Department of Chemistry, Rice University, MS-222, 6100 Main Street, Houston, Texas 77005, USA.
J Am Chem Soc. 2012 Feb 8;134(5):2815-22. doi: 10.1021/ja211531y. Epub 2012 Jan 27.
Graphite oxide (GO) is a lamellar substance with an ambiguous structure due to material complexity. Recently published GO-related studies employ only one out of several existing models to interpret the experimental data. Because the models are different, this leads to confusion in understanding the nature of the observed phenomena. Lessening the structural ambiguity would lead to further developments in functionalization and use of GO. Here, we show that the structure and properties of GO depend significantly on the quenching and purification procedures, rather than, as is commonly thought, on the type of graphite used or oxidation protocol. We introduce a new purification protocol that produces a product that we refer to as pristine GO (pGO) in contrast to the commonly known material that we will refer to as conventional GO (cGO). We explain the differences between pGO and cGO by transformations caused by reaction with water. We produce ultraviolet-visible spectroscopic, Fourier transform infrared spectroscopic, solid-state nuclear magnetic resonance spectroscopic, thermogravimetric, and scanning electron microscopic analytical evidence for the structure of pGO. This work provides a new explanation for the acidity of GO solutions and allows us to add critical details to existing GO models.
氧化石墨(GO)是一种层状物质,由于材料的复杂性,其结构不明确。最近发表的与 GO 相关的研究仅使用了几种现有模型中的一种来解释实验数据。由于模型不同,这导致对观察到的现象的本质的理解存在混淆。减少结构上的模糊性将促进 GO 的功能化和使用的进一步发展。在这里,我们表明 GO 的结构和性质显著取决于淬火和纯化过程,而不是像通常认为的那样取决于所使用的石墨类型或氧化方案。我们引入了一种新的纯化方案,该方案产生了一种我们称之为原始 GO(pGO)的产物,与通常所知的我们称之为常规 GO(cGO)的材料形成对比。我们通过与水反应引起的转变来解释 pGO 和 cGO 之间的差异。我们通过紫外可见光谱、傅里叶变换红外光谱、固态核磁共振光谱、热重分析和扫描电子显微镜分析为 pGO 的结构提供了证据。这项工作为 GO 溶液的酸度提供了新的解释,并允许我们为现有的 GO 模型添加关键细节。