不同尺度过程对洪泛区林地恢复的重要性

F. Hughes, W. Adams, E. Muller, C. Nilsson, K. Richards, N. Barsoum, H. Décamps, R. Foussadier, Jacky Girel, Hélène Guilloy, A. Hayes, M. Johansson, L. Lambs, G. Pautou, J. Peiry, M. Perrow, F. Vautier, M. Winfield
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引用次数: 103

摘要

洪泛区林地的恢复需要了解当地和流域尺度上的过程、形式和过去管理历史之间的联系。本文描述了影响洪泛区林地物种组成的地点和河段尺度过程,特别关注洪泛区水文和沉积物输入与树种更新响应之间的关系。然后讨论了将在场地范围尺度上获得的自然科学知识与在集水区尺度上对水分配优先次序作出的决定相结合的重要性。研究对象包括瑞典的奥尔河、英国的乌塞河、法国的伊泽尔河和加隆河。在场地和河段范围内的研究结果可以对洪泛区树种再生和生长的理想条件以及提供这些条件的水流进行广泛的定义:(1)为了形成早期演替物种再生所需的沉积地点以及提供这些地点的水流,必须发生河道运动;(2)洪水事件应周期性发生,以引起河道移动并补充洪泛区地下水位;(3)洪水后地下水位下降速度必须足够慢,以使幼苗根系能够与后退的水面保持接触;(4)非季节性洪水事件可造成幼苗高死亡率,阻碍任何季节的成功再生。河漫滩林地恢复的一些要求可以通过场地和河段规模的恢复工程来实现,并具有合理可预测的生态结果。为洪泛区林地提供再生场地的更全面的方法还包括以提供能够恢复地貌过程的流动条件为目标的水分配决定。然而,很难预测生态系统对流域尺度流量分配措施的响应,因此,在西欧集中管理的河流走廊中,河流恢复措施往往局限于场地和河段尺度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The importance of different scale processes for the restoration of floodplain woodlands
The restoration of floodplain woodlands demands an understanding of the linkages between process, form and past management history at both a local and catchment scale. Site and reach scale processes that influence the species composition of floodplain woodland species are described with a particular focus on the relationships between hydrological and sediment inputs to floodplains and the regeneration response by tree species. The importance of integrating natural science knowledge gained at the site reach scale with decisions taken at the catchment scale on water allocation priorities is then discussed. Research was carried out on the River Ore in Sweden, The River Ouse in the United Kingdom and the River Isere and River Garonne in France. Research results at the site and reach scale allow broad definition of ideal conditions for the regeneration and growth of floodplain tree species and the flows that provide them: (1) channel movement has to occur for the creation of sedimentation sites required for the regeneration of early successional species and the flows that provide them; (2) flooding events should occur periodically to cause both channel movement and recharge floodplain water tables; (3) water table decline rates following a flood event must be slow enough that seedling roots can maintain contact with the retreating water front; (4) unseasonal flood events can cause high mortality of seedlings and prevent successful regeneration in any season. Some of the requirements for the restoration of floodplain woodlands can be delivered through site and reach scale restoration projects with reasonably predictable ecological outcomes. A more holistic approach to the provision of regeneration sites for floodplain woodlands would also include water allocation decisions targeted at providing flow conditions which could restore geomorphological processes. However, it is difficult to predict ecosystem responses to catchment scale flow allocation measures and, therefore, in the intensively managed river corridors of Western Europe, river restoration initiatives tend to be restricted to the site and reach scale.
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