Sensible Heat: Heat that causes a change in temperature, measurable by a thermometer.
Latent Heat: Heat energy absorbed or released during a change in the state of matter, without changing temperature.
Heat Fusion: Heat required to change a solid into a liquid.
Heat of Vaporization: Heat needed to transform liquid into gas.
Enthalpy: Total heat content of a system.
Radiant Heat: Heat energy transferred as electromagnetic radiation, like infrared waves; does not require a medium and can transfer through a vacuum.
Heat transfer from one particle to another in direct contact.
Fluids expand, become less dense, and rise, depending on gravity.
Heat transferred by electromagnetic waves emanating from warm bodies, carrying energy to bodies in direct line of sight.
Transmittance: Radiation passing through materials (ceilings, walls).
Absorptance: Radiation converted into sensible heat within a material.
Reflectance: Radiation reflected off the surface.
Emittance: Radiation given off by the surface, reducing sensible heat.
Infiltration: Cold air enters through construction joints (cracks around doors and windows).
Blower Door Test: Measures building tightness.
Ventilation: Controlled and purposeful infiltration of air.
Evaporative Cooling: Heat from vaporization cools the environment.
Greenhouse Effect: Shortwave solar radiation passes through glass and is absorbed by indoor objects.
Stratification: Separation of cooler and warmer layers of fluid/air as warm air rises.
Mean Radiant Temperature: Environmental factor in human comfort.
Balance between absorptance and emittance.
Movement of heat from one body to another.
Heat Capacity: Amount of heat required to raise temperature.
Thermal Resistance: Opposition to heat flow by conduction, convection, and radiation.
Heat-flow Coefficient (U): Measure of heat flow; reciprocal of thermal resistance.
Time Lag: Delay in heat flow phenomenon.
The temperature at which air is fully saturated and can hold no more moisture.
Altitude: Sun’s angle in the vertical plane.
Azimuth: Sun’s angle in the horizontal plane.
Sky Vault: Imaginary dome indicating the sun's path.
Solar Window: Portion of the sky vault most beneficial for sunlight, typically from 9 AM to 3 PM.
Reflected Light: Light reflected from surfaces.
Passive Solar: System collecting, storing, and redistributing solar energy without mechanical systems.
Bernoulli Effect: Velocity of fluid increases, static pressure decreases, creating negative pressure in venturi tubes.
Stack Effect: Expels air from buildings through natural convection.
Various methods of cooling through ventilation, such as Day and Night cooling strategies.
Sensible vs. Latent Heat: Sensible heat raises temperature; latent heat causes phase changes without temperature change.
Heating Water Example: Heating 1 lb of water requires 1 BTU to raise by 1 °F. Latent heat required to change states (144 BTU for ice to water, 1000 BTU for water to steam).
Energy Calculations for Ice and Water:
To melt 2 lbs of ice: 2 lbs × 144 BTU/lb = 288 BTU.
To heat 2 lbs of water from 32°F to 122°F: 2 lbs × 1 BTU/lb°F × 90°F = 180 BTU.
Total energy for both processes: 288 BTU + 180 BTU = 468 BTU.
All objects absorb and emit radiation with net flow from warm to cool.
Different materials affect thermal properties:
White: Low solar absorptance; high emittance.
Black: High absorptance; high emittance.
Shiny Metal: Low absorptance; low emittance.
Wet-Bulb Temperature: Shows variation between dry and humid air.
Climate Zones: Tropical, Temperate, Arctic, affecting design priorities for buildings.
ASHRAE factors: temperature, relative humidity, air motion affect thermal comfort.
Region 15 (Houston): Keep heat out, allow ventilation, summer sun protection.
Region 14 (New Orleans): Natural ventilation for cooling and moisture removal.
Region 9 (Arkansas): Keep heat in during winter, ventilation for summer cooling.
Vapor barriers' placement varies by climate (warm exterior, cool interior).
Sun's position (23.5 degrees tilted) affects seasonal light availability.
Summer Solstice: 24 hours light above the Arctic Circle.
Winter Solstice: 24 hours darkness above the Arctic Circle.
Occurs March and September; Sun is above the equator.
Noon solar altitude calculation: A = 90 - L (L being latitude). For Lafayette (30°), A = 60°.
Ground is the dominant light source on sunny days; overcast skies change dynamics.
Cloud Cover Dynamics: Varies intensity from zenith to horizon.
Increase distance from task areas to ceilings to improve light distribution.
Side lighting effectiveness is affected by height placement of windows.
Direct Gain: Collects solar energy during the day for nighttime use.
Trombe Walls: Store and vent heat to interior.
Sun Spaces: Collect solar energy while sealing at night to retain heat.
Wind Towers: Direct air into buildings; historical structures (Chickees, Trulli).
Airflow Principles: Air takes straight routes, conservation of air is key in design considerations.
Cross-Ventilation: Air enters windows set with respect to wind direction; effectively ventilated spaces.
Effective building design requires understanding of thermal mass, shading, and solar exposure.
Use of well-placed windows and ventilation strategies enhances energy efficiency and occupant comfort.