State Key Laboratory of Coal Combustion, School of Energy and Power Engineering, Huazhong University of Science and Technology , 430074 Wuhan, China.
Environ Sci Technol. 2017 Jun 6;51(11):6570-6579. doi: 10.1021/acs.est.7b00434. Epub 2017 May 19.
Transformation and evolution mechanisms of nitrogen during algae pyrolysis were investigated in depth with exploration of N-containing products under variant temperature. Results indicated nitrogen in algae is mainly in the form of protein-N (∼90%) with some inorganic-N. At 400-600 °C, protein-N in algae cracked first with algae pyrolysis and formed pyridinic-N, pyrrolic-N, and quaternary-N in char. The content of protein-N decreased significantly, while that of pyrrolic-N and quaternary-N increased gradually with temperature increasing. Pyridinic-N and pyrrolic-N formation was due to deamination or dehydrogenation of amino acids; subsequently, some pyridinic-N converted to quaternary-N. Increasing temperature decreased amides content greatly while increased that of nitriles and N-heterocyclic compounds (pyridines, pyrroles, and indoles) in bio-oil. Amides were formed through NH reacting with fatty acids, that underwent dehydration to form nitriles. Besides, NH and HCN yields increased gradually. NH resulted from ammonia-N, labile amino acids and amides decomposition, while HCN came from nitrile decomposition. At 700-800 °C, evolution trend of N-containing products was similar to that at 400-600 °C. While N-heterocyclic compounds in bio-oil mainly came from pyrifinic-N, pyrrolic-N, and quaternary-N decomposition. Moreover, cracking of pyridinic-N and pyrrolic-N produced HCN and NH. A mechanism of nitrogen transformation during algae pyrolysis is proposed based on amino acids decomposition.
深入研究了藻类热解过程中氮的转化和演变机制,并探讨了不同温度下含氮产物的情况。结果表明,藻类中的氮主要以蛋白质氮(约 90%)和一些无机氮的形式存在。在 400-600°C 时,藻类中的蛋白质氮首先发生裂化,在焦中形成吡啶氮、吡咯氮和季氮。随着温度的升高,蛋白质氮的含量显著下降,而吡咯氮和季氮的含量逐渐增加。吡啶氮和吡咯氮的形成是由于氨基酸的脱氨或脱氢;随后,一些吡啶氮转化为季氮。随着温度的升高,酰胺含量大大降低,而生物油中的腈和含氮杂环化合物(吡啶、吡咯和吲哚)的含量增加。酰胺是通过 NH 与脂肪酸反应形成的,脂肪酸经脱水形成腈。此外,NH 和 HCN 的产率逐渐增加。NH 来自氨氮、不稳定氨基酸和酰胺的分解,而 HCN 来自腈的分解。在 700-800°C 时,含氮产物的演变趋势与 400-600°C 时相似。然而,生物油中的含氮杂环化合物主要来自吡嗪氮、吡咯氮和季氮的分解。此外,吡啶氮和吡咯氮的裂化产生了 HCN 和 NH。根据氨基酸的分解,提出了藻类热解过程中氮转化的机理。