Poiseuille’s Law
- At the microscopic scale of an individual pore, approximated as a water-filled cylinder of given radius (r), the volumetric flow rate (Q) is described by Poiseuille’s equation:
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Soil water movement under saturated and unsaturated conditions
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Air and heat movement in soil and infiltration characteristics in soil
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Surface sealing, its effect on soil and crop growth and its management
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Structural management of arable soil
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Soil profile development
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Surface and subsurface soil horizons
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Soil moisture and temperature regimes
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Soil classification on the basis of USDA soil taxonomy
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The FAO-UNESCO soil classification system
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