Comparative observation of the flow behavior of low- and high-temperature ashes of biomass

被引:3
|
作者
Li, Jiazhu [1 ]
Wei, Juntao [2 ]
Reinmoeller, Markus [3 ,4 ]
Liang, Chen [1 ]
Li, Shuangshuang [1 ]
Xiao, Ruirui [5 ]
Xu, Jie [1 ]
机构
[1] Qingdao Agr Univ, Lab React & Separat Technol, 700 Changcheng Rd, Qingdao 266109, Peoples R China
[2] Nanjing Forestry Univ, Coll Mat Sci & Engn, Coinnovat Ctr Efficient Proc & Utilizat Forest Re, Joint Int Res Lab Biomass Energy & Mat, Nanjing 210037, Peoples R China
[3] Tech Univ Denmark, DTU Engn Technol, Lautrupvang 15, DK-2750 Ballerup, Denmark
[4] TU Bergakad Freiberg, Inst Energy Proc Engn & Chem Engn, Fuchsmuehlenweg 9 Reiche Zeche, D-09599 Freiberg, Germany
[5] Zaozhuang Univ, Key Lab Coal Chem Ind Shandong Prov, 1 Beian Rd, Zaozhuang 277160, Peoples R China
基金
中国国家自然科学基金;
关键词
Biomass; Mineral phase transformation; Ashing temperatures; Ash fusion test; Heating-stage microscope; Thermochemical calculations; SLAGGING CHARACTERISTICS; FUSION CHARACTERISTICS; CHEMICAL-COMPOSITION; COMBUSTION SYSTEMS; MELTING BEHAVIOR; CO-GASIFICATION; TRANSFORMATION; PHOSPHORUS; BLENDS; FUELS;
D O I
10.1016/j.fuel.2022.125232
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Biomass ashes are frequently known for their limiting effects in thermochemical conversion processes. Thus, a comprehensive understanding and prediction of the temperature-depending behavior of the ashes is indispensable for practical applications. In the present study, the flow behavior of low-temperature ash (LTA) and high-temperature ash (HTA) of biomass is investigated in detail and monitored by in situ methods. For this purpose, the mineral matter formation and transformation of both ashes are studied by X-ray diffraction (XRD) and X-ray fluorescence (XRF) analysis. A combination of heating-stage microscope and scanning electron microscope equipped with energy-dispersive X-ray spectroscopy (SEM-EDX) has enabled a systematic identification of the microstructures and observations of LTA and HTA. The results have illustrated an associated release of K and Cl and the formation of new mineral phases in the remaining material during ashing at increased temperature. Both ashes have exhibited flow temperatures below 1100 degrees C and a rarely observed behavior of higher characteristic temperatures for LTA than for HTA is detected. From the heating-stage microscopy, the ashes have given evidence to a significant formation of slag at the characteristic temperatures and a viscosity-driven behavior at the characteristic points of ash fusion. Based on these results, a conclusion can be drawn regarding the usability of this biomass for high-temperature conversion processes on the industrial scale.
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页数:9
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