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首页> 外文期刊>The Science of the Total Environment >Variations in bar material grain-size and hydraulic conditions of managed and re-naturalized reaches of the gravel-bed Becva River (Czech Republic)
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Variations in bar material grain-size and hydraulic conditions of managed and re-naturalized reaches of the gravel-bed Becva River (Czech Republic)

机译:砾石床Becva河(捷克共和国)经管理和重新归化的河段的棒材粒度和水力条件的变化

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European multi-thread rivers have undergone rapid morphological changes during past centuries due to the extensive direct and indirect human impacts on fluvial systems. As a consequence, we can identify altered patterns of bed sediment calibre reflecting disturbed sediment connectivity and modified flow hydraulics. Changes in the grain-sizes of samples collected on 68 gravel bars in August 2015 were studied along 14.0-km river reach of the Becva River (Outer Western Carpathian Mts., Czech Republic). The grain-size characteristics obtained were confronted with modeled flow hydraulics and the present stage of the channel. The studied channel reach is presently characterized by several distinctive sections: for a long time (ca. 100 years) regulated single channel sections with artificial bank stabilizations incised several meters in the floodplain and by contrast, multi-thread channel patterns of two sections, which have witnessed retrograde development after large floods in 1997 and 2010 with 100- and 50-year recurrence intervals, respectively. The present channel behaviour of managed (regulated) and re-naturalized (multi-thread) river sections corresponded well with the modeled hydraulic variables for one-year discharge recurrence interval. Especially, re-naturalized river sections showed lower values of flow competence which facilitated the deposition of sediment material in the form of gravel bars. The high occurrence of lateral sediment sources (e.g., tributaries, bank failures) together with sediment disconnectivities (e.g., boulder ramps) in the longitudinal river reach were observed, and grain-size parameters did not particularly reflect the hydraulic conditions. Especially tributaries as sediment inputs had significant effect on bar grain size and increase of channel diversity, although, in general results indicate a gradual downstream fining. (C) 2018 Elsevier B.V. All rights reserved.
机译:由于人类对河流系统的广泛直接和间接影响,欧洲多线程河流在过去几个世纪中经历了快速的形态变化。因此,我们可以确定反映出受干扰的泥沙连通性和修改后的水力的床泥沙口径的变化模式。 2015年8月,在Becva河(捷克共和国西喀尔巴阡山)的14.0公里河段,研究了从68个砾石坝上采集的样品的粒径变化。所获得的晶粒尺寸特性面临着模型化的流动水力学和通道的当前阶段的挑战。目前,所研究的河道有几个截然不同的断面:在很长一段时间(约100年)内,在漫滩上切开了几米的人工河岸稳定装置,调节了单河道断面,与此相反,两个断面的多螺纹断面模式经历了1997年和2010年的大洪水之后,逆行发展,分别发生了100年和50年。当前的管理(调节)河段和重新归化(多线程)河段的河道行为与为期一年的排放重复间隔的模型水力变量很好地吻合。特别是,重新归化的河段显示出较低的水流能力值,这有助于以砾石条形式沉积沉积物。观察到在纵向河段中侧向沉积物源(例如支流,河堤破坏)的大量发生以及沉积物的不连续性(例如巨石坡道),并且粒度参数并没有特别反映水力条件。尽管一般结果表明下游逐渐细化,但特别是支流作为沉积物输入对棒材的晶粒尺寸和河道多样性的增加有重大影响。 (C)2018 Elsevier B.V.保留所有权利。

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