2503
River Flow 2014 – Schleiss et al. (Eds)
© 2014 Taylor & Francis Group, London, ISBN 978-1-138-02674-2
Wood density assessment to improve understanding of large wood
buoyancy in rivers
Virginia Ruiz-Villanueva & Markus Stoffel
Dendrolab.ch, Institute of Geological Sciences, University of Bern, Switzerland
Institute for Environmental Sciences, University of Geneva, Switzerland
Hervé Piégay, Vincent Gaertner & Franck Perret
National Center for Scientific Research (CNRS), UMR 5600 EVS/Site ENS de Lyon, France
ABSTRACT: Drift wood (or in-stream large wood, LW) plays an important role in river ecosystems
by influencing hydrodynamics and morphology. Wood density, therefore, buoyancy, is the main factor
conditioning initial motion of wood in rivers. The better understanding of wood density and the dry-wet
process and decay, may be useful to improve the knowledge of wood dynamics in rivers. We analyze wood
pieces retained in a dam, in the French Rhone, and a set of freshly cut riparian trees. Different protocols
were set to measure density and buoyancy of these two series of wood and to test effects of drying and
wetting, species and wood decay stages. Preliminary results after seven months of experiments show dif-
ferent behaviors in density and buoyancy depending on species. Light wood (360–500 kg m
3
) is likely to
show a buoyancy rate about 52% (half of the log emerged), medium density wood (500–700 kg m
3
) about
39%, 21% for dense wood (700–900 kg m
3
) and 12% for very dense wood (900 kg m
3
). We observed
a significant negative correlation between wood density and buoyancy and proposed a model to predict
wood buoyancy. The results from this work will help to understand the evolution of buoyancy through
time and estimate local conditions of entrainment and transport of wood in rivers.
varies greatly among tree species, but it also varies
for each of the species according to water content
and degree of decay.
Therefore, the time during which wood pieces are
wetting or drying can affect their dynamics when
they enter the river. The final goal of this work is to
improve our understanding of wood buoyancy in
rivers throughout the assessment of wood density
for different types of wood and decay stages and to
find a model to predict wood buoyancy.
2 STUDY SITE AND METHODOLOGY
2.1 Sampling
The characteristics of the wood are assessed using
two series of wood pieces, one extracted from a
reservoir (decayed floating wood) and another
from living trees used as a reference (green or fresh
wood). The decayed wood analyzed was collected
from wood pieces retained in the Génissiat reser-
voir, French Rhone (watershed area of 10,910 km
2
at Génissiat). This gravity dam has no overflow
pathway so that all wood coming from two main
tributaries, the Arve and Valserine Rivers, is
blocked by the dam, even during floods, and must
be extracted mechanically (Fig. 1).
1 INTRODUCTION
In-stream Large Wood (LW) plays an important
role in river ecosystems by influencing hydrology,
hydraulics, sedimentology, and morphology
(Montgomery, 2003). An extensive literature now
exists describing the influence of wood on stream
ecology (Gregory et al., 2003; Kasprak et al., 2011),
and more recently on stream geomorphology
(Gurnell, 2012; Wohl, 2013). Recent research has
focused on the mobilization of woody material
during floods (Comiti et al., 2012), as transported
woody material can cause a substantial increase in
the destructive power of floods (Ruiz-Villanueva
et al., 2012).
Various characteristics of a piece of wood affect
its likelihood of movement (e.g., wood density,
buoyancy, orientation, size, and form related to flow
depth, velocity, and roughness; Le Lay et al., 2013).
In this study, we analyze wood buoyancy to
determine whether floating or sinking of wood
pieces through the water column has a funda-
mental impact on river dynamics. Buoyancy typi-
cally varies with tree species and decay rates. So,
the most important property affecting river wood
mobility and particularly the capacity of LW to
float in freshwater is wood density. Wood density