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Landscape morphology is a function of drainage, climate, and structure of a particular basin region.
Therefore, the objectives of this study were to characterize within-ditch nutrient pools and processes as a function of drainage duration: recent (7 15 years), medium (20 34 years), and long-term (36 50 years).
The study presents the hydraulic geometry relations of bankfull discharge, channel width, mean depth, cross-sectional area, longitudinal slope, unit stream power, and mean velocity at bankfull discharge as a function of drainage area using simple linear regression.
We developed downstream hydraulic geometry relationships for bankfull channel width w as a function of drainage area A, w = α Aβ, (DHGwA) for nine aggregate ecoregions comprising the conterminous United States using 1588 sites from the U.S. Environmental Protection Agency's National Wadeable Streams Assessment (WSA), including 1152 sites from a randomized probability survey sample.
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In the Global NEWS-DIN model, DIN loss by denitrification during river transport is estimated as a simple function of drainage area, which does not exhibit long-term change trends (Dumont et al., 2005).
In the lower Macquarie valley, near Trangie and Warren, the cause appears to be the mobilisation of salts from perched water tables and as a function of excessive deep drainage from water storages and conveyance channels.
The fourth-order differential equation governing the shape of the dimple as a function of time during the drainage of thin liquid film, derived by Hartland (1969, Chem. Engng Prog. Symp. Ser. No. 91, 65, 82-89), isolveded numerically.
The key of the new structure is the porous crushed-rock layer which has smaller thermal conductivity with function of drainage and blocking of moisture migration induced by freezing.
Indeed it's hydraulic connection to the limestone layers and their permeability was not clear as well as the exact position and function of drainage pipes which had been placed in the rockfill below the platform.
We chose a function of parabola-like form to represent drainage efficiency (Fig. 4), in which when the depth of AWORS exceeded 120 mm, drainage efficiency was assumed to be the same because the drainage system was always overwhelmed.
These phases were a function of the rate of change in drainage density with defined minimum contributing area.
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