Title: Movement of Thermal Energy: Heat Flow
1Heat/Energy Transfer
- Movement of Thermal Energy Heat Flow
- Three methods
- Conduction
- Convection
- Radiant
- Most heat transfer has some combination of all
three occurring at the same time
2Three Types of Heat Transfer
3Definitions
- Conduction
- A method by which heat is transferred from a
warmer substance to a cooler substance by
molecular collisions. Direct contact. - Convection
- The transfer of thermal energy from a fluid
flowing over a solid object- Air is a fluid! - Radiation
- A method by which heat can be transferred
through objects and empty space. Electromagnetic.
4 5Conduction Examples
- Liquid - Liquid - Pouring cold cream into coffee
- Liquid - Gas - Ocean and Atmosphere
- Gas - Gas Cold and warm weather systems mixing
- Solid - Solid Touch a hot pot on a stove
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7Conduction Rate Factors
- Contact Area
- Type of Material i.e. Cast Iron vs. Stainless
Steel - Temperature Difference
- Distance heat must travel
8 9Convection
- The transfer of thermal energy from a fluid
flowing over a solid object- Air is a fluid! - But, air is a relatively poor conductor of heat
- A solid object dense arrangement of molecules
- Liquid less dense arrangement
- Gas least dense arrangement of molecules
- Transferring heat using a gas is inefficient
- Must pass a lot of molecules over an object to
equal the carrying capacity of a denser material.
10Convection Examples
- In a closed room cool air will settle to the
bottom while warm air will rise - Warm air rising through a heat register
11Convection Examples
- Bowl of soup Hot liquid in the center moves to
the cooler outside where it drops and is reheated
at the center and the cycle continues.
12CONVECTION
- What is required of convection to occur
- Air Flow Pressure Difference Path (Hole)
13The Stack Effect
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15Convection
Temperature is typically the dominant effect
16 17Radiation
- A method by which heat can be transferred through
objects and empty space. Electromagnetic. - The transfer of thermal energy or heat that is in
direct line of sight of the object being heated.
18Radiation Examples
- The suns heat
- A bonfire
- Warm soil on a cool night
19Radiation Rate Factors
- Surface area
- Temperature difference
- Type of material
- Emittance
- Reflectivity
20Radiation Terms
- Emittance (or emissivity), refers to the ability
of a materials surface to give off radiant
energy. All materials have emissivities ranging
from zero to one. The lower the emittance of a
material, the lower the heat radiated from its
surface.
21Radiation Terms
- Reflectance (or reflectivity) refers to the
fraction of incoming radiant energy that is
reflected from the surface. Reflectivity and
emissivity are related and effect each other
inversely. - For example, aluminum with a reflectance of 0.97
has an emittance of 0.03
22Emissivity or Emittance
Material Surface Emittance
Asphalt 0.90 - 0.98
Aluminum foil 0.03 0.05
Brick 0.93
Fiberglass 0.80 0.90
Glass 0.95
Steel 0.12
Wood 0.90
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24HUMAN COMFORT
25Human Comfort Zone
- As humans we try to maintain a body
- temperature of 98.6 F
- Three Mechanisms
- Heat generated within the body
- Heat gained from surroundings
- Heat lost to surroundings
26Human Comfort Zone
- We shiver to
- generate heat
27Human Comfort Zone
- We sweat to
- Give off heat
28Human Comfort Zone
29Human Comfort Zone
- Blood Flow
- Decreases to hands and feet in winter
- Increase in summer to encourage heat loss
30Thermal Neutrality
- To be comfortable humans must loose heat at the
same rate as it is produced or gained.
31Factors Affecting Human Comfort
- Air temperature
- Air Speed
- Humidity
- Mean radiant temperature
- Each has a direct influence on heat loss or gain
to the human body
32Factors Affecting Human Comfort
- Air Temperature - This affects temperature
differences between the body and the
surroundings, consequently affecting the rate of
heat loss or gain by convection.
33Factors Affecting Human Comfort
- Air Speed - This affects the rate at which
- the body loses heat by convection.
- An air temperature of 35F and a wind speed of 20
miles/hour combine to give a wind chill
temperature of 11.2F. - Air speed is also very important during summer
when the body is trying to lose heat to maintain
comfort.
34Factors Affecting Human Comfort
- Humidity - Affects the rate at which the
- body loses heat by evaporation. During hot
- weather, high humidity increases discomfort
- by making it more difficult to evaporate
- perspiration into the air.
35The Chill Factor
- The Chill Factor can be a direct cause of
discomfort - A lesser noticed effect of unbalanced forced air
systems is inducing increased infiltration - Due to pressure imbalances and duct leaks
- Heating the air in a room does a relatively poor
job of heating solid objects - Those objects in the room at a temperature lower
than ones body act to rob the body of heat
(through radiation), requiring higher room
temperatures to offset that effect
36Factors Affecting Human Comfort
- Mean Radiant Temperature (MRT) - MRT is the
average surface temperature of the surroundings
with which the body can exchange heat by radiant
transfer. - Radiant heat transfer to and from the body is
quite apparent when sitting near a fireplace
(high MRT) or large cold window area (low MRT).
37Mean Radiant Temperature
38Cold Surfaces
39Comfort
- Comfort is achieved by either increasing the
ambient temperature or by raising the mean
radiant temperature of an environment. - A higher radiant temperature means that people
become comfortable with a lower ambient
temperature and the reverse is also true.
40Mean Radiant Temperature
- In general for every 1 degree F that MRT drops,
the air temperature must be raised about 1.4
degrees F to achieve comfort conditions. - How can you raise the MRT?
- Close blinds and curtains
- Solar Film on windows
- Seal heat leaks
- Low-E Windows
- Insulated exterior doors
41Bioclimate Chart
42Example 1
- Dry Bulb 73
- Relative Humidity 50
43In the zone
44Example 2
- Dry Bulb Temp. 78
- Relative Humidity 70
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46Example 2
- Dry Bulb Temp. 78
- Relative Humidity 70
- Requires a wind speed of 250 FPM
- (25060)/5280
- MPH 2.84
47Example 3
- Dry Bulb Temp. 50F
- Relative Humidity 55
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49Example 3
- Dry Bulb Temp. 50F
- Relative Humidity 55
- BTU/Hour 250
50What Does All This Mean?
51Relative Importance of Usage
52British Thermal Units
- The basic measure of heat
- The amount of heat needed to raise one pound of
water one degree Fahrenheit
53Heat Content of Fuels
- 1 Kilowatt-hour electricity 3,413 Btu
- 1 cubic foot of natural gas 1,025 Btu
- 1 gallon fuel oil 138,700 Btu
- 1 gallon kerosene 135,000 Btu
- 1 ton of coal 27,000,000 BTU
- 1 gallon LPG 91,000 Btu
- 1 pound LPG 21,500 Btu
54Energy and Power
- Power is theINSTANTANEOUS use of energy
- Think of it as POTENTIAL use, whether it is
running or not (engine, light bulb) - Btu/h
- Watts, Kilowatts (Watts Volts x Amps)
- the amount of voltage across a circuit x the
current through the circuit - Energy is USE of power over TIME (heat energy)
- Btu/h x hours Btu
- Watts x hours Watt hour (Kilowatt x h kWh)
55 56R-Value Resistance
- R-Value is the measure of resistance to heat flow
through the defined material. The higher the
R-Value the less heat will transfer through the
wall, making the system more energy efficient.
57R-Value Resistance
- Its the most common unit of measure for
describing insulation performance - Its the inverse of U-Value
- It represents Resistance to heat flow
- R-Value can be added (in thermal path)
- But cant be averaged over area
58U Value Measure of Heat Loss
- U-Value
- Rate of heat energy (Btu) flowing through 1 SF
of material, per hour, per 1F temp. difference - Basis of heat loss calculations
- U-Value is one over Rvalue (U1/R)
- Smaller U-Value means lower heat loss
- Larger U-Value means higher heat loss
- Windows and doors are rated in U
- U-Values can be averaged over surface areas
- but cannot be added in thermal path
59R Value in Assemblies
- Bevel Siding R .80
- ½ Plywood Sheathing R.63
- Wood Studs R1/In.
- Insulation R21
- Drywall R .45
60- BUILDING
- ASSEMBLY PROBLEM
- Calculate the theoretical R-Value of a wall
assembly
61R Value Calculation for an Assembly
- Wood Stud 5.5 X 1 R-5.5
- 1/5.5 .1818 U Value
- Insulation R-21
- 1/21 .048 U Value
- Siding R-.80
- 1/.8 1.25 U Value
- ½ Wall Sheathing R.63
- 1/.63 1.59
- Dry Wall R-.45
- 1/.45 2.22 U Value
62R Value Calculation for an Assembly
- Walls are framed 16 On Center (Add the R
Values) - 14.5 of the wall .8 .63 21 .45 22.88
- 1/23.02 .0437U Value
- 1.5 of the wall .8 .63 5.5 .45 R7.38
- 1/7.38 .1355 U Value
63R Value Calculation for an Assembly
- Stud Bevel Siding 1/2 Sheathing 1/2
Drywall - 5.5 .8 .63 .45 7.38
- 1/7.38 .1355 U Value
- Cavity Insulation Bevel Siding ½ Sheathing
1/2 Drywall - 21 .8 .63 .45 22.88
- 1/22.88 .0437 U Value
- UA Calculation
- UA (14.5 x .0437) (1.5 x .1355)/16 .052 U
Value - R Value of the Wall Assembly R 19
64 65UA
- UA refers to the U-Value, times the area of a
given component - UA is the heat transfer through that component
- Example 1000 SF of R-11 wall (U-Value 0.091)
- U x A .091 x 1000 91 Btu/hr/F
- U x A x ?T is the heat transfer at a given
temperature - Example Heat loss at 70F in and 30F out
- 91 x 40 3640 Btu/hr
- A Area
- U 1/R
66- R 1/U
- Btu/h U A ? T
- U Btu/h/ (A ? T)
- Btu/h 3.413 Watts
- U (3.413 W )/(A ? T)
- R (A ? T) / (3.413 W)
- R R-Value
- U U-Value
- A Surface Area (Must be in Square Feet)
- ? T Change in Temperature
- W Watts
671st Law of Thermodynamics
- The change in the internal energy of a system is
equal to the heat added to the system minus the
work done by the system. - ?U Q W
- ? U Change in internal energy
- Q Heat added to the system
- W Work done by the system
68Keeping it Real
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70- What conditions do we need for radiant heat
transfer to take place? - Difference in temperature
- An air gap between objects
- Two objects touch have the same temperature
- (Conduction)
71Can this product stop radiant heat transfer?
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73WINDOWS - 4 Ways to Evaluate
- U-FACTOR
- Solar Heat Gain Coefficient
- Visible Transmittance
- Air Leakage
74U-FACTOR
U-FACTOR The rate of heat loss is indicated in
terms of the U-Factor of a window assembly. The
insulating value is indicated by the R-Value
which is the inverse of the U-Value. The lower
the U-Value the greater a windows resistance to
heat flow and the better the insulating value.
75Solar Heat Gain COEFFICIENT
The SHGC is the fraction of incident solar
radiation admitted through a window. SHGC is
expressed as a number between 0 and 1. The lower
a windows solar heat gain coefficient, the less
solar heat it transmits.
76Visible Transmittance
The visible transmittance is an optical property
that indicates the amount of visible light
transmitted. Theoretical values vary between 0
and 1, but most values are between 0.3 and 0.8
77Air Leakage
Heat loss and gain occur by infiltration through
cracks in the window assembly. Air leakage is
expressed in cubic feet of air passing through a
square foot of window area. .3 is recommended
for Oregon
78Low-E Windows
- Glass is coated with silver or tin oxide which
allows visible light to pass through but reflects
infrared heat radiation back into the room. - Reduces heat loss in cool climates
- Allows visible light to pass through but reflects
infrared heat radiation away from the room,
admits up to 40 less radiant heat from the sun. - Reduces heat gain in warm climates
79High number for cold climate. Low number for warm
climates
The lower the number the better the insulating
value
The best windows have air leakage rating between
0.1 and 0.6 cfm/ft.
Varies from 0 to 1.0 The higher the the more
light is transmitted.
80Single-Glazed with Clear Glass
81Single-Glazed with Bronze or Gray Tinted Glass
82Double-Glazed with High Solar Gain Low-E Glass,
Argon/Krypton Gas
83Triple-Glazed with Moderate Solar Gain Low-E
Glass, Argon/Krypton Gas
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