Hi Don Perhaps I am reading this wrong... but... it looks preeeettty much to me like the time it takes for wood to come to equilibrium with a change in climate is dependant on L² / D... which is explained directly below in a snip taken from the web site. Doesnt look like there is any provision in this formula for anything that would allow for wood to give off moisture at any different rate then it takes it on. If someone can explain otherwise then great.... but it looks like Ron N was not only right about not being able to find any support for the different rates idea... but that there is direct support for his claim that the idea is mistaken. Cheers RicB ........................ "At MC lower than the fiber saturation point (usually 35%), moisture change takes place by diffusion within the wood. The standard diffusion equation may be written as t = L² / D where D = 1x10-6 cm²/s transverse and radial, 1x10-5 cm²/s lengthwise, L is the length along the direction of diffusion. t is the time to 1/e of the moisture change, that is to 63% of the equilibrium change. So, if you have a piece of seasoned wood 2 cm thick that is at the 15% MC of typical outdoors storage here, and you want to estimate how fast it will come to equilibrium in your workshop at 30% RH (7% MC) if exposed to air both sides, L = 1 cm and the diffusion equation gives t = 1x106 s, 11 days. The equilibrium MC change required is 8%, so in 11 days you can expect 63% of 8% = 5% lower MC, that is 10% total MC. That leaves 3% to go, and you can expect 63% of that 3% to take place over the next 11 days, to 8% MC. So, 3 weeks should be enough time for 2 cm thick wood. If your wood is 4 cm thick, it will take 3 months, 6 cm thick, 7 months. According to the literature, most seasoned temperate woods change moisture at a rate within ±20% of this. "
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