摘要
The second part of this paper is devoted to the computational modelling of transient water migration in hardwood. During re-saturation, the moisture content, measured during the process by using X-ray attenuation (see part 1 of this paper), increases quickly very close to the cavity, but requires a very long time for the remaining part of the sample to absorb the moisture in wetting. For this configuration and this material, the macroscopic approach fails. Consequently, a dual-porosity approach is proposed. The computational domain uses a 2-D axisymmetric configuration for which the axial coordinate represents the macroscopic longitudinal direction of the sample whereas the radial coordinate allows the slow migration from each active vessel towards the fibre zone to be considered. The latter is a microscopic space variable. The moisture content field evolution depicts clearly the dual scale mechanisms:a very fast longitudinal migration in the vessel followed by a slow migration from the vessel towards the fibre zone.The macroscopic moisture content field resulting from this dual scale mechanism is in quite good agreement with the experimental data.
The second part of this paper is devoted to the computational modelling oftransient water migration in hardwood. During re-saturation, the moisture content, measured duringthe process by using X-ray attenuation (see part 1 of this paper), increases quickly very close tothe cavity, but requires a very long time for the remaining part of the sample to absorb themoisture in wetting. For this configuration and this material, the macroscopic approach fails.Consequently, a dual-porosity approach is proposed. The computational domain uses a 2-D axisymmetricconfiguration for which the axial coordinate represents the macroscopic longitudinal direction ofthe sample whereas the radial coordinate allows the slow migration from each active vessel towardsthe fibre zone to be considered. The latter is a microscopic space variable. The moisture contentfield evolution depicts clearly the dual scale mechanisms: a very fast longitudinal migration in thevessel followed by a slow migration from the vessel towards the fibre zone. The macroscopicmoisture content field resulting from this dual scale mechanism is in quite good agreement with theexperimental data.
