Water Conservation@@t « wr w þ « g r v þ r bþr rw v w þ r v v g þ r b v b¼rðrg¼Deff rv v ÞðT1ÞEnergy Conservation@@t « wr w h w þ « g ðr v h v þ r a h a Þþr bhb þ r o h s « g P g þr rw h w v w þ ðr v h v þ r a h a Þv g þ h b r b v b¼¼r r gDeff ðh v rv v þ h a rv a Þþl eff rT þ FðT2ÞAir Conservation@@t « ¼gr a þr ra v g ¼r rgDeff rv a(T3)where the gas- and liquid-phase velocities are given by the generalized Darcy’s law:v ‘ ¼¼K ‘¼kr‘m ‘rw ‘ , rw ‘ ¼rP ‘ r ‘ grx (T4)where ‘ is w, g, the quantity w is known as the phase potential, and x is the depth scalar. All other symbolshave their usual meaning.Boundary ConditionsFor the external drying surfaces <strong>of</strong> the sample, the boundary conditions are assumed to be <strong>of</strong> the following form: 1 x 1J w j x¼0 þ ^n ¼ h m cM v ln1 x v j x¼0(T5)J e j x¼0 þ ^n ¼ h(Tj x¼0 T 1 )P g j x¼0 þ ¼ P atmwhere J w and J e represent the fluxes <strong>of</strong> total moisture and total enthalpy at the boundary, respectively, and xdenotes the normal position from the boundary in the external medium.<strong>36</strong>.2.3 PROCESS OF DRYING<strong>36</strong>.2.3 .1 Lo w-Temper ature Convecti ve Dry ingLow-temperature convective drying is the most widespreadindustrial process for seasoning wood in kilns.In this case, the role <strong>of</strong> internal gaseous pressure isalmost negligible and transfer occurs mainly in thedirection <strong>of</strong> the board thickness. Two periods <strong>of</strong> dryingmay be distinguished: (1) a constant drying-rateperiod and (2) a decreasing drying-rate period.<strong>36</strong>.2.3 .1.1 The Cons tant <strong>Drying</strong>- Rate Peri odThis stage is very common for certain porous media,but is rarely seen with wood. However, it exists almostalways for fresh boards consisting <strong>of</strong> sapwoodthat are dried under moderate conditions (Perré et al.,1993; Perré and Martin, 1994). During this period,the exposed surface <strong>of</strong> the board is still above theFSP. As a result, the vapor pressure at the surface isequal to the saturated vapor pressure, and is a function<strong>of</strong> the surface temperature only.Coupled heat and vapor transfer occur across inthe boundary layer (Figure <strong>36</strong>.17). The heat flux suppliedby the airflow is used solely for transforming theliquid water into vapor. During this stage, the dryingrate is constant and depends only on the externalconditions (temperature, relative humidity, velocity,and flow configuration). The temperature at the surfaceis equal to the wet-bulb temperature. Moreover,because no energy transfer occurs within the mediumduring this period, the whole temperature <strong>of</strong> theboard remains at the wet-bulb temperature.ß 2006 by Taylor & Francis Group, LLC.
Boundary layersExternal flowTP vHeatVaporCapillary migrationLow moisturecontent=small radiusLiquid flow<strong>Wood</strong>High moisturecontent=large radiusFIGURE <strong>36</strong>.17 Constant drying-rate period: the moisture migrates inside the medium mostly by capillary forces; evaporationoccurs at the exchange surface with a dynamical equilibrium within the boundary layers between the heat and the vaporflows. (Adapted from Perré, P., The numerical modeling <strong>of</strong> physical and mechanical phenomena involved in wood drying: anexcellent tool for assisting with the study <strong>of</strong> new processes, Tutorial, Proceedings <strong>of</strong> the Fifth International IUFRO <strong>Wood</strong><strong>Drying</strong> Conference, Québec, Canada, 1996, 9–38.)The exposed surface is supplied with liquid watercoming from the inside <strong>of</strong> the board by capillaryaction; the liquid migrates from regions with highmoisture content (liquid–gas interfaces within largepores) toward regions with low moisture content(liquid–gas interfaces within small pores).The constant drying-rate period lasts as long as thesurface is supplied with liquid. Its duration dependsstrongly on the drying conditions (magnitude <strong>of</strong> theexternal flux) and on the medium properties. The liquidflow inside the medium is expressed by Darcy’slaw (permeability gradient <strong>of</strong> liquid pressure).<strong>36</strong>.2.3 .1.2 The Decr easing <strong>Drying</strong>- Rate Pe riodOnce the surface attained the hygroscopic range,the vapor pressure becomes smaller than the saturatedvapor pressure (Figure <strong>36</strong>.18). Consequently, theexternal vapor flux is reduced and the heat flux suppliedto the medium is temporarily greater than whatis necessary for liquid evaporation. The energy inexcess is used to heat the board, the surface at firstand then the inner part by conduction. A new, moresubtle, dynamic equilibrium takes place. The surfacevaporpressure,hencetheexternalvaporflow,dependson both temperature and moisture content. To maintainthe energy balance, the surface temperature increasesas the surface moisture content decreases. Thisleads to a decreasing drying rate (the heat supplied bythe airflow becomes smaller and smaller).A two-zone process develops inside the wood: (1)an inner zone, where liquid migration prevails, and(2) a surface zone, where both bound-water andwater-vapor diffusion take place. During this period,a conductive heat flux must exist inside the board toincrease the temperature and to evaporate the liquiddriven by gaseous diffusion. The region <strong>of</strong> liquidmigration naturally reduces as the drying progressesand finally disappears. The process is finished whenthe temperature and the moisture content attain theoutside air temperature and the EMC, respectively.<strong>36</strong>.2.3 .2 Dry ing at High Temper ature: The Effect<strong>of</strong> Inter nal Pressur e on Mass Tr ansferTo reduce the drying time without decreasing thequality <strong>of</strong> the dried product, the drying conditionsmust be such that the temperature <strong>of</strong> the product isabove the boiling point <strong>of</strong> water. Such conditionsensure that an overpressure exists within the material,which implies that a pressure gradient drives themoisture (liquid or vapor) toward the exchange surfaces(Lowery, 1979; Kamke and Casey, 1988).At normal atmospheric pressure, the boiling point<strong>of</strong> water equals 1008C. Consequently, in order toß 2006 by Taylor & Francis Group, LLC.