Abstract
After more than 300 years of river management, scientific knowledge of European river systems has evolved with limited empirical knowledge of truly natural systems. In particular, little is known of the mechanisms supporting the evolution and maintenance of islands and secondary channels. The dynamic, gravel-bed Flume Tagliamento, Italy, provides an opportunity to acquire baseline data from a river where the level of direct engineering intervention along the main stem is remarkably small. Against a background of a strong alpine to mediterranean climatic and hydrological gradient, this paper explores relationships between topography, sediment and vegetation at eight sites along the active zone of the Tagliamento. A conceptual model of island development is proposed which integrates the interactions between large woody debris and vegetation, geomorphic features, sediment calibre and hydrological regime. Islands may develop on bare gravel sites or be dissected from the floodplain by channel avulsion. Depositional and erosional processes result in different island types and developmental stages. Differences in the apparent trajectories of island development are identified for each of the eight study sites along the river. The management implications of the model and associated observations of the role of riparian vegetation in island development are considered. In particular, the potential impacts of woody debris removal, riparian tree management, regulation of river flow and sediment regimes, and changes in riparian tree species' distribution are discussed. Copyright (C) 2001 John Wiley & Sons, Ltd.
| Original language | English |
|---|---|
| Pages (from-to) | 31-62 |
| Number of pages | 32 |
| Journal | Earth Surface Processes and Landforms |
| Volume | 26 |
| Issue number | 1 |
| Early online date | 1 Jan 2001 |
| DOIs | |
| Publication status | Published - 1 Jan 2001 |
Keywords
- gravel-bed river
- wood debris
- riparian woodland
- island formation
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