Quiz 4 Flashcards
Comfort for Occupants:
● Room temperature (also called dry-bulb temperature)
● Airflow (rate of air motion)
● Humidity or moisture content of the room
● Radiation or surface temperature of surrounding surfaces in the rooms
● Indoor air quality
Room temperature:
72 to 78 F (22.2C to 25.5C) in the winter.
In the summer: 72 - 76F (22.2 to 24.4C)
Humidity: moisture content
A high humidity (often occurring in the summer) will cause the surrounding
air to absorb less heat from the body, making the occupant feel warmer.
A low humidity (often occurring in the winter) allows the air to absorb
greater quantities of body heat, making the occupant feel cooler.
- To lower the summer humidity
- To increase the winter humidity
Airflow: rate of air motion
In the summer:
increased air motion increases the evaporation rate of heat
from the body to help keep it cool.
Buildings without air conditioners use fans to increase the
movement of the air on hot days.
In the winter:
a slower rate of air motion is desired, or the occupants will
feel cool due to evaporative heat loss.
Even in the winter it is desirable to have a flow of air to keep
the air from becoming stagnant.
When the air velocity is less than 10 feet per minutes the space is considered to
be stuffy.
Air velocities more than 50 feet per minute will seem drafty.
Radiation:
heat flows from a hot to a cold surface.
Windows and exterior walls will probably be cooler in the winter than
interior walls and the furniture.
The temperatures of the floors and ceilings will depend on the air
temperature on the other side of the construction.
Comfort can be increased (in the winter) by directing the flow of warm
air over the colder surfaces.
This is why most heating elements are located under a window.
HVAC: Heating, Ventilation, Air Conditioning
These systems are designed to provide
* Thermal conditions
* Adequate amounts of outdoor air
Absolute Humidity (humidity ratio, specific humidity, W):
Ratio of the mass of water vapor (mw) to the mass of dry
air (ma):
Types of air
Dry air: air that contains no water vapor.
Moist air: air that contains water vapor.
Saturated air: air that contains the maximum amount of moisture it can hold at that temperature.
Relative Humidity (RH):
Ratio of the actual water content to the maximum
amount of moisture it could hold at the same temperature
and pressure (when fully saturated).
It is expressed in percent.
Relative humidity is measured by an instrument called hydrometer.
Dew point (or saturation) temperature (DPT):
The temperature of the air/water-vapor mixture when it is fully saturated (100% relative humidity).
At this temperature moisture will begin to condense (water vapor from
the air begins to form water droplets on surfaces that are colder than the
dew point of the air).
Frost point temperature:
Dew point temperature below freezing. In this case, the water vapor creates frost instead of dew.
Effect of Temperature on Humidity
● The moisture holding capacity of the air depends on the air temperature.
● Warm air holds more moisture than cold air.
Dry bulb temperature (DBT)
The temperature of the mixture of air and moisture
at rest.
It is measured with a common thermometer.
Wet-bulb Temperature:
Temperature measured by a thermometer with a
wetted cloth sock covering its bulb as fast-moving air
passes across it.
Specific volume (v):
Ratio of unit volume of dry air per unit weight of dry air.
It is expressed in cubic feet of air per pound of dry air (ft3/lb)
or cubic meter of air per kilogram of dry air (m3/kg).
It is the inverse of density.