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Titel Unified Measurement System (UMS) for the Gas Dispersion Coefficient, Permeability and Diffusion Coefficient, and their Interrelations in Differently-Textured, Variably-Saturated Soil
VerfasserIn S. Hamamoto, P. Moldrup, K. Kawamoto, T. Komatsu, D. E. Rolston
Konferenz EGU General Assembly 2009
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 11 (2009)
Datensatznummer 250024819
 
Zusammenfassung
The transport of gaseous compounds in soil occurs by gas diffusion, advection, and dispersion. These gas transport processes are controlled by the soil-gas diffusion coefficient (Dp), air permeability (ka) and soil-gas dispersion coefficient (DH), respectively. Among the three main gas transport parameters, the DH and how it is linked to soil types, moisture conditions and other gas transport parameters, are the least understood. In this study, a unified measurement system (UMS) that enables sequential measurement of gas transport parameters (i.e., Dp, ka and DH) on the same soil core was developed. Using different particle size fractions of non-aggregated (Toyoura sand) and aggregated (Nishi-Tokyo loam) soils, the effects of soil structure, particle (aggregate) size and column scale (5-cm i.d. and 30-cm or 60-cm length) on the three gas transport parameters were investigated and possible links between gas transport parameters were identified. In the arterial pore region (APR) for both soils (soil-air content (ɛ) < around 0.45 m3 m-3, corresponding to the total pore volume for Narita sand and the inter-aggregate pore volume for Nishi-Tokyo loam), measured gas dispersivity (λ = DH/u0, u0: pore-air velocity) for both soils decreased with increasing ɛ. However, for Nishi-Tokyo loam at higher ɛ, the λ values increased again with higher ɛ, suggesting that the gas movement becomes more dispersive since intra-aggregate pores with a smaller and complicated pore structure act as additional tortuous gas pathways. In the APR for both soils, strong linear relations between the gas dispersivity (λ), the pore tortuosity-connectivity factor (X) calculated from the measured Dp and the log-transformed ka were found.