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Biogasification and combustion reactions of Turkish lignites: adsorption behavior and biogasification of Soma lignite and co-combustion of Beypazari lignite with biomass

机译:土耳其褐煤的生物气化和燃烧反应:索马褐煤的吸附行为和生物气化以及Beypazari褐煤与生物质的共燃烧

摘要

In this study, our primary objective is to understand CBM capacity of the Soma coal basin. For this reason, porosity of the coal samples must be determined. Usually, surface area and the porosity of the materials can be calculated through the N2 physical sorption experiment, in this method entire relative pressure range (10-8 to 1) can be analyzed without using high pressure equipments. However, for microporous materials like carbon materials and zeolites physical sorption occurs at very low relative pressure ranges (10-8 to 10-3) and experiments that are conducted with N2 are less reliable due to the low diffusion rate and adsorption equilibrium in the pores between 0,5 to 1 nm at 77 K. It is also known that specifically for carbon materials experiments that are conducted at low temperatures such as N2 sorption causes pore shrinkage that leads to the low sorption equilibrium.
机译:在这项研究中,我们的主要目标是了解索马盆地的煤层气产能。因此,必须确定煤样品的孔隙率。通常,可以通过N2物理吸附实验来计算材料的表面积和孔隙率,在这种方法中,无需使用高压设备就可以分析整个相对压力范围(10-8至1)。但是,对于微孔材料(如碳材料和沸石),在相对较低的相对压力范围(10-8至10-3)下会发生物理吸附,并且由于孔中的低扩散速率和吸附平衡,使用N2进行的实验不太可靠。在77 K时介于0.5到1 nm之间。众所周知,对于碳材料,在低温下进行的实验(例如N2吸附)会导致孔收缩,从而导致低吸附平衡。

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