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Infiltration is a critical process impacting the hydrological cycle, influencing runoff, groundwater recharge, and soil moisture dynamics. Understanding and modeling infiltration capacity is vital for effective hydrologic design, flood forecasting, and watershed management. This chapter explores various factors affecting infiltration, different empirical and conceptual models for modeling infiltration processes, and the recent advances that enhance the accuracy of these models.
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References
Chapter_29_Model.pdfClass Notes
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Final Test
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Term: Infiltration Capacity
Definition: The maximum rate at which soil can absorb rainfall under specific conditions.
Term: Infiltration Rate
Definition: The actual rate of infiltration, which may be less than the infiltration capacity depending on rainfall rate.
Term: Horton’s Infiltration Model
Definition: An empirical model that assumes infiltration capacity decreases exponentially over time.
Term: Richards’ Equation
Definition: An equation governing unsaturated flow in soils, integrating Darcy's law with the continuity equation.
Term: Erosion
Definition: The process by which soil and rock material are removed from the Earth's surface and transported elsewhere.