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Physical Basis for Quasi-Universal Relationships Describing Bankfull Hydraulic Geometry of Sand-Bed Rivers

机译:含沙河河岸水力几何关系的拟-普遍关系的物理基础

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摘要

Empirical data indicate that hydraulic geometry relationships for single-thread sand-bed rivers (i.e., rivers with median bed-material size between 0.062 and 0.50 mm) can be delineated such that bankfull width, bankfull depth, and channel slope are related in consistent ways to bankfull discharge. Such relationships ought to be the external expression of physical relationships intrinsic to sand-bed river dynamics. In this study, a back-calculation is performed to identify parameters (exponents and coefficients) for three relationships taken to be intrinsic to sand-bed rivers: (1) a generalized Manning-Strickler resistance relationship; (2) a relationship for channel-forming Shields number; and (3) a relationship for sand yield at bankfull flow. To back-calculate parameters for the physical relationships, first the hydraulic geometry relationships are expressed in suitable dimensionless form. Second, the physical relationships are expressed with coefficients and exponents that are analytically related to parameters in the hydraulic geometry relationships. Third, parameters from the hydraulic geometry relationships are used to calculate parameters for the physical relationships. The analysis yields the following results for the sand-bed rivers: (1) no physical basis exists for using an exponent of 1/6 in the resistance relationship; (2) channel-forming Shields number decreases with particle Reynolds number, and thus grain size, in a consistent way; and (3) sand concentration at bankfull flow must decline with increasing bankfull discharge. Although each of these relationships could have been established independently on its own, in this study they have been obtained as the only conclusions consistent with the observed hydraulic geometry relationships and the proposed physical framework. The analysis also yields a useful, dimensionally homogeneous predictive relationship for bankfull discharge as a function of bankfull width, bankfull depth, bed slope, and bed-material median grain size. Bankfull hydraulic geometry; Sand-bed rivers; Suspended-load rivers; Bankfull discharge; Bankfull
机译:经验数据表明,单线沙床河流(即,河床中位物料尺寸在0.062至0.50 mm之间的河流)的水力几何关系可以被描述,从而使堤岸宽度,堤岸深度和河道坡度以一致的方式关联完全放电。这种关系应该是沙床河流动力学固有的物理关系的外部表达。在这项研究中,进行了反向计算以识别沙床河流固有的三个关系的参数(指数和系数):(1)广义的曼宁-斯特里克勒阻力关系; (2)与形成信道的Shields编号的关系; (3)堤岸满流量下的出砂率关系。为了反算物理关系的参数,首先以合适的无量纲形式表示水力几何关系。其次,用与液压几何关系中的参数解析相关的系数和指数来表示物理关系。第三,来自水力几何关系的参数用于计算物理关系的参数。对于沙床河流,分析得出以下结果:(1)在阻力关系中使用1/6的指数不存在物理依据; (2)通道形成的Shields数以一致的方式随粒子雷诺数而减小,从而随晶粒尺寸减小; (3)满溢流量下的砂浓度必须随着满溢流量的增加而降低。尽管这些关系中的每一个都可以独立地独立建立,但是在本研究中,它们是与观察到的水力几何关系和所提出的物理框架一致的唯一结论。该分析还产生了一个有用的,尺寸均匀的预测关系,作为堤宽的函数,堤宽,堤深,床坡度和床料中值晶粒尺寸的函数。 Bankfull液压几何;沙床河流;吊河银行全额清算;银行满额

著录项

  • 来源
    《Journal of Hydraulic Engineering》 |2011年第7期|p.739-753|共15页
  • 作者单位

    Dept. of Civil and Environmental Engineering, Southern Illinois Univ. Carbondale, 1230 Lincoln Dr., MC 6603, Carbondale, IL 62901;

    Dept. of Civil and Environmental Engineering, Southern Illinois Univ. Carbondale, 1230 Lincoln Dr., MC 6603, Carbondale, IL 62901;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    depth; bankfull width; slope; median grain size;

    机译:深度;银行全宽;坡;中值晶粒度;

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