Volume 9,
Issue 1, 2000
Interfacial
Pathways in Wood
Caroline
Baillie*, Delphine Tual and Jean Christophe
Terraillon
Dept. Materials, Imperial College of Science, Technology
and Medicine, Prince Consort Rd., London SW72BP
(Received 12/99; accepted 2/00)
*Author to whom correspondence should be addressed)
Abstract
Wood structure and properties have been established for
many years. The interaction of structure with properties has also been studied, but rarely
from a materials science perspective. This paper attempts to focus on a particular aspect
of composite structure, that of the interface. In engineered fibre composites the
interface is the most important feature as it is the medium by which the stress is
transferred from the matrix to the fibres so that they may bear the load. Much research
has been focused on solving the optimisation of the interfacial stress transfer, as it is
always suggested that the interface needs to be weak for high toughness and strong for
high strength of the composite. More recent studies have identified the fact that it may
be more advantageous to create an interface, which is not destructive in its energy
absorbing capacity. Another area of weakness at the interface is the resistance to water
ingress in certain environmental conditions.
Biomimetics is an emerging approach to solving scientific issues by
looking to nature to see what solutions are offered for the particular concerns of
engineers and their products. In this case wood is the subject of study. It is assumed
that wood has optimised its internal interfaces to cope with strength and toughness
requirements as well as harsh environmental conditions. The internal interfaces thus need
to be firstly examined and identified. This paper looks in a qualitative way at the three
different interfacial crack paths which may be likened to those occurring in engineered
composites: interfacial, interlaminar and intercellular (bundle/bundle interaction) and
their proposed relation to energy absorption mechanisms, It also explores the influence of
moisture on these fracture paths.