Croke Jacky, Thompson Chris, Fryirs Kirstie
School of Geography, Planning and Environmental Management, University of Queensland, St Lucia, Brisbane, Queensland 4072, Australia; Department of Science, Information Technology and Innovation, Ecoscience Precinct, Dutton Park, Queensland 4102, Australia.
School of Geography, Planning and Environmental Management, University of Queensland, St Lucia, Brisbane, Queensland 4072, Australia.
J Environ Manage. 2017 Apr 1;190:9-19. doi: 10.1016/j.jenvman.2016.12.046. Epub 2016 Dec 24.
In perennial stream settings, there is abundant literature confirming that riparian vegetation affects flood hydrology by attenuating the flood wave, enhancing deposition and reducing bank erosion. In contrast, relatively little is known about the effectiveness of riparian vegetation during floods in hydrologically-variable regions. The dominant channel form in these settings is often referred to as a 'macrochannel' or compound channel-in-channel which displays multiple inundation surfaces where it is often difficult to identify the active channel bank and bank top. This study uses the inundation pattern of recent flood events in the Lockyer Valley of South East Queensland (SEQ), Australia to present a framework which specifically considers the interaction between inundation frequency and trapping potential on a range of inundation surfaces. Using hydrological modelling and a consistent definition of floodplains and within-channel features, it outlines five key priority areas for the placement of riparian vegetation to alleviate common flood problems within the catchment. The highest priority for the placement of riparian vegetation to ameliorate the effects of small-moderate floods is on within-channel benches. For out-of-macrochannel flows, riparian vegetation is most effective on genetic floodplains which occupy the largest spatial extent within the valley. In particular, it identifies the need for, and benefits of, revegetation in spill out zones (SOZ) which occur where upstream channel capacity is larger and flow is funnelled at high velocity onto the floodplain downstream. This study highlights the importance of understanding the key geomorphic processes occurring within a catchment and developing effective catchment management plans to suit these conditions.
在常年性溪流环境中,有大量文献证实河岸植被通过减弱洪水波、增强沉积作用和减少河岸侵蚀来影响洪水水文特征。相比之下,对于水文多变地区洪水期间河岸植被的有效性了解相对较少。这些环境中主要的河道形态通常被称为“大河道”或复式河道套河道,其具有多个淹没面,在这些淹没面上往往很难确定活动河岸和河岸顶部。本研究利用澳大利亚昆士兰州东南部洛克耶山谷近期洪水事件的淹没模式,提出了一个专门考虑淹没频率与一系列淹没面上的截留潜力之间相互作用的框架。通过水文建模以及对洪泛平原和河道内特征的一致定义,该研究概述了河岸植被种植的五个关键优先区域,以缓解集水区内常见的洪水问题。为减轻中小洪水影响而种植河岸植被的最高优先区域是河道内的阶地。对于大河道外的水流,河岸植被在山谷中占据最大空间范围的原生洪泛平原上最为有效。特别是,该研究确定了在上游河道容量较大且水流高速汇入下游洪泛平原的溢出区进行植被恢复的必要性和益处。这项研究强调了了解集水区内发生的关键地貌过程以及制定适合这些条件的有效集水区管理计划的重要性。