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Black Body
Absorbs all SW and LW
High emissivity - Emits max LW (can emit SW)
Low solar reflectivity (albedo)
High heat gain
High heat loss
Examples:
Dark asphalt
Sand
Roofing tar/gravel
Black paint
White Body
Absorb zero SW and LW
Emit zero LW (Zero Emissivity)
Reflects SW and LW
Low heat loss
Low heat gain
Examples:
Polish aluminum foil
Low-e suspended coated polymer film
Perfect Dissipater
Absorbs zero SW
Emits max LW
High heat loss
High solar reflectivity
Examples:
white plaster/paint
Perfect Collector
Absorbs all SW
Emits zero LW
High heat gain
Low Heat loss
Examples:
Spectrally selective black coating
Solar reflectivity
Albedo
reflection of shortwave radiation
how much incoming solar energy, or light, is immediately reflected back to space
LW Emissivity vs LW Reflectivity
LW Emissivity:
a material's ability to emit infrared radiation within the longwave spectrum
how well it radiates heat
high emissivity means the material readily releases heat
only LW
LW Reflectivity:
how much of that longwave infrared radiation a material reflects back
high reflectivity means it bounces back most of the incoming longwave radiation
latent heat
energy transferred through a change in state
sensory heat
thermal mass
object property
the ability of a material to absorb, store, and release heat
depends on both the material's properties (like density and specific heat capacity) and the size and volume of the object or system.
relationship between absorption (α), transmission (T), and reflectivity (ρ)
100% incident radiation = radiation absorbed (a) + radiation transmitted (T) + radiation reflected (p)
radiation transmitted = the fraction of radiation that passes through the material (important for transparent materials).
In opaque materials, T = 0, so:
100% incident radiation =absorbed (α)+reflected (ρ)
balance point temp
outdoor temp at which heat losses from the building exactly match internal gains
the temp below which the furnace turns on
in BPT, heat gain = heat loss (steady state)
If outdoor temp < BPT, heat loss (Temp inside drops)
A lower BPT is achieved by:
high internal gains to match higher heat loss due to cold outdoor temp
well-insulated thermal envelope to retain more indoor heat
“__ivity”
property of a material (independent of amount)
2 dimensional
“__ance”
property of an object (depends on amount)
1 dimensional
conductivity
symbol: k
describes how well a material conducts heat
It is a measure of the ability of a material to transfer heat from the hotter side to the cooler side when there is a temperature difference.
conductance
symbol - C
Thermal conductance refers to the ability of an object or material to conduct heat.
property of the object as a whole, not the material itself
depends on:
thermal conductivity of the material
the size (area) and thickness of the object
specific heat capacity
material property
the amount of heat energy required to raise the temperature of a substance by one degree Celsius (°C) per unit mass
If a material has low specific heat capacity, it means that the material requires less energy to raise its temperature by a certain amount. In other words, it heats up or cools down faster when energy is added or removed.
volumetric heat capacity
object property
dependent on volume of thing
the amount of heat energy needed to raise the temperature of a unit volume of a substance by one degree
thermal mass functions
stores energy
moderates indoor temp fluctuations
reduces heat flow through envelope
reduces and shifts peak heating loads
thermal mass applications
passive solar heating
passive cooling (night flush)
commercial buildings
passive (structural mass)
active (ice storage, radiant systems)
Thermal mass needs
outdoor temp swings on both sides of comfort zone (dry climates better)
to be exposed to the indoor air (insulate from exterior)
to be well-distributed
cycle continuously
When thermal mass doesn’t work
humid climates, small diurnal temp swing
cold climates with overcast skies (little solar gain)
too much mass not connected to interior
intermittent occupancy or need for fast response time
direct-gain passive solar system
south facing windows (building positioning)
overhang prevents summer solar gain
insulation on our outside of envelope (keeps heat in)
thermal mass on inside stabilizes temp fluctuations
nighttime insulation on glass
indirect-gain passive solar system
sunspace/attached greenhouse
vents open in day maximizing heat gains, vents close at night to prevent heat loss
trombe wall
absorbing wall collects/stores heat energy
natural convection circulates heat
power
energy/time
rate of energy transferred
ACH
air changes per hour (room volumes/hour)
the number of times the air within a defined space is replaced with outdoor air in one hour
thermal bridging
a break in the thermal envelope through which heat can easily transfer (thin-cross section)
example:
slab, beam, etc
cons:
can make moisture control an issue “ghosting” “fogging”
sensible heat
temp change
thermometer
convection
transfer of heat between surface and fluid
induced by temperature differential
forced convection:
when fluid motion is caused by differences in temperature
hot air rising
forced convection:
mechanical force (like a fan, pump, or blower) is used to move the fluid
mechanically increase rate of heat transfer
radiation
energy transferred by electromagnetic waves across a transparent medium
solar radiation:
shortwave
uv, visible light, near infrared
terrestrial radiation
longwave
energy radiated from essentially every surface
Series heat flows
sum the resistance of the different layers heat must move through
parallel heat flows
sum the different “conductive” paths of series heat flow
more than one path
the perfect wall
rain control layer
air control layer
vapor control layer
thermal control layer
institutional wall
long-lasting
insulation adapted to climate
hella layers (drainage, insulation, vapor barrier, concrete, etc)
clever wall
like institutional wall but has all-in-one layer with all control layers
bad for environment
commercial wall
uninsulated steel stud cavity
slab-on-grade
a shallow concrete slab that rests directly on the ground
common in warmer climates
interrupt the flow of heat
vapor barrier location
cold, dry air
inside
warm and humid climates
outside