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来自多个燃烧源的烟灰沉积物的孔隙结构。

Pore structure of soot deposits from several combustion sources.

作者信息

Rockne K J, Taghon G L, Kosson D S

机构信息

Department of Chemical and Biochemical Engineering, Rutgers, The State University of New Jersey, Piscataway 08854-8058, USA.

出版信息

Chemosphere. 2000 Oct;41(8):1125-35. doi: 10.1016/s0045-6535(00)00040-0.

Abstract

Soot was harvested from five combustion sources: a dodecane flame, marine and bus diesel engines, a wood stove, and an oil furnace. The soots ranged from 20% to 90% carbon by weight and molar C/H ratios from 1 to 7, the latter suggesting a highly condensed aromatic structure. Total surface areas (by nitrogen adsorption using the Brunauer Emmett Teller, BET method) ranged from 1 to 85 m2 g(-1). Comparison of the surface area and meso-pore (pores 2-50 nm) surface area predicted by density functional theory (DFT) suggested that the soot was highly porous. Total meso-pore volume and surface area ranged from 0.004-0.08 cm3 g(-1) and from 0.33-6.9 m2 g(-1) respectively, accounting for up 33% of the BET surface area. The micro-pore volume (pores <2 nm) calculated from CO2 adsorption data (by DFT) ranged from 0.0009 to 0.013 cm3 g(-1) and micro-pore surface area was 3.1-41 m2 g(-1), accounting for 10-20% of the total intra-particle (meso-plus micro-pores) pore volume and 70-90% of the total intra-particle surface area. Higher pore volume and surface area values were computed using the Dubinin Radushkevich plot technique; ranging from 0.004-0.04 cm3 g(-1) to 11-102 m2 g(-1) for micro-pore volume and surface area, respectively. Comparison of the C/H ratio and the micro-pore structure showed a strong correlation, suggesting a relationship between the condensation of the skeletal structure and micro-porosity of the soot. These data contradict literature reports that soot particles are non-porous and are consistent with recent literature reports that soil organic matter has large micro-pore surface areas.

摘要

烟灰取自五种燃烧源

十二烷火焰、船用和公交柴油发动机、木炉以及燃油炉。这些烟灰的碳含量按重量计在20%至90%之间,摩尔碳氢比在1至7之间,后者表明其具有高度缩合的芳香结构。总表面积(采用布鲁诺尔-埃米特-泰勒(BET)方法通过氮气吸附测定)在1至85平方米/克之间。通过密度泛函理论(DFT)预测的表面积和中孔(孔径2至50纳米)表面积的比较表明,烟灰具有高度多孔性。总中孔体积和表面积分别在0.004至0.08立方厘米/克和0.33至6.9平方米/克之间,占BET表面积的33%。根据二氧化碳吸附数据(通过DFT)计算得出的微孔体积(孔径<2纳米)在0.0009至0.013立方厘米/克之间,微孔表面积为3.1至41平方米/克,占颗粒内(中孔加微孔)总体积的10%至20%以及颗粒内总表面积的70%至90%。使用杜比宁-拉杜什凯维奇(Dubinin Radushkevich)绘图技术计算得出的较高孔体积和表面积值分别为:微孔体积在0.004至0.04立方厘米/克之间,微孔表面积在11至102平方米/克之间。碳氢比与微孔结构的比较显示出很强的相关性,表明骨架结构的缩合与烟灰的微孔性之间存在关联。这些数据与文献中关于烟灰颗粒无孔的报道相矛盾,与近期文献中关于土壤有机质具有大微孔表面积的报道一致。

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