In this paper, the theory and method for investigating the permeability of
wood and basalt particle aggregates, were developed. It was found that if t
he air flow velocity over the characteristic length of the particle bed was
less than 3 m/s, there existed a linear relationship between the air flow
rate and the pressure gradient. Under this circumstance, Darcy's law was va
lid for describing the fluid flow process in particle aggregates. The perme
ability of different wood chips of linden, poplar, birch and elm was experi
mentally tested with respect to a number of factors like tree species, part
icle size distribution, porosity, moisture content and bulk density. The st
udy showed that the permeability of wood particle aggregates was influenced
by tree species having great effects on particle size distribution and, in
turn, on porosity, and that increased with the increasing of the mean part
icle size of wood chips. Also the permeability of different basalt particle
size distribution and porosity were measured.