Richards equation
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non-linear partial differential equation that represents the movement of water in unsaturated soils
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differential equation
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digital object identifier
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International Standard Serial Number
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conservation of mass
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bibcode
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tensor
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aquifer
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partial differential equation
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divergence
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isotropy
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chain rule
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Q22908627
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Lewis Fry Richardson
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infiltration
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vadose zone
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water content
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soil type
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hydraulic conductivity
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aspect ratio
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discretization
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