首页> 外文期刊>Sonklanakarin Journal of Science and Technology >Combustion of microalgae Nannochloropsis oculata biomass: Cellular macromolecular and mineralogical content changes during thermal decomposition
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Combustion of microalgae Nannochloropsis oculata biomass: Cellular macromolecular and mineralogical content changes during thermal decomposition

机译:微藻Nannochloropsis oculata生物质的燃烧:热分解过程中细胞大分子和矿物含量的变化

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The cellular macromolecular and mineralogical content changes during the combustion of Nannochloropsis oculatabiomass have been investigated. A Fourier transform infrared spectroscopy (FTIR) analyzer was used to investigate the cellularmacromolecular content changes of biomass at every stage of decomposition during heating to 1200 ?C. From ambient temperaturesto 190 ?C, similar spectra were obtained, indicating relatively little change in the chemical structure of the biomassmaterial. Changes in the spectra are very noticeable from 190 to 1200 ?C. The combustion process begins with thermal crackingof the ?OH groups of silanol that escape together with moisture at temperatures up to 190 ?C. Subsequent temperature increasedecreased intensity of the spectrum, indicating thermal degradation of the organic compounds derived from lipids, proteins, andcarbohydrates. These processes occur up to 800 ?C. The X-ray diffraction (XRD) results showed that the mineral constituents ofbiomass degraded during the combustion process, and a portion reacted to form new compounds such as melilite (Ca6Na2O15Si4).The SEM images show a morphological distinction between biomass and its residue at 1200 ?C, due to the decomposition andrearrangement of the mineral content during heating. Fragmentation of the samples also occurred during heating, characterizedby more uniform residue at 1200 ?C.
机译:研究了拟南芥眼球生物量燃烧过程中细胞大分子和矿物学含量的变化。使用傅里叶变换红外光谱(FTIR)分析仪研究加热到1200°C期间分解的每个阶段中生物量的细胞大分子含量变化。从环境温度到190°C,获得了相似的光谱,表明生物质材料的化学结构变化相对较小。从190到1200°C,光谱变化非常明显。燃烧过程从热裂解硅烷醇的OH基团开始,这些硅烷醇与水分一起在高达190°C的温度下逸出。随后温度升高,光谱强度增加,表明衍生自脂质,蛋白质和碳水化合物的有机化合物发生热降解。这些过程会在最高800°C的温度下发生。 X射线衍射(XRD)结果表明,生物质的矿物质成分在燃烧过程中降解,一部分反应形成了新化合物,如melilite(Ca6Na2O15Si4).SEM图像显示了1200℃时生物质及其残留物的形态学区别由于加热过程中矿物质含量的分解和重新排列,导致温度升高。加热过程中也会发生样品碎裂,其特征是在1200°C下残留更均匀。

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