overland flow

Sheet erosion is the transport of loosened soil particles by overland flow.

Overland flow can erode soil particles and transport them downslope.

Soil that is at field capacity (among other reasons) may preclude infiltration so to increase overland flow.

He believed these to include drainage density, channel slope, overland flow length, and other less important factors.

Vegetation can also be used to control water erosion by limiting surface processes such as sheet wash and overland flow.

Water flowing over the ground surface as overland flow cuts channels, and these channels combine to form a stream network.

The erosion associated with overland flow may occur through different methods depending on meteorological and flow conditions.

However, their dense canopies and thick litter do reduce overland flows compared to grazed grasses.

Paved surfaces such as asphalt, which are designed to be flat and impermeable, rapidly achieve Horton overland flow.

Fluvial geomorphologists would assist in examining sediment transport in overland flow.

Thereafter the model recalculates the current solution with a smaller time step for the affected process (reach or overland flow or porous media).

If overland flow is directly responsible for sediment entrainment but does not form gullies, it is called "sheet erosion".

He analyzed and separated the water cycle into the processes of infiltration, evaporation, interception, transpiration, overland flow, etc.

His studies of overland flow aided in the understanding of soil erosion and provided a scientific basis for soil conservation efforts.

Overland flow can be routed between sub-areas, between subcatchments, or between entry points of a drainage system.

The topographic dividing line around the perimeter of a basin, beyond which overland flow (i.e.; runoff) drains away into another basin.

Surface runoff consists of building roof runoff, parking lot runoff and overland flow from properties to the north of the project site.

Horton overland flow is most commonly encountered in urban construction sites and rural dirt roads, where vegetation has been stripped away, exposing bare dirt.

As water accumulates in the subsurface, saturation may occur, and interflow may exfiltrate as return flows, becoming overland flow.

In fluvial geomorphology, a rill is a narrow and shallow incision into topsoil layers, resulting from erosion by overland flow or surface runoff.

This runoff is called saturation excess overland flow or saturated overland flow.

His results demonstrate that the salient factor in aqueous soil erosion is the minimum length of overland flow necessary to produce enough runoff to effect erosion.

Surface-water hydrology is a field that encompasses all surface waters of the globe (overland flows, rivers, lakes, wetlands, estuaries, oceans, etc.).

Surface runoff, also known as storm flow or overland flow, is that portion of precipitation that runs rapidly over the ground surface to a defined channel.

Horton overland flow - the tendency of water to flow horizontally across land surfaces when rainfall has exceeded infiltration capacity and depression storage capacity.