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    Bed‐Surface Size Changes in Gravel‐Bed Channel

    Source: Journal of Hydraulic Engineering:;1989:;Volume ( 115 ):;issue: 006
    Author:
    Roger A. Kuhnle
    DOI: 10.1061/(ASCE)0733-9429(1989)115:6(731)
    Publisher: American Society of Civil Engineers
    Abstract: Equilibrium sediment transport experiments were made in two flumes, one with a 6‐m long by 0.15‐m wide channel and the other with an 11‐m long and either 0.74‐ or 0.53‐m wide channel. The sediment (0.1 to 32 mm,
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      Bed‐Surface Size Changes in Gravel‐Bed Channel

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    http://yetl.yabesh.ir/yetl1/handle/yetl/23158
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    contributor authorRoger A. Kuhnle
    date accessioned2017-05-08T20:40:32Z
    date available2017-05-08T20:40:32Z
    date copyrightJune 1989
    date issued1989
    identifier other%28asce%290733-9429%281989%29115%3A6%28731%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/23158
    description abstractEquilibrium sediment transport experiments were made in two flumes, one with a 6‐m long by 0.15‐m wide channel and the other with an 11‐m long and either 0.74‐ or 0.53‐m wide channel. The sediment (0.1 to 32 mm,
    publisherAmerican Society of Civil Engineers
    titleBed‐Surface Size Changes in Gravel‐Bed Channel
    typeJournal Paper
    journal volume115
    journal issue6
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)0733-9429(1989)115:6(731)
    treeJournal of Hydraulic Engineering:;1989:;Volume ( 115 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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