首页|生物质热解过程中焦炭物化结构演变特性

生物质热解过程中焦炭物化结构演变特性

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利用比表面积孔径分析仪测定生物质热解焦炭的氮气等温吸附曲线并得到结构和孔径分布特性,同时对焦炭的形貌和微区化学组成进行深入分析.研究表明:随着热解终温的升高,生物质焦炭的孔隙结构变得复杂,600℃时焦炭的孔隙结构、比表面积和吸附特性较好,1000℃时出现孔坍塌和融合现象,稻壳焦炭微区元素主要是C、O、Si和K,并在800℃时表面存在硅化物和碳化物两种不同的结构.
EVOLUTION OF CHAR'S PHYSICAL AND CHEMICAL STRUCTURE DURING BIOMASS PYROLYSIS
The internal porosity characteristic of the pyrolysis char is one of the important parameters of the thermal decomposition mechanism and char properties. The different final pyrolysis temperatures of char for straw, rice husk and sawdust were used in a fixed bed reactor, with nitrogen atmosphere. The specific surface area of pore size analyzer was used to measure the nitrogen adsorption isotherm of char and the characteristics of pore structure and pore size distributions were obtained. The char pore morphology and micro chemical composition were analyzed in detail. The results show that the pore sturcture of biochar changes complex with the final pyrolysis temperature increasing, the char pore structure, specific surface area and absorption characteristics are fine at 600℃ ; the hole collapses and hybridization appear at l000℃ , micro elements are mainly C, 0, Si and K; There are charcoals and silicide two different structures on the surface of rice husk pyrolysis char at 800℃.

pore structureadsorption curvebiocharpore size distribution

陈应泉、朱波、王贤华、胥广福、杨海平、陈汉平

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华中科技大学煤燃烧国家重点实验室,武汉430074

孔隙结构 吸附曲线 生物质焦炭 孔径分布

国家自然科学基金国家自然科学基金国家自然科学基金

509300065102106550906032

2012

太阳能学报
中国可再生能源学会

太阳能学报

CSTPCDCSCD北大核心EI
影响因子:0.392
ISSN:0254-0096
年,卷(期):2012.33(8)
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