Cui Zhongxun, Bu Kejun, Zhuang Yukai, Donnelly Mary-Ellen, Zhang Dongzhou, Dalladay-Simpson Philip, Howie Ross T, Zhang Jiandong, Lü Xujie, Hu Qingyang
Center for High Pressure Science and Technology Advanced Research, Shanghai, P.R. China.
Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitor, Ministry of Education, Central South University, Changsha, P.R. China.
Commun Chem. 2021 Sep 2;4(1):125. doi: 10.1038/s42004-021-00565-4.
Earth-abundant antimony trisulfide (SbS), or simply antimonite, is a promising material for capturing natural energies like solar power and heat flux. The layered structure, held up by weak van-der Waals forces, induces anisotropic behaviors in carrier transportation and thermal expansion. Here, we used stress as mechanical stimuli to destabilize the layered structure and observed the structural phase transition to a three-dimensional (3D) structure. We combined in situ x-ray diffraction (XRD), Raman spectroscopy, ultraviolet-visible spectroscopy, and first-principles calculations to study the evolution of structure and bandgap width up to 20.1 GPa. The optical band gap energy of SbS followed a two-step hierarchical sequence at approximately 4 and 11 GPa. We also revealed that the first step of change is mainly caused by the redistribution of band states near the conduction band maximum. The second transition is controlled by an isostructural phase transition, with collapsed layers and the formation of a higher coordinated bulky structure. The band gap reduced from 1.73 eV at ambient to 0.68 eV at 15 GPa, making it a promising thermoelectric material under high pressure.
地球上储量丰富的三硫化锑(SbS),即锑矿,是一种用于捕获太阳能和热通量等自然能量的有前景的材料。由弱范德华力支撑的层状结构在载流子输运和热膨胀中引发各向异性行为。在此,我们将应力用作机械刺激来破坏层状结构,并观察到向三维(3D)结构的结构相变。我们结合原位X射线衍射(XRD)、拉曼光谱、紫外可见光谱和第一性原理计算,研究了高达20.1吉帕斯卡压力下结构和带隙宽度的演变。SbS的光学带隙能量在约4吉帕斯卡和11吉帕斯卡时遵循两步分级序列。我们还揭示,第一步变化主要由导带最大值附近能带态的重新分布引起。第二次转变由同结构相变控制,伴随着层的坍塌和形成更高配位的块状结构。带隙从常压下的1.73电子伏特降至15吉帕斯卡时的0.68电子伏特,使其成为高压下一种有前景的热电材料。