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The concept of channeled surface flow, however, remains central to the definition.
Channeled surface flow begins when overland flow becomes deep enough to be erosive; and depth of overland flow represents a balance between short-term precipitation and soil infiltration.
Moisture supply sufficient to sustain channeled surface flow is governed primarily by climate, which regulates precipitation, temperature, and evapotranspiration water loss caused by vegetation.
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Cross-channel diffusion can occur in the case of channeled surfaces.
One of the more dramatic examples of directional anisotropy is the diffusion of adatoms on channeled surfaces such as fcc (110), where diffusion along the channel is much faster than diffusion across the channel.
In others, water may be refreezing near the surface into solid sheets that can more easily channel surface melt to the sea in succeeding seasons.
Devices were then imaged using an Andor iXON 885 fluorescent camera, and at least 10 images were analyzed for binding to channel surface by calculating total surface area covered using ImageJ.
Finally, devices were modified by grafting of PEG methacrylate from surfaces to prevent non-specific protein adsorption and ultimately cell adhesion to channel surfaces.
Chen, L. et al. Migration of PIP2 lipids on voltage-gated potassium channel surface influences channel deactivation.
Optimization of the channel surface crystalline orientation can further increase on-state drive current (Ion), e.g., electron mobility is highest for a (100) Si channel surface while hole mobility is highest for a (110) Si channel surface.
Therefore, roughness of the bottom channel surface was measured using Atomic Force Microscopy (AFM) scans on the surfaces.
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