supply a new way for determining the band structure of natural semiconductor minerals and also provide a basis for better understanding of photocatalytic mechanism of them under visible light.
引文
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