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Effects of Soil Morphology on Hydraulic Properties

I. Quantification of Soil Morphology

^a College of Natural Resources, Univ. of Wisconsin, Stevens Point, WI 54481 USA
^b Dep. of Soil and Crop Sciences, Texas A&M Univ., College Station, TX 77843-2474 USA

View larger version (19K): [in a new window]   Fig. 1 Relative comparison of the Pearson correlation coefficients between the steady infiltration rates at different potentials (i-0.24 to i0) and the mass fractions of clay (mc), silt (msi), and sand (ms) separates, field-estimated macroporosity (macro), very fine porosity at root–soil interface (root), and laboratory-determined total soil porosity (total)