Characteristics and temporal variability of large woody debris trapped in a reservoir on the River Rhone (Rhone): implications for river basin management

Woody debris is a structural element of river systems, which provides habitats for aquatic communities but may enhance flooding frequency and damage infrastructure. An abundant scientific literature highlights the role of the wood, particularly in the fields of ecology and geomorphology. In order to find a balance between woody debris preservation and reintroduction for ecological purposes, and the need for channel clearing for risk management, more research is now needed to understand woody debris delivery residence time and transport dynamics in regulated rivers. This work uses reservoirs, which trap woody debris, to determine its geographical origin and temporal variability in relation to the flow regime. This approach is illustrated by data collected on the Genissiat dam on the upper Rhone river (France), which traps all the woody debris even during high floods. The results show that the wood input increases with flood frequency but also depends on the position of the flood event in the hydrological series. The wood load is significantly high and removed from the reservoir when the flood recurrence attains one in 1.5 years. Qualitative description of the wood extracted from the reservoir indicates that 83% of the pieces, whatever the size, have a natural origin (broken, cut by beaver) and 17% has been cut by humans. The large pieces of wood (diameter >12.5 cm) more frequently have a human origin (40%). Large pieces with roots are infrequent (10%) underlining the low contribution of bank erosion. Most of the pieces are strongly smoothed, without any branches, roots and bark confirming the effect of physical breakage of high energy rivers. Amongst 503 samples, 45% have a riparian origin (Populus, Fraxinus, Alnus). Copyright © 2003 John Wiley & Sons, Ltd.

[1]  M. Bryant The Role and Management of Woody Debris in West Coast Salmonid Nursery Streams , 1983 .

[2]  M. Harmon,et al.  Ecology of Coarse Woody Debris in Temperate Ecosystems , 1986 .

[3]  Dynamics of wood in large rivers , 2003 .

[4]  G. Minshall,et al.  The River Continuum Concept , 1980 .

[5]  F. Swanson,et al.  History, physical effects, and management implications of large organic debris in western Oregon streams. , 1976 .

[6]  B. Finlayson,et al.  Distribution and hydraulic significance of large woody debris in a lowland Australian river , 1996, Hydrobiologia.

[7]  F. Douglas Shields,et al.  Effects of large woody debris removal on physical characteristics of a sand-bed river , 1992 .

[8]  Richard M. Lehtinen,et al.  Autumn use of woody snags by fishes in backwater and channel border habitats of a large river , 1997, Environmental Biology of Fishes.

[9]  A. Lemly,et al.  Effects of large woody debris placement on stream channels and benthic macroinvertebrates , 1997 .

[10]  Val Crispin,et al.  Changes in Instream Habitat, Large Woody Debris, and Salmon Habitat after the Restructuring of a Coastal Oregon Stream , 1993 .

[11]  F. Swanson,et al.  EFFECTS OF LARGE ORGANIC MATERIAL ON CHANNEL FORM AND FLUVIAL PROCESSES , 1979 .

[12]  F. Triska Role of wood debris in modifying channel geomorphology and riparian areas of a large lowland river under pristine conditions: A historical case study: With 7 figures and 4 tables in the text , 1984 .

[13]  Chris Maser,et al.  From the Forest to the Sea: A Story of Fallen Trees , 1990 .

[14]  B. Kronvang,et al.  Re‐establishment of Danish streams: Restoration and maintenance measures , 1993 .

[15]  S. Darby,et al.  Fluvial maintenance operations in managed alluvial rivers , 1995 .

[16]  B. Finlayson,et al.  Hydraulic guidelines for the re-introduction and management of large woody debris in lowland rivers , 1996 .

[17]  A. Benke,et al.  Importance of Snag Habitat for Animal Production in Southeastern Streams , 1985 .

[18]  F. D. Shields,et al.  Environmental Aspects of Clearing and Snagging , 1984 .

[19]  M. L. Murphy,et al.  Large woody debris in forested streams in the Pacific Northwest: past , 1987 .

[20]  J. Peiry Approche géographique de la dynamique spatio-temporelle des sédiments d'un cours d'eau intra-montagnard : l'exemple de la plaine alluviale de l'Arve (Haute-Savoie) , 1988 .

[21]  J. Webster,et al.  Influence of log additions on physical and biotic characteristics of a mountain stream , 1995 .

[22]  Angela M. Gurnell,et al.  The role of coarse woody debris in forest aquatic habitats: Implications for management , 1995 .

[23]  M. Gordon Wolman,et al.  Fluvial Processes in Geomorphology , 1965 .

[24]  H. Piégay,et al.  DISTRIBUTION OF LARGE WOODY DEBRIS ALONG THE OUTER BEND OF MEANDERS IN THE AIN RIVER, FRANCE , 1998 .

[25]  Yoshiharu Ishikawa,et al.  DYNAMICS OF WOOD TRANSPORT IN STREAMS: A FLUME EXPERIMENT , 1997 .