262-3 Linking Air and Water Transport In Intact Soils to Macro-Porosity by Combining Laboratory Measurements and X-Ray Computed Tomography.

See more from this Division: S01 Soil Physics
See more from this Session: Tomography and Imaging for Soil-Water-Root Processes: III
Tuesday, October 23, 2012: 9:30 AM
Duke Energy Convention Center, Room 237-238, Level 2
Share |

Sheela Katuwal1, Trine NÝrgaard1, Per Moldrup2, Mathieu Lamande1, Dorthe Wildenschild3 and Lis de Jonge1, (1)Department of Agroecology, Aarhus University, Tjele, DK-8830, Denmark
(2)Department of Biotechnology, Chemistry and Environmental Engineering, Aalborg University, Aalborg, Denmark
(3)School of Chemical, Biological, and Environmental Engineering, Oregon State University, Corvallis, OR
Soil macropores often control fluid flow and solute transport, and quantification of macropore characteristics including their variability in space and time are essential to predict soil hydraulic and hydrogeochemical functions. In this study, measurements of air and solute transport properties and direct macropore visualization by X-ray CT scanning were carried out on 17 large (19-cm diam.; 20-cm length) undisturbed soil columns sampled across a field site (Silstrup, Denmark) with natural gradients in texture and density. Air permeability (ka) at in-situ water content and -20 hPa of matric potential, and 5% arrival time of tracer (time taken to recover 5% of the applied tracer in the outflow) were measured and linked to macropore characteristics (macro-porosity, macro-porosity of the restricting layer, number of macropores, branches, node density, and length density) quantified via X-ray CT. There was a high positive correlation between the CT-inferred macro-porosity carefully corrected for rock artifacts and the other macropore characteristics. High variability in ka (4.66 to 78.10 µm2 at -20 hPa), and 5% arrival time (0.07 to 2.36 h) were observed. Both ka and 5% arrival time were strongly positively correlated with macro-porosity (R2 = 0.77 for ka at -20 hPa; R2 = 0.59 for 5% arrival time) and macro-porosity of the restricting layer (R2 = 0.80 for ka at -20 hPa; R2 = 0.70 for 5% arrival time). High negative correlations with soil bulk density were found for ka, 5% arrival time, and macro-porosity, suggesting that density is the main control of functional soil structure and gas and solute transport at the Silstrup site. Linking gas transport and chemical tracer experiments with X-ray CT based visualization and quantification of macro-porosity was found to be a powerful method to understand field scale variations in gas and solute transport properties as influenced by soil structure and density.
See more from this Division: S01 Soil Physics
See more from this Session: Tomography and Imaging for Soil-Water-Root Processes: III