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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Physical laboratory analyses of intergravel flow through brown trout redds (Salmo trutta fario) in response to coarse sand infiltration
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Physical laboratory analyses of intergravel flow through brown trout redds (Salmo trutta fario) in response to coarse sand infiltration

机译:对粗砂渗透反应经褐鳟鱼红鳟鱼(Salmo trutta fario)的砾石间流的物理实验室分析

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In the spawning environment of salmonids, the quality of the intergravel flow is an essential abiotic requirement for the survival success of incubated embryos. As one of the most frequently investigated anthropogenic environmental impacts, the enhanced mobilization of fine sediments (< 1 mm) and their entry into riverine ecosystems is considered as a major cause for the degradation of a variety of biological processes and habitats, including the spawning habitats of salmonids. In catchments draining crystalline bedrock, however, like the Bohemian Massif in the northern part of Austria, the excessive loading of river channels with coarse sand and fine gravel sediments (D = 1-10 mm) and less cohesive than fines is common as a consequence of altered catchment land use. Here, far less understanding exists of the mechanism and the possible implications of coarse sand infiltration on the functioning of the intergravel flow in salmonid redds. To investigate the intergravel flow hydraulics in response to coarse sand infiltration (D-50 = 2 mm) in brown trout spawning redds (Salmo trutta fario) under controlled conditions, a laboratory flume experiment with three infiltration scenarios was conducted: (1) no infiltration; (2) segmental infiltration; and (3) full section infiltration. A more than two times drop in the average intergravel flow velocity was documented from scenario 1 (5.85 cms(-1)) to scenario 2 (2.53 cms(-1)) and another clear reduction was seen from scenario 2 (2.53 cms(-1)) to scenario 3 (1.61 cms(-1)). Moreover, in scenario 3, a clear reduction of the intergravel flow distance traveled was observed. Based on the findings we conclude that future considerations regarding the sustainable catchment management of salmonid fisheries should include programs to reduce not only the excessive entry of fines, but, in the relevant catchments, also the entry of excessive coarse sand into the riverine ecosystem. Copyright (C) 2016 John Wiley Sons, Ltd.
机译:在鲑鱼的产卵环境中,砾石间流的质量是孵化胚胎成功存活的基本非生物要求。作为最常被调查的人为环境影响之一,细小沉积物(<1毫米)的增强移动及其进入河流生态系统被认为是各种生物过程和生境退化的主要原因,包括鲑鱼的产卵生境。然而,在排干结晶基岩的集水区,如奥地利北部的波希米亚地块,由于集水区土地利用的改变,河道中含有粗砂和细砾石沉积物(D = 1-10 mm)且粘性不如细粒,这种情况很常见。在这里,对粗砂渗透的机制和对鲑鱼间砾石流功能的可能影响的了解要少得多。为了研究在受控条件下褐鳟鱼产卵红鳟鱼(Salmo trutta fario)对粗砂入渗(D-50 = 2 mm)的响应,进行了三种入渗情景的实验室水槽实验:(1)无入渗;(2)节段浸润;(3)全截面浸润。从情景 1 (5.85 cms(-1)) 到情景 2 (2.53 cms(-1)),平均砾石间流速下降了两倍以上,而从情景 2 (2.53 cms(-1)) 到方案 3 (1.61 cms(-1))。此外,在情景 3 中,观察到砾石间流的行进距离明显减少。根据研究结果,我们得出结论,未来关于鲑鱼渔业可持续集水区管理的考虑应包括不仅减少过度进入细则的计划,而且在相关集水区中,也应减少过多的粗沙进入河流生态系统。版权所有 (C) 2016 John Wiley & Sons, Ltd.

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