We use a simple experimental procedure of pressurized water absorption
to show the fractal nature of the pore space in wood. Cubic blocks of
wood were immersed in water at a given pressure for 14 days, and mass
changes were measured. The plots of the mass changes versus block edg
e sizes are straight lines whose slopes correspond to the fractal dime
nsions of the void volume in wood. Results for different species and f
or distinct water pressures are shown, suggesting the fractal dimensio
n as a new relevant parameter to characterize the porosity of wood.