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含磷基团在活性炭热处理过程中的演变。

Evolution of Phosphorus-Containing Groups on Activated Carbons during Heat Treatment.

机构信息

College of Chemical Engineering, Jiangsu Key Laboratory of Biomass-Based Green Fuels and Chemicals, Nanjing Forestry University , Nanjing 210037, China.

College of Materials Science and Engineering, Hunan University , Changsha 410082, China.

出版信息

Langmuir. 2017 Mar 28;33(12):3112-3122. doi: 10.1021/acs.langmuir.7b00095. Epub 2017 Mar 17.

Abstract

Two types of activated carbons have been prepared by HPO activation of lignocellulose and by HPO modification of activated carbon, and then heat-treated at temperatures from 400 to 900 °C in an atmosphere of N or H to investigate the evolution of phosphorus-containing groups. Elemental analysis, X-ray photoelectron spectroscopy, P nuclear magnetic resonance, nitrogen adsorption, and scanning electron microscopy have been used to analyze the physicochemical properties of the activated carbons. The results show that C-O-P linkages of phosphorus-containing groups can progressively evolve into C-P-O, C-P═O, C-P, and eventually elemental phosphorus as a result of heat treatment. Phosphate-like groups are much more thermally stable in an N than in an H atmosphere. In N, C-O-P linkages significantly evolve into C-P-O and C-P═O at up to 800 °C, whereas C-P linkages are not formed even at 900 °C. In H, the corresponding evolution remarkably occurs at 500 °C, forming C-P linkages and eventually elemental phosphorus. Moreover, the two activated carbons exhibit different evolution trends, suggesting that the evolution happens more easily for phosphorus-containing groups located on the edges of graphite-like crystallites than those in the lattice. Finally, we propose different evolution pathways of phosphorus-containing groups upon heat treatment in N and H atmospheres.

摘要

两种类型的活性炭通过木质纤维素的 HPO 活化和活性炭的 HPO 改性制备得到,然后在 N 或 H 气氛中在 400 至 900°C 的温度下进行热处理,以研究含磷基团的演变。元素分析、X 射线光电子能谱、磷核磁共振、氮气吸附和扫描电子显微镜用于分析活性炭的物理化学性质。结果表明,含磷基团的 C-O-P 键由于热处理可以逐步演变为 C-P-O、C-P═O、C-P,最终形成元素磷。在 N 气氛中,磷酸盐类基团比在 H 气氛中热稳定性更高。在 N 中,C-O-P 键在高达 800°C 时显著演变为 C-P-O 和 C-P═O,而在 900°C 时甚至没有形成 C-P 键。在 H 中,相应的演变在 500°C 时明显发生,形成 C-P 键并最终形成元素磷。此外,这两种活性炭表现出不同的演变趋势,这表明对于位于类石墨微晶边缘的含磷基团,其演变比晶格中的含磷基团更容易发生。最后,我们提出了在 N 和 H 气氛中热处理时含磷基团的不同演变途径。

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