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The sediment budget of a large river regulated by dams (The lower River Ebro, NE Spain)

机译:由大坝控制的大河(西班牙内布拉斯加州埃布罗河下游)的沉积物预算

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Purpose The aim of this work was to develop a comprehensive fluvial suspended sediment budget for a large regulated river, the lower River Ebro (NE Spain). Materials and methods The sediment loads of the Ebro mainstem and its main tributaries were estimated from continuous records of water discharge and turbidity (appropriately transformed to suspended sediment concentrations). Records were obtained at ten monitoring sections during the relatively dry 2008-2011 period. Results and discussion The sediment load estimated for the River Ebro upstream of the Mequinenza Reservoir is remarkable (i.e. mean suspended load of 0.6× 10~6tyear~(-1)), despite the fact that the site is already affected by a sediment deficit due to upstream reservoirs. Further downstream, and owing to their humid characteristics, the contribution of the Pyrenean tributaries (Segre and Cinca Rivers) is much larger compared with their Iberian Massif counterparts (Matarranya and Algars Rivers), with sediment loads of 0.49×10~6 and 2,260 t, respectively. The suspended sediment load trapped in the Mequinenza-Ribarroja-Flix Dam Complex for the study period was estimated at 2.3 × 10~6t. Below the dams, the sediment load was reduced by 95 % but increased gradually in a downstream direction due to the erosion processes that clear water (i.e. very low sediment concentrations) flood flows exert on the river bed and banks and the episodic contribution from ephemeral tributaries. Conclusions Reservoirs have reduced the overall sediment load and the natural variability of flow and sediment transport in the River Ebro. In addition, the sediment budget revealed that floods were not the only drivers of the sediment dynamics in the lower Ebro. For instance, the particular location of the monitoring sections showed that episodic contributions from small tributaries alter the general sediment load of the river during certain torrential events.
机译:目的这项工作的目的是为一条大型调节河埃布罗河下游(西班牙东北)制定一个综合的河流悬浮泥沙预算。材料和方法根据连续的排水和浊度记录(适当地转换为悬浮的泥沙浓度)估算了埃布罗主干及其主要支流的泥沙负荷。在相对干燥的2008-2011年期间,在十个监测部门获得了记录。结果与讨论尽管梅克嫩扎水库上游的埃布罗河已经受到了泥沙淤积的影响,但据估计,梅克伦扎水库上游的埃布罗河的泥沙淤积是惊人的(即平均悬浮泥土为0.6×10〜6tyear〜(-1))。到上游水库。比利牛斯支流(马塔拉尼亚河和阿尔加斯河)的支流,比利牛斯支流(塞格雷河和辛卡河)的下游地区,由于其湿润的特性,其贡献更大,其泥沙负荷为0.49×10〜6和2,260 t , 分别。在研究期间,Mequinenza-Ribarroja-Flix大坝综合体中截留的悬浮泥沙负荷估计为2.3×10〜6t。在大坝下方,泥沙负荷减少了95%,但在下游方向逐渐增加,这是由于冲刷过程导致清水(即非常低的泥沙浓度)洪水在河床和河岸上施加的作用以及短暂支流的周期性贡献。结论水库降低了埃布罗河的总体泥沙负荷以及流量和泥沙输送的自然变化。此外,沉积物预算显示,洪水不是埃布罗河下游沉积物动力学的唯一驱动因素。例如,监测部分的特定位置表明,在某些洪流事件中,小支流的阵发性贡献改变了河流的总体泥沙负荷。

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  • 来源
    《Journal of soil & sediments》 |2013年第5期|966-980|共15页
  • 作者

    Alvaro Tena; Ramon J. Batalla;

  • 作者单位

    Fluvial Dynamics Research Group -RIUS, University of Lleida, 25198 Lleida, Catalonia, Spain,Department of Environment and Soil Sciences, University of Lleida, 25198 Lleida, Catalonia, Spain;

    Fluvial Dynamics Research Group -RIUS, University of Lleida, 25198 Lleida, Catalonia, Spain,Department of Environment and Soil Sciences, University of Lleida, 25198 Lleida,Catalonia, Spain,Catalan Institute for Water Research, H2O Building, 17003 Girona, Catalonia, Spain,Forest Science Centre of Catalonia, Solsona, 25280 Lleida, Catalonia, Spain;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Fluvial sediment budget; Reservoirs; River Ebro; Suspended sediment transport;

    机译:河流沉积物预算;水库;埃布罗河;悬浮泥沙输送;

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