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    Surface-Subsurface Model for Trench Infiltration Basins

    Source: Journal of Water Resources Planning and Management:;1998:;Volume ( 124 ):;issue: 005
    Author:
    James C. Y. Guo
    DOI: 10.1061/(ASCE)0733-9496(1998)124:5(280)
    Publisher: American Society of Civil Engineers
    Abstract: This study presents a surface-to-subsurface two-dimensional (2D) model for the design of infiltration trench basins. It assists engineers in estimating the size of an infiltration basin and in determining the subsurface geometry required for having an adequate hydraulic conductivity. The Federal Aviation Administration (FAA) method is revised to predict the detention storage volume by maximizing the volume difference between the design storm runoff and the basin infiltration rate. Diffusion of the wetting front beneath the basin is depicted by the streamline-equipotential flow-net model derived in this study with consideration of nonisotropic permeability. The required subsurface geometry is found to be related to the width of the basin, and the length of the saturation zone is proportional to the ratio of infiltration rate-to-coefficient of permeability.
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      Surface-Subsurface Model for Trench Infiltration Basins

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    contributor authorJames C. Y. Guo
    date accessioned2017-05-08T21:07:28Z
    date available2017-05-08T21:07:28Z
    date copyrightSeptember 1998
    date issued1998
    identifier other%28asce%290733-9496%281998%29124%3A5%28280%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/39540
    description abstractThis study presents a surface-to-subsurface two-dimensional (2D) model for the design of infiltration trench basins. It assists engineers in estimating the size of an infiltration basin and in determining the subsurface geometry required for having an adequate hydraulic conductivity. The Federal Aviation Administration (FAA) method is revised to predict the detention storage volume by maximizing the volume difference between the design storm runoff and the basin infiltration rate. Diffusion of the wetting front beneath the basin is depicted by the streamline-equipotential flow-net model derived in this study with consideration of nonisotropic permeability. The required subsurface geometry is found to be related to the width of the basin, and the length of the saturation zone is proportional to the ratio of infiltration rate-to-coefficient of permeability.
    publisherAmerican Society of Civil Engineers
    titleSurface-Subsurface Model for Trench Infiltration Basins
    typeJournal Paper
    journal volume124
    journal issue5
    journal titleJournal of Water Resources Planning and Management
    identifier doi10.1061/(ASCE)0733-9496(1998)124:5(280)
    treeJournal of Water Resources Planning and Management:;1998:;Volume ( 124 ):;issue: 005
    contenttypeFulltext
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