The natural ventilation of a room, both with a heated floor and connected t
o a cold exterior through two openings, is investigated by combining quanti
tative models with analogue laboratory experiments. The heated floor genera
tes an areal source of buoyancy while the openings allow displacement venti
lation to operate. When combined, these produce a steady state in which the
air in the room is well-mixed, and the heat provided by the floor equals t
he heat lost by displacement. We develop a quantitative model describing th
is process, in which the advective heat transfer through the openings is ba
lanced with the heat flux supplied at the floor. This model is successfully
tested with observations from small-scale analogue laboratory experiments.
We compare our results with the steady-state flow associated with a point
source of buoyancy: for a given applied heat flux, an areal source produces
heated air of lower temperature but a greater volume flux of air circulate
s through the room. We generalize the model to account for the effects of (
i) a cooled roof as well as a heated floor, and (ii) an external wind or te
mperature gradient. In the former case, the direction of the flow through t
he openings depends on the temperature of the exterior air relative to an a
veraged roof and floor temperature. In the latter case, the flow is either
buoyancy dominated or wind dominated depending on the strength of the press
ure associated with the wind. Furthermore, there is an intermediate multipl
e-solution regime in which either flow regime may develop.