A theoretical investigation of moisture movement in pine sapwood was undertaken using two different models of behaviour. Firstly a model was developed using a single diffusion process; this model predicted levels of water absorption and moisture content which were in broad agreement with experimental results. However, this approach proved to be over-simplistic, and predicted a more rapid penetration of moisture than was observed in practice. The model also failed to predict the deceleration in absorption which was recorded in laboratory tests. Consequently, the predictions of the model were of a more uniform moisture distribution than was consistent with experience. A development of the model, to include flow mechanisms appropriate for the level of moisture content, gave more realistic predictions. The improved model is based on different flow mechanisms in three distinct regions of moisture content. Below fibre saturation point (FSP), a diffusion mechanism is assumed for the calculation of moisture flow. Between FSP and a threshold, termed the irreducible saturation point (ISP), flow takes place through the cell wall material. Above the ISP, a continuous path is established for moisture movement from cell to cell through the bordered pits. The improved model proved capable of predicting levels of moisture uptake and moisture content, and of predicting the moisture gradients observed in practice. It also provided an explanation of some of the observed patterns of wood moisture movement reported in earlier parts of this series of papers. In particular it explained why, when water is absorbed by coated timber, the rise in surface moisture content appears not to exceed FSP. Additionally it provided an understanding of the continuing penetration of moisture in depth during the early stages of drying. This is a significant conclusion, because it imposes a limitation, in principle, on the performance of high permeability wood coatings.
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