Advanced Building Simulation
Advanced Building Simulation
Advanced Building Simulation
Create successful ePaper yourself
Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.
38 de Wit<br />
AIR TEMPERATURE STRATIFICATION<br />
In the mainstream building simulation approach, it is assumed that the air temperature<br />
in building spaces is uniform. This will generally not be the case, however. In naturally<br />
ventilated buildings there is limited control over either ventilation rates or convective<br />
internal heat loads. This results in flow regimes varying from predominantly<br />
forced convection to fully buoyancy-driven flow. In the case of buoyancy-driven flow,<br />
plumes from both heat sources and warm walls rise in the relatively cool ambient air,<br />
entraining air from their environment in the process, and creating a stratified temperature<br />
profile. Cold plumes from heat sinks and cool walls may contribute to this<br />
stratification. Forced convection flow elements, like jets, may either enhance the<br />
stratification effect or reduce it, depending on their location, direction, air stream<br />
temperature, and momentum flow.<br />
As in the case of the wind pressure coefficients, the simplified modeling approach<br />
of the air temperature distribution in mainstream simulation introduces modeling<br />
uncertainty. There is a difference however. Whereas the effect of the airflow around<br />
the building on the ventilation flows is reduced to an empirical model with a few<br />
coefficients, the effect of temperature stratification in a building space on heat flows<br />
and occupant satisfaction is completely ignored. To be able to account for thermal<br />
stratification and the uncertainty in its magnitude and effects, we will first have to<br />
model it.<br />
If we consider the current approach as a zero-order approximation of the spatial<br />
temperature distribution, then it is a logical step to refine the model by incorporating<br />
first-order terms. As vertical temperature gradients in a space are commonly dominant,<br />
we will use the following model:<br />
T air(z) � T air � �(z � H/2)<br />
(2.3)<br />
where Tair is the air temperature; Tair,<br />
the mean air temperature; z, the height above<br />
the floor; H, the ceiling height of the space; and �, the stratification parameter.<br />
Dropping the assumption of uniform air temperature has the following consequences:<br />
● the temperature of the outgoing air is no longer equal to the mean air temperature<br />
as the ventilation openings in the spaces are close to the ceiling;<br />
● the (mean) temperature differences over the air boundary layers at the ceiling and<br />
floor, driving the convective heat exchange between the air and those wall components,<br />
are no longer equal to the difference between the surface temperature<br />
and the mean air temperature;<br />
● the occupants, who are assumed to be sitting while doing their office work, are<br />
residing in the lower half of the space and hence experience an air temperature<br />
that is different from the mean air temperature.<br />
With Equation (2.3) we can quantify these changes and modify the simulation model<br />
to account for them. In most commercially available simulation environments this is<br />
not feasible, but in the open simulation toolkit BFEP this can be done.<br />
In the analysis we will assume that � in Equation (2.3) is a fixed, but uncertain<br />
parameter. This means that we randomize over a wide variety of flow conditions in<br />
the space that may occur over the simulated period. In, for examples, Loomans