Thin film Iron Pyrite synthesized by sulfurization of Iron Oxide for application in photovoltaics

Pravakar P. Rajbhandari, T. Dhakal, C. Westgate
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Abstract

Iron Pyrite (FeS2) is considered as a promising candidate for photovoltaic application because of its suitable band-gap, very high light absorption coefficient and the abundance of the component elements in the earth's crust. The problem however is that Iron Sulfide has several coexisting phases. Even with the same stoichiometry, it may have two different phases such as pyrite and marcasite. In this report, a phase pure iron pyrite is fabricated on a plain glass and molybdenum coated glass in an atmospheric pressure chemical vapor deposition system (APCVD) by annealing sputtered iron oxide (Fe2O3) in sulfur environment (elemental sulfur) at temperatures higher than 350°C. X-ray Diffraction measurement showed only pyrite phase and energy dispersive spectroscopy (EDS) showed 1:2 ratio for iron to sulfur. Depth profile using X-ray Photoelectron Spectroscopy showed a full conversion of iron oxide into pyrite. Increasing the temperature beyond 350°C, grain size got bigger, but pyrrhotite phase with very low resistivity started to appear.
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氧化铁硫化法制备薄膜硫铁矿在光伏中的应用
铁黄铁矿(FeS2)因其具有合适的带隙、很高的光吸收系数和地壳中丰富的组成元素而被认为是光伏应用的有前途的候选者。然而,问题是硫化铁有几个共存的相。即使在相同的化学计量下,它也可能有两种不同的相,如黄铁矿和黄铁矿。在常压化学气相沉积系统(APCVD)中,将溅射氧化铁(Fe2O3)在高于350℃的硫环境(单质硫)中退火,制备出相纯的黄铁矿。x射线衍射测定显示为黄铁矿相,能谱分析显示铁与硫的比例为1:2。x射线光电子能谱深度剖面显示氧化铁完全转化为黄铁矿。当温度超过350℃时,晶粒尺寸变大,但开始出现电阻率极低的磁黄铁矿相。
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