Title: | Estimation of Knudsen diffusion coefficients from tracer experiments conducted with a binary gas system and a porous medium |
Address: | "Faculty of Science and Technology, Meijo University, 1-501 Shiogamaguchi, Tenpaku-ku, Nagoya, Aichi 468-8502, Japan. Electronic address: hibiy@meijo-u.ac.jp. Faculty of Science and Technology, Meijo University, 1-501 Shiogamaguchi, Tenpaku-ku, Nagoya, Aichi 468-8502, Japan" |
DOI: | 10.1016/j.jconhyd.2018.02.007 |
ISSN/ISBN: | 1873-6009 (Electronic) 0169-7722 (Linking) |
Abstract: | "A previous study has reported that Knudsen diffusion coefficients obtained by tracer experiments conducted with a binary gas system and a porous medium are consistently smaller than those obtained by permeability experiments conducted with a single-gas system and a porous medium. To date, however, that study is the only one in which tracer experiments have been conducted with a binary gas system. Therefore, to confirm this difference in Knudsen diffusion coefficients, we used a method we had developed previously to conduct tracer experiments with a binary carbon dioxide-nitrogen gas system and five porous media with permeability coefficients ranging from 10(-13) to 10(-11)?ª+m(2). The results showed that the Knudsen diffusion coefficient of N(2) (D(N2)) (cm(2)/s) was related to the effective permeability coefficient k(e) (m(2)) as D(N2)?ª+=?ª+7.39?ª+x?ª+10(7)k(e)(0.767). Thus, the Knudsen diffusion coefficients of N(2) obtained by our tracer experiments were consistently 1/27 of those obtained by permeability experiments conducted with many porous media and air by other researchers. By using an inversion simulation to fit the advection-diffusion equation to the distribution of concentrations at observation points calculated by mathematically solving the equation, we confirmed that the method used to obtain the Knudsen diffusion coefficient in this study yielded accurate values. Moreover, because the Knudsen diffusion coefficient did not differ when columns with two different lengths, 900 and 1500?ª+mm, were used, this column property did not influence the flow of gas in the column. The equation of the dusty gas model already includes obstruction factors for Knudsen diffusion and molecular diffusion, which relate to medium heterogeneity and tortuosity and depend only on the structure of the porous medium. Furthermore, there is no need to take account of any additional correction factor for molecular diffusion except the obstruction factor because molecular diffusion is only treated in a multicomponent gas system. Thus, molecular diffusion considers only the obstruction factor related to tortuosity. Therefore, we introduced a correction factor for a multicomponent gas system into the DGM equation, multiplying the Knudsen diffusion coefficient, which includes the obstruction factor related to tortuosity, by this correction factor. From the present experimental results, the value of this correction factor was 1/27, and it depended only on the structure of the gas system in the porous medium" |
Keywords: | "Carbon Dioxide/*analysis Diffusion Environmental Pollutants/*analysis Glass/chemistry *Models, Theoretical Nitrogen/*analysis Permeability Porosity Soil/chemistry Volatile Organic Compounds/*analysis Binary gas system Dusty gas model Knudsen diffusion Per;" |
Notes: | "MedlineHibi, Yoshihiko Kashihara, Ayumi eng Netherlands 2018/03/10 J Contam Hydrol. 2018 Mar; 210:65-80. doi: 10.1016/j.jconhyd.2018.02.007. Epub 2018 Feb 27" |