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The model calculations show that the length of flow segment is generally more than the length of the Kuhn segment, and for high molecular weight polymers, the length of the flow segment is considerably less than the length of polymer chain between molecular entanglements.
Fig. 5 Series of resampled UAS-derived DEMs showing the loss of detail with coarser resolution data depicted in the varying lavasheds (orange) and the total length of flow paths in a given lavashed.
It is defined as the length of flow path projected to the horizontal of non-channel flow from a point on the drainage divide to a point on the adjacent stream channel (Gardiner 1975).
Horton (1945) defined length of overland flow (Lg) as the length of flow path, projected to the horizontal of non-channel flow from a point on the drainage divide to a point on the adjacent stream channel.
The length of overland flow (Lg) is the length of flow path, projected to the horizontal, non-channel flow from a point on the stream divide to a point on the neighboring stream channel (Horton 1945).
Length of overland flow which is half the reciprocal of drainage density (Horton 1945) is used to describe the length of flow of water over the ground before it becomes concentrated in definite stream channels.
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Given that headwater streams comprise a large portion of the length of flowing waterways in western Oregon forests, there is a need to better understand how forest management affects headwater forest taxa and their habitats.
In general, maximum expected VEI for the eruption correlated well with the estimated length of flows from individual volcanoes for lahars, debris avalanches and PFs, but not for lateral blasts, perhaps suggesting that these events have an uncertain provenance (are more difficult to anticipate).
We gave suggestion to further optimize the landscape pattern: reducing percentage cover of grasslands with high soil erosion rate; decreasing soil erosion rate of sediment source in the Heishui subwatershed; increasing lengths of flow path from crops to river channels.
A larger value of length of overland flow indicates longer flow path and thus gentler slopes.
In this study, linear parameters are bifurcation ratio, drainage density, texture ratio, length of overland flow, stream frequency, and the shape parameters are circularity ratio, form factor, elongation ratio and compactness coefficient.
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