Simultaneous heat and moisture transport in building components. one- and two-dimensional calculation using simple parameters
Kščnzel, H.M
1995 Dissertation, Universit?t Stuttgart, 1994
Kščnzel, H.M, (1995), Simultaneous heat and moisture transport in building components. one- and two-dimensional calculation using simple parameters, Dissertation, Universit?t Stuttgart, 1994.
Abstract
Object of this study was the development of a method for the one and two-dimensional calculation of the simultaneous heat and moisture transport in building components, using simple parameters. For this purpose, we first examined closely the moisture storage and transport mechanisms and their effect on heat transport. We disregarded moisture movements based on air flows, gravitation, hydraulic pressure differentials as well as osmotic or electrokinetic effects.
Moisture storage in building components is divided into three regions. The first region is characterized by hygroscopic equilibrium water contents (sorption isotherms). In capillary-active materials, this is followed by the super-hygroscopic region with water contents up to free saturation. In this region, the equilibrium moisture depends on the capillary vacuum in the water-filled pores or the relative humidity over the pore water. This dependence, which can be determined with measuring techniques, forms the basis for supplementing the sorption isotherms for high water contents. This results in a steady storage function which can be defined throughout the entire moisture region of 0-100% relative humidity. Water contents above free saturation are characterized by a third region, in which there are no more equilibrium states. The building material is supersaturated, i.e. the relative humidity, regardless of the water content, is always 100%. Using results from the literature as well as our own findings, we analyze the significance of the temperature dependence and hysteresis of the moisture storage function for moisture storage calculations. For the determination of the moisture storage function, we provide a simple approximation which is sufficiently accurate in cases without liquid transport across layer boundaries. |
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