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首页> 外文期刊>Journal of soil & sediments >Sediment dynamics and the role of flash floods in sediment export from medium-sized catchments: a case study from the semi-arid tropical highlands in northern Ethiopia
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Sediment dynamics and the role of flash floods in sediment export from medium-sized catchments: a case study from the semi-arid tropical highlands in northern Ethiopia

机译:沉积动力学和山洪在中等规模流域沉积物输出中的作用:以埃塞俄比亚北部半干旱热带高地为例

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摘要

Purpose The Ethiopian highlands are a fragile environment characterized by steep slopes, intense rainfall, a sparse vegetation cover, and the occurrence of flash floods. Although important efforts have been made to mitigate the ongoing soil erosion and land degradation problems, the sediment dynamics at medium-sized catchment scale (100-10,000 km~2) are not fully understood. Therefore, this study aims to provide a better understanding of sediment export processes and the importance of flash flood events in semi-arid tropical catchments.rnMaterials and methods Measuring campaigns were conducted in ten sub-catchments of the Geba, a tributary of the Tekeze, representative of the northern Ethiopian highlands. During two to four rainy seasons, the rivers were sampled for their suspended sediment concentration (SSC) and runoff discharge.rnResults and discussion Variations in SSC and sediment grain size distribution indicate changes in sediment supply during the rainy season due to the depletion of readily availablernsediments and the development of a vegetation cover. Also, during flood events, changes in sediment supply are observed. Sediment yields (i.e., 497-6,543 t km~(-2) year~(-1)) are higher than suggested by previous studies and correlate with rainfall depth. The majority of sediment export occurs during a few short but intense flash floods. No clear effect of implemented soil and water conservation measures could be detected in the sediment yields of the catchments. Conclusions Sediment export rates in the Ethiopian highlands are high, are characterized by important changes in sediment supply, and are mainly controlled by the occurrence and magnitude of flash flood events. Mitigation measures to reduce sediment yield at the catchment scale should therefore not only focus on the reduction of hillslope erosion rates but also on the magnitude of these floods.
机译:目的埃塞俄比亚高地是一个脆弱的环境,其特征是陡峭的山坡,强降雨,稀疏的植被覆盖和山洪暴发。尽管人们为缓解持续的水土流失和土地退化问题做出了巨大努力,但对中型集水规模(100-10,000 km〜2)的沉积物动力学还没有完全了解。因此,本研究旨在更好地了解沉积物的输出过程以及半干旱热带流域突发性洪水事件的重要性。材料和方法在特克泽支流格巴支流的十个子流域开展了测量活动。埃塞俄比亚北部高地的代表。在两到四个雨季中,对河流的悬浮泥沙浓度(SSC)和径流量进行了采样。rn结果与讨论SSC和泥沙粒度分布的变化表明,由于容易获得的沉积物的耗尽,雨季期间的泥沙供应发生了变化。以及植被覆盖的发展。此外,在洪水事件中,观察到沉积物供应量的变化。沉积物产量(即497-6,543 t km〜(-2)年〜(-1))高于以前的研究结果,并且与降雨深度有关。大部分的沉积物出口发生在几次短暂但强烈的山洪暴发期间。在集水区的泥沙产量中未发现已实施的水土保持措施的明显效果。结论埃塞俄比亚高地的泥沙出口率很高,其特点是沉积物供应发生了重要变化,并且主要受暴洪事件的发生和程度控制。因此,在流域尺度上减少沉积物产量的缓解措施不仅应着重于降低山坡侵蚀率,而且应着重于这些洪水的规模。

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  • 来源
    《Journal of soil & sediments》 |2010年第4期|p.611-627|共17页
  • 作者单位

    Department of Earth and Environmental Sciences, K.U. Leuven, Celestijnenlaan 200 E, 3001 Heverlee, Belgium;

    rnDepartment of Earth and Environmental Sciences, K.U. Leuven, Celestijnenlaan 200 E, 3001 Heverlee, Belgium Department of Land Resources Management and Environmental Protection, Mekelle University, Mekelle, Ethiopia;

    rnDepartment of Earth and Environmental Sciences, K.U. Leuven, Celestijnenlaan 200 E, 3001 Heverlee, Belgium;

    rnDepartment of Geography, Ghent University, 9000 Gent, Belgium;

    rnDepartment of Earth and Environmental Sciences, K.U. Leuven, Celestijnenlaan 200 E, 3001 Heverlee, Belgium;

    rnDepartment of Earth and Environmental Sciences, K.U. Leuven, Celestijnenlaan 200 E, 3001 Heverlee, Belgium;

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

    catchment; flash floods; hysteresis; sediment yield; soil conservation; suspended sediments;

    机译:集水;洪水泛滥;磁滞泥沙产量水土保持;悬浮沉积物;

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