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Published byFerdinand Oliver Modified over 8 years ago
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Infiltration Equations Fundamental Mass Balance Equation: Darcy’s Law (z direction): Where
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Infiltration Equations h( ), K(
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Infiltration Equations h( ), K(
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Infiltration Equations h( ), K(
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Infiltration Equations Vertical Darcy’s Law is then Soil water diffusivity is defined combining
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Infiltration Equations In three dimensions, using K ) defining the specific moisture capacity as C( ) = d /d
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Infiltration Equations For 1-D vertical, saturated flow:
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Infiltration Equations Boundary conditions for infiltration at ground surface:
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Infiltration Equations Lower boundary conditions for infiltration
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Infiltration Equations Mixed form of Richards Equation
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Infiltration Equations Parameters (van Genuchten, 1980): where m = 1-1/n for n > 1 S e = ( - r )/( s - r ) r is the residual volumetric moisture content l, and n are van Genuchten model parameters
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Infiltration Equations Parameters: Rosetta by Marcel G. Schaap (1999) Soil textural classes; Sand, silt and clay percentages; Sand, silt and clay percentages and bulk density; Sand, silt and clay percentages, bulk density and the value of at = 330 cm (33 kPa); and Sand, silt and clay percentages, bulk density and the value of at = 330 and 15,000 cm (33 and 1500 kPa).
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Infiltration Equations
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Green-Ampt from conceptualization: Darcy’s Law: combining:
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Infiltration Equations since f = dF/dt how is this solved?
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Infiltration Equations Green-Ampt ponding time for t < t p, how are f and F computed?
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Infiltration Equations Green-Ampt with a hyetograph discrete, steady pulses of rainfall of t duration is used to describe i(t) F(t + t) = F(t) + i(t) t while f < i when the surface is ponded throughout the time increment:
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Infiltration Equations Green-Ampt with hyetograph continued... If f(t + t) < i(t), then ponding occurs during the time interval and using f(t) = i(t) and F(t) = F p : then t p = t + t' where
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after Chow et al., 1988
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Infiltration Equations Green-Ampt parameters, after Chow et al., 1988
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Infiltration Equations Kostiakov
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Infiltration Equations Horton
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Infiltration Equations Holtan
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Infiltration Equations Phillip
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Infiltration Equations Smith-Parlange
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