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Geometrical attributes of pore systems in soil have shown fractal scaling. Scaling in natural materials is inherently statistical, i.e., fractal dimensions may change with scale. While fractal dimensions characterizing pore surface roughness, D s , or scaling of pore sizes, D v , have been reported, seldom are both measurements made at more than one scale. We examine a scale effect...
Tillage and residue management influence soil organic carbon (SOC) and lead to changes in soil physical behaviour and functioning. We examined the effect of the clay-to-carbon ratio on soil physical properties in a humid sandy loam soil with contrasting tillage and residue management. Soil was sampled at the 0–10, 10–20 and 25–30cm depths of a sandy loam soil at Flakkebjerg, Denmark in 2013. We used...
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