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Research
note
Air movements in an indoor space may be
experienced in very different ways. For persons feeling cool, air movements
tend to be perceived as draught, whilst feeling warm air movements may provide
a desired cooling effect. In the transition zone it therefore seems difficult
to use constant air velocity as a tool for cooling without creating draught.
One possible way is to use intermittent air velocity instead of constant
velocity. Intermittent air velocity, or velocity variations (Table 1),
consists of high velocity pulses, strong enough to offer occupants the desired
cooling effect but with a limited duration, in order to avoid draught. This new
method was implemented in a high school in Sweden. One classroom where equipped
with a ventilation system which could produce velocity variations in the
occupied zone. This was realized by letting the supply air enter the room
either through high velocity terminals (Figure 1) placed
in four rows straight above the occupants, or through standard low velocity
diffusers. During the high velocity period the ventilation system produced a downward air jet with a mean
speed of 0.4 m/s, measured straight below the terminals at head level of a
sitting person.
Figure 1. High velocity terminals installed in a class room.
The intermittent velocity changes or
velocity profile, periods of high respectively low velocity (Table 1),
were controlled by the room temperature. Two classrooms, which were placed beside each other and considered as
having approximately identical climate conditions beside the velocity, were
used to collect data. Evaluation was done during spring (April) and
autumn (September). The analysis did show significant effects of velocity
condition on thermal comfort and air quality. People exposed to velocity
variation perceived the air as cooler and fresher compared with those exposed
to constant low velocity and very few classified the air movement as draught. A
further conclusion is that even the pupils who were exposed to velocity
variation wanted slightly more air movements.
Table 1. Intermittent velocity profiles at different room temperatures. H 5 and L 15 correspond to five minutes of high velocity followed by 15 minutes of low velocity, which will be repeated as long as the temperature remain unchanged.
Temperature [°C] | Velocity profile [min] |
below 22 | Constant low velocity |
22-23 | H 5 L 20 |
23-24 | H 5 L 15 |
24-25 | H 5 L 10 |
25-26 | H 5 L 8 |
26-27 | H 5 L 6 |
27-28 | H 5 L 4 |
above 28 | Constant high velocity |
This Research note is based on the paper submitted to International Journal of Ventilation. |
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