= Horton overland flow
{wiki=Horton_overland_flow}
Horton overland flow refers to a type of surface runoff that occurs when rainfall intensity exceeds the soil's infiltration capacity, leading to water flowing over the land surface. The concept was introduced by the hydrologist Robert E. Horton in the early 20th century. This process is characterized by several key features: 1. **Infiltration Capacity**: Each soil type has a specific ability to absorb water, known as infiltration capacity.
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