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Effect of water content on kinetics of volatile organic compounds mass transfer between gas and aqueous phases during gas transport in unsaturated sand.

机译:水分对非饱和砂岩中气运过程中气相和水相之间挥发性有机化合物传质动力学的影响。

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The effect of changing water content on the air-water mass transfer kinetics of volatile organic compounds (VOCs) during gas transport in unsaturated sand was investigated. The kinetics of VOC adsorption at the air-water interface from the gas phase was explored using n-decane, whereas methylene chloride was used to examine the effect of air-water partitioning. Methane was used as the nonreactive tracer in VOC transport experiments conducted using a sand column installed in a gas chromatography system. The longitudinal dispersion of methane, estimated from methane breakthrough curve (BTC), was found to be constant in the water content range (0.07 to 0.18) examined in this study at a constant pore-gas velocity (vg), whereas an inverse proportionality between the longitudinal dispersion and vg was observed. The BTCs for methane and n-decane, measured at constant vg, were fairly symmetric, indicating that both gas diffusion and adsorption at air-water interfaces do not produce nonequilibrium transport. The shape of the methylene chloride BTC was gradually distorted at a constant vg as water content increased. Fitting methylene chloride BTCs with a modified two-region model showed that the water partitioning becomes more rate-limited as water content increases. The overall mass transfer coefficient for water partitioning of methylene chloride was found to be a direct function of specific air-water interfacial area..
机译:研究了在不饱和砂岩中进行输运过程中,水分含量的变化对挥发性有机化合物(VOCs)的气水传质动力学的影响。使用正癸烷探索了气相中VOC在空气-水界面处的吸附动力学,而使用二氯甲烷来检查空气-水分配的影响。在使用气相色谱系统中安装的沙柱进行的VOC传输实验中,甲烷用作非反应示踪剂。根据甲烷穿透曲线(BTC)估算,甲烷的纵向扩散在恒定孔隙气体速度(vg)下在本研究中研究的水含量范围(0.07至0.18)中是恒定的,而之间的反比例是观察到纵向分散和vg。甲烷和正癸烷的BTC在恒定vg下测得相当对称,表明气体扩散和在空气-水界面的吸附不会产生非平衡迁移。随着水含量的增加,二氯甲烷BTC的形状以恒定的vg逐渐变形。用改进的两区域模型拟合二氯甲烷BTCs表明,随着水含量的增加,水分配的速率受到更大的限制。发现用于二氯甲烷的水分配的总传质系数是特定的空气-水界面面积的直接函数。

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