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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Nitrogen functionality in 'oil window' rank range vitrinite rich coals and chars
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Nitrogen functionality in 'oil window' rank range vitrinite rich coals and chars

机译:“油窗”中的氮功能等级范围为富含镜质石的煤和焦

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摘要

X-ray photoelectron spectroscopy (XPS) was used to characterize organic nitrogen species in coals and chars. The coals comprise a set of vitrinite-rich samples from the Penn State Coal Bank set, ranging from vitrinite reflectance (R_r) 0.42-1.60%. Chars were obtained after coal pyrolysis under an inert atmosphere at 800 °C and fast heating rate. In the coals, pyrrolic nitrogen was the predominant form, steadily decreasing with coal rank, while pyridinic and quaternary nitrogen showed pronounced variation with rank. In contrast to the coals, the chars show much less pyrrolic and pyridinic nitrogen, and more quaternary nitrogen. The chars were also characterized by having oxidized nitrogen and nitro sub-peaks, which were not observed for the coals. Apparently the occurrence of these forms is related to the decrease in the pyridinic nitrogen.
机译:X射线光电子能谱(XPS)用于表征煤和焦炭中的有机氮物种。这些煤包含一组来自宾州州立煤炭银行的富含镜质石样品,其镜质体反射率(R_r)为0.42-1.60%。煤在惰性气氛,800°C和快速加热速率下热解后得到焦炭。煤中以吡咯型氮为主要形式,随煤级的升高而稳定降低,而吡啶二元和季氮型的氮含量随煤级的升高而显着变化。与煤相比,炭显示出更少的吡咯和吡啶氮,更多的是季氮。炭的特征还在于具有氧化的氮和硝基亚峰,煤中未观察到。显然,这些形式的出现与吡啶氮的减少有关。

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