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Nonempirical modeling of hydrated single-layer graphene oxide (GO) fragments revealed that at least one, but substantial origin of the acidity of aqueous GO solutions is the dissociation in closely grouped and favorably H-bonded hydroxyls. The process can further be promoted by the adjacent -conjugated carbon segments at the edges of GO flakes or their inner defects. The apparent values of the groups fall in a range of ca. 2.0 to 5.3. Under certain conditions the ionization may become spontaneous.

生成讲解博客的中文版本

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