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Two algorithms to estimate erosivity, expressed as energy times intensity, using daily rainfall or storm depth and duration as predictor variables are derived.. Erosivity of

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Weathered pumice-derived soils have morphologi- cal, physical, chemical and mineralogical properties that can be attributed to the in¯uence of a combination of factors involved in

However, in the case of clay soil (with 1.3±10.4% organic matter) it appears that organic matter increases the strength of moist soil aggregates, and decreases the tensile strength

Providing that the organic matter carried in soil water has surface proper- ties similar to those of organic matter in the soil matrix, transport on organic matter seems likely

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Root diameter at soil level (Tables 2 and 3) was larger under low soil water, and clay loam soil type whereas low compaction pressures (0 – 125 kPa) resulted in larger diameter

We assessed the effects of canopy position and feral pig disturbance on soil moisture, pH, and inorganic nitrogen con- centrations beneath canopies of Quercus agrifolia and