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Geomorphic variation of a transitional river: Blue Ridge to Piedmont, South Carolina.

机译:过渡河的地貌变异:蓝岭到南卡罗来纳州皮埃蒙特。

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摘要

Field data was collected systematically to characterize the geomorphic variations in a river transition from the southern Blue Ridge to the Piedmont physiographic regions in South Carolina. Ten study reaches were surveyed for cross-sections and longitudinal profiles. Surface grid samples of bed material collected. Downstream hydraulic geometry and downstream fining of bed material were analyzed using traditional power functions and exponential decay relationships. Reach-scale channel bed morphology (bedforms) was analyzed under the assumption that the transition in bedforms is related to changes in hydraulic geometry and sediment characteristics. Well-developed downstream trends of hydraulic geometry variables (width, depth and velocity) and bed material fining were observed. However, variations within the general trends reflect the influence of a key transition zone characterized by substantial tributary inputs, drastic decreases in slope, and the presence of erosion-resistant bedrock knickpoints. Bedforms were distinguished using a regime diagram, an approach that utilizes hydraulic and sediment data that is independent of drainage area. Plots of relative grain submergence (R/D84), relative form submergence (R/H), Darcy-Weisbach friction factor (f) and slope vs. area reveal trends in the data that are not discernible with downstream models. Hydraulic, sediment, and bedform data suggest that structurally controlled breaks in slope are influential to bedform characteristics, resulting in forced morphologies that may not be distinguished using simple downstream models. This corroborates the utility of scale-independent methods, especially in mountain or transitional environments where fluvial controls may be longitudinally forced and sporadic. These results have implications for river management and restoration approaches in such environments, as scale-independent models and landscape-scale perspectives can be beneficial to management objectives.
机译:系统地收集了野外数据,以表征从南部蓝岭到南卡罗来纳州皮埃蒙特地理区域的河流过渡中的地貌变化。调查了十个研究范围的横截面和纵向轮廓。收集床料的表面网格样品。使用传统幂函数和指数衰减关系分析了床层材料的下游水力几何形状和下游细化。在河床形态的转换与水力几何形状和沉积物特征的变化有关的假设下,分析了河床河床形态(河床形态)。观察到水力几何变量(宽度,深度和速度)和床料细化的良好发展的下游趋势。但是,总体趋势内的变化反映了关键过渡带的影响,该过渡带的特征是大量的支流输入,坡度急剧下降以及存在抗侵蚀的基岩拐点。底模使用状态图进行区分,该图利用了与排水面积无关的水力和泥沙数据。相对晶粒浸没度(R / D84),相对形态浸没度(R / H),Darcy-Weisbach摩擦系数(f)和斜率与面积的关系图揭示了下游模型无法识别的数据趋势。水力,沉积物和地层数据表明,边坡的结构控制断裂对地层特征有影响,导致强迫形貌无法用简单的下游模型来区分。这证实了与比例无关的方法的实用性,尤其是在山区或过渡性环境中,河流控制可能会被纵向强加和零星地使用。这些结果对这种环境下的河流管理和恢复方法具有影响,因为与比例无关的模型和景观比例观点可能对管理目标有利。

著录项

  • 作者

    Arrington, Tanner.;

  • 作者单位

    University of South Carolina.;

  • 授予单位 University of South Carolina.;
  • 学科 Geography.;Water Resource Management.;Geomorphology.
  • 学位 M.S.
  • 年度 2013
  • 页码 85 p.
  • 总页数 85
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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