The influence of large wood on sediment routing and flow characteristics: A study in a low-order stream in the southern brazilian plateau

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Bruno Henrique Abatti , Gean Paulo Michel , Ronald Erwin Poeppl , Marina Refatti Fagundes , Leonardo Rodolfo Paul , Franciele Zanandrea
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Abstract

The coupling of sediment sources varies in terms of efficiency and availability based on the frequency and intensity patterns of rainfall events over time. It is commonly assumed that reaches with steeper gradients have higher longitudinal connectivity, while lower gradient reaches have lower longitudinal connectivity. However, considering that the longitudinal connectivity of channels is not always perfectly established, this conception regarding channel gradient may not always hold true. In forested regions, elements such as large wood can be the main agents of this disconnectivity. Thus, this study investigates the effects of large wood on sediment flux, flow characteristics and channel morphology in the context of the Atlantic Forest Biome in a low-order stream in the southern Brazilian plateau. To achieve this, measurements of hydrological variables, characterization of sediments, and channel morphology were conducted. Hydraulic and morphological variables were estimated to define hydraulic signatures for each river section. The influences of large wood barriers in the study section were highlighted through an analysis of hydraulic characteristics at different cross-sections and the assessment of morphological variables. The investigation revealed a tendency for a reduction in velocity of approximately 90 % in low-discharge conditions in sections where large wood barriers were present. In the case of high-magnitude events, the velocity reduction was considerably lower. Additionally, it was found that each large wood deposit presented uniqueness, and the structural characteristics of each reflected the potential for system disconnectivity. Finally, it was observed that both barriers have the capacity to store sediments, leading to the constriction of the cross-section due to the formation of sediment bars, although surveys revealed that fine sediments were poorly retained in both barriers.

大型木材对沉积物流向和水流特征的影响:对巴西南部高原一条低阶溪流的研究
根据降雨事件的频率和强度模式,沉积物来源的耦合效率和可用性各不相同。通常认为,梯度较陡的河段具有较高的纵向连通性,而梯度较低的河段则具有较低的纵向连通性。然而,考虑到河道的纵向连通性并不总是完全确定的,这种关于河道坡度的概念可能并不总是正确的。在森林地区,大木头等因素可能是造成这种不连通性的主要原因。因此,本研究以大西洋森林生物群落为背景,在巴西南部高原的一条低阶溪流中研究了大木对沉积物流量、水流特征和河道形态的影响。为此,对水文变量、沉积物特征和河道形态进行了测量。通过估算水文和形态变量,确定了每个河段的水文特征。通过分析不同断面的水力特征和评估形态变量,突出了研究河段中大型木质障碍物的影响。调查显示,在存在大型木质屏障的河段,低排水量条件下的流速有下降约 90% 的趋势。在发生高水位事件时,流速的降低幅度要小得多。此外,研究还发现,每种大型木材沉积物都有其独特性,每种沉积物的结构特征都反映了系统断开的可能性。最后,据观察,两道屏障都有储存沉积物的能力,从而形成沉积条,导致横截面收缩,但调查显示,细小沉积物在两道屏障中的滞留能力都很差。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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