1968
DOI: 10.1007/bf00829695
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The propagation of radiation in capillary-porous colloidal bodies

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1969
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“…'l'hcn if a body coiiics to equilibrium with the reference body when the latter has a nioisture content u, thc iiiass transfer potential 0 is calculated as (12) 111 this case, we can rewrite the isothermal part of Equation (6) as ---u,pu v 2 1 = -u, Po ("3 VO =k,\JO.. (13) ae where (:!) I t is known from experiments that even in the absence of temperature acd pressure gradients, moisture can be transferred from one porous material of low moisture content u to one of higher moisture content if the properties of the two porous materials are sclected suitably.…”
Section: 3 J 4 ) mentioning
confidence: 99%
“…'l'hcn if a body coiiics to equilibrium with the reference body when the latter has a nioisture content u, thc iiiass transfer potential 0 is calculated as (12) 111 this case, we can rewrite the isothermal part of Equation (6) as ---u,pu v 2 1 = -u, Po ("3 VO =k,\JO.. (13) ae where (:!) I t is known from experiments that even in the absence of temperature acd pressure gradients, moisture can be transferred from one porous material of low moisture content u to one of higher moisture content if the properties of the two porous materials are sclected suitably.…”
Section: 3 J 4 ) mentioning
confidence: 99%