Facile synthesis and optimization of graphene oxide reduction by annealing in hydrazine vapour in ambient air for potential application in perovskite solar cells

S. Ochigbo, Alfred Obukohwo Obar, M.A.T. Suleiman, A.S. Kovo
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Abstract

Graphene oxide (GO) was synthesized from graphite via a modified Hummer's method, followed by thermal and chemical reductions to produce reduced graphene oxide (RGO) samples at various temperatures. A suite of characterization techniques including Fourier Transform Infrared Spectroscopy (FTIR), Scanning Electron Microscopy (SEM), Energy-Dispersive X-ray Spectroscopy (EDS), UV-Visible Spectroscopy, thermogravimetric analysis (TGA), X-ray diffraction (XRD), and Hall effect measurements were employed to assess the structural, morphological, optical, and electrical properties of the samples. FTIR analysis confirmed the successful functionalization of graphite to GO and subsequent reduction to reduced graphene oxide, with peak intensities decreasing as the reduction temperature increased. UV-visible spectroscopy of GO showed a maximum absorption at 235 nm which confirmed the synthesis of GO while the reduction revealed a notable red shift in absorption peaks with increasing annealing temperature, and that signified a reduction in bandgap. XRD analyses demonstrated the removal of oxygen functional groups. The X-ray diffraction (XRD) analysis of GO showed diffraction at 2θ = 10.74° which revealed a fully oxidized graphene oxide with oxygen-containing functional groups, and hence an increase in interlayer spacing (d002) from 3.341 Å (graphite) to 8.228 Å (GO). Upon reduction, there is a gradual decrease in d002 from 8.228 Å (GO) to 3.387 Å (HRGO300), suggesting the gradual removal of intercalated oxygen molecules, and hence the gradual restoration of sp2 hybridisation in graphene. The EDS analysis revealed an increase in the carbon-to-oxygen (C/O) ratio from 1.78 in GO to 2.75 in HRGO300 as the annealing temperature for the reduction process increased which further confirmed the removal of oxygen functional groups. The Hall effect data showed hole mobility of 4.634 x101 (GO), 4.831 x101 (HRGO200), and 5.462 x100 (HRGO300) with conductivities of 8.985 x10-5 (GO), 1.087 x100 (HRGO200) and 1.791 x101 1/Ω cm, suggesting an increase in conductivity as the annealing temperature increased as revealed in the EDS. Out of the three samples identified as hole transport materials, the sample HRGO300 with the highest C/O ratio of 2.75 has the highest conductivity, and hence most suitable for application as hole transport material in perovskite solar cell.
在环境空气中通过肼蒸气退火还原氧化石墨烯的简便合成和优化,使其在过氧化物太阳能电池中得到潜在应用
通过改进的汉默法从石墨中合成了氧化石墨烯 (GO),然后在不同温度下通过热还原和化学还原生成了还原型氧化石墨烯 (RGO) 样品。为评估样品的结构、形态、光学和电学特性,采用了一系列表征技术,包括傅立叶变换红外光谱(FTIR)、扫描电子显微镜(SEM)、能量色散 X 射线光谱(EDS)、紫外可见光谱、热重分析(TGA)、X 射线衍射(XRD)和霍尔效应测量。傅立叶变换红外光谱分析证实,石墨成功官能化为 GO,随后还原为还原型氧化石墨烯,峰强度随着还原温度的升高而降低。GO 的紫外可见光谱显示,在 235 纳米处有最大吸收,这证实了 GO 的合成,而还原显示,随着退火温度的升高,吸收峰有明显的红移,这表明带隙减小了。XRD 分析表明氧官能团已被去除。GO 的 X 射线衍射 (XRD) 分析显示,在 2θ = 10.74° 处有衍射,这表明氧化石墨烯完全氧化,含有氧官能团,因此层间距 (d002) 从 3.341 Å(石墨)增加到 8.228 Å(GO)。在还原过程中,d002 从 8.228 Å(GO)逐渐减小到 3.387 Å(HRGO300),这表明插层氧分子逐渐去除,从而逐渐恢复了石墨烯中的 sp2 杂化。EDS 分析表明,随着还原过程退火温度的升高,碳氧(C/O)比从 GO 的 1.78 增加到 HRGO300 的 2.75,这进一步证实了氧官能团的去除。霍尔效应数据显示,空穴迁移率分别为 4.634 x101(GO)、4.831 x101(HRGO200)和 5.462 x100(HRGO300),电导率分别为 8.985 x10-5(GO)、1.087 x100(HRGO200)和 1.791 x101 1/Ω 厘米,这表明随着退火温度的升高,电导率也随之升高,正如 EDS 所显示的那样。在被确定为空穴传输材料的三种样品中,C/O 比最高为 2.75 的样品 HRGO300 的电导率最高,因此最适合用作过氧化物太阳能电池中的空穴传输材料。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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