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A customised approach to determining the geomorphic effectiveness of small flood events in a regulated river

机译:一种定制的方法,可以确定受监管河流小洪水事件的地貌效力

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摘要

The construction of dams significantly alters flow and sediment regimes with subsequent deleterious effects on the morphological and ecological character of rivers. Effective experimental floods can ameliorate the downstream geomorphic impacts of dams. The traditional view is that large floods are required to perform effective geomorphic work, and the geomorphic outcomes of small floods are often overlooked. Many river restoration frameworks do not consider small floods. Yet, there is evidence that the hydrological characteristics that ameliorate specific geomorphic impacts in a river are unique to each river, and a customised approach to setting the right mix of floods (including small experimental floods) is needed. In this study, we modify an existing flood effectiveness model developed for large floods, for determining the geomorphic effectiveness of small floods in a highly regulated Australian river. Two flood classes were added to the model (medium peak stream power and moderate total energy expenditure), and the flood power characteristics were rescaled to reflect the relative difference in the magnitude of the small floods and the magnitude of the geomorphic work performed. Using a step-wise approach, this customised model determined the geomorphic effectiveness of small floods. The best flood for ameliorating the geomorphic impacts of flow regulation had medium to long duration (10 to 51 days), high peak unit stream power (77 to 123 Wm(-2)) and moderate to large total energy expenditure (78,600 to 342,320 x 10(3) J). This approach to determining flood effectiveness for small floods is applicable to other geomorphically impacted river channels downstream of dams and can be used to inform experimental flood releases for geomorphic outcomes.
机译:水坝的建设显着改变了流动和沉积物制度,随后对河流形态和生态特征的有害影响。有效的实验洪水可以改善水坝的下游地貌冲击。传统观点是,大型洪水需要进行有效的地貌工作,并且往往忽略了小洪水的地貌结果。许多河流修复框架不考虑小洪水。然而,有证据表明,在河流中改善特定地貌影响的水文特征是每条河流的独特性,以及需要定制的方法来设定洪水的正确混合(包括小实验洪水)。在这项研究中,我们修改了对大型洪水开发的现有洪水效力模型,以确定澳大利亚高度监管的小洪水的地貌效果。将两种洪水类添加到模型(中峰流功率和中等总能量消耗)中,重新探斥洪水特性以反映小洪水幅度的相对差异,并且所执行的地貌工作的大小。使用逐步方面的方法,这种定制模型确定了小洪水的几何效果。改善流量调节的几何冲击的最佳洪水有中长期(10至51天),高峰单位流电源(77至123瓦米(-2))和中度到大的总能量消耗(78,600至342,320 x 10(3)j)。这种对小洪水洪水效力的这种方法适用于水坝下游的其他地理上受影响的河流渠道,可用于通知实验洪水释放地貌结果。

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