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    • Hydrology and Water Resources in Arizona and the Southwest, Volume 08 (1978)
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    A Sediment Yield Equation from an Erosion Simulation Model

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    Author
    Shirley, E. D.
    Lane, L. J.
    Affiliation
    Southwest Watershed Research Center, Tucson, Arizona 85705
    Issue Date
    1978-04-15
    Keywords
    Hydrology -- Arizona.
    Water resources development -- Arizona.
    Hydrology -- Southwestern states.
    Water resources development -- Southwestern states.
    Sedimentation rates
    Sediment yield
    Water pollution sources
    Estimating equation
    Equations
    Overland flow
    Simulation analysis
    Model studies
    Sedimentation
    Erosion
    Numerical analysis
    Rill erosion
    Runoff
    Hydraulic properties
    Watershed management
    Land use
    Forecasting
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    Copyright ©, where appropriate, is held by the author.
    Collection Information
    This article is part of the Hydrology and Water Resources in Arizona and the Southwest collections. Digital access to this material is made possible by the Arizona-Nevada Academy of Science and the University of Arizona Libraries. For more information about items in this collection, contact anashydrology@gmail.com.
    Publisher
    Arizona-Nevada Academy of Science
    Journal
    Hydrology and Water Resources in Arizona and the Southwest
    Abstract
    Sediment is widely recognized as a significant pollutant affecting water quality. To assess the impact of land use and management practices upon sediment yield from upland areas, it is necessary to predict erosion and sediment yield as functions of runoff, soil characteristics such as erodibility, and watershed characteristics. The combined runoff-erosion process on upland areas was modeled as overland flow on a plane, with rill and interrill erosion. Solutions to the model were previously obtained for sediment concentration in overland flow, and the combined runoff-erosion model was tested using observed runoff and sediment data. In this paper, the equations are integrated to produce a relationship between volume of runoff and total sediment yield for a given storm. The sediment yield equation is linear in runoff volume, but nonlinear in distance and, thus, watershed area. Parameters of the sediment yield equation include the hydraulic resistance parameter, rill and interrill erodibility terms, and flow depth-detachment coefficient and exponent.
    ISSN
    0272-6106
    Collections
    Hydrology and Water Resources in Arizona and the Southwest, Volume 08 (1978)

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