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8/3/2019 1 - Thermal Effects in Buildings
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THERMAL EFFECTS IN BUILDINGS
Composite Materials Performance
MHK221188
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Introduction
The Basics
transfer; gases and vapours
Thermal Effects
Thermal insulation; insulation values; thermal bridging;
structural temperatures
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Nature of Heat
THERMAL ENERGYTHERMAL ENERGY
Heat is form of energy ie thermal energy
SI unit of heat is the Joule (J)Joule (J)
Others sometimes used; Calorie; kilowatt hour; and BTU
Other forms of energy also measured in Joules
POWERPOWER
Rate at which energy is converted from one form to another
P= H / t where H is Heat energy and t is time
SI unit of power is the Watt (W)Watt (W)(1 watt = 1 J/sec.)
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Nature of Heat
TEMPERATURETEMPERATURE
Simply, heat flows from objects at high temperature to those at
low temperature
By definition, when no heat transfer between the two objects they
are at the same temperature. Think of a heated building, heat will tend to flow from the hot
building to the cooler outside air (in winter) and visa versa in
summer
SI unit of temperature is the Kelvin (K)Kelvin (K)
0C = 273K 100C = 373K
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Nature of Heat
HEAT CAPACITY
Ability to hold heat
Do not confuse with Thermal Conductivity
Specific Heat Capacity = Quantity of heat required to raise 1kg of the
material by 1K(or1C) (Measured in J/kg K)
Water4190 J/kg K
Concrete 3300 J/kg K
Copper390 J/kg K
So water is a very good medium for storing heat
Water around British Isles retains heat and creates a temperate climate
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Nature of heat
DENSITY
Relates the mass of an object to its volume
Density () = mass (m) / volume (v)
Masonry high density (small volume has large
mass) therefore high heat capacity within smallvolume
Electric storage heater uses cheap electricity to
heat bricks up, which then emitheat during the day.
Heat storage capacity of brick, concrete and stone
very relevant to thermal behaviour of buildings
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Nature of Heat
CHANGE OF STATE
Solid; liquid; gas
Material absorbs heat to change from solid to liquid then to gas
Material releases heat when change form gas to liquid then solid
SENSIBLE AND LATENT HEAT
Sensible heat heat energy absorbed or released during a changein temperature
Latent heat ditto during change of state
Enthalpy
steam @ 373K > energy than water at 373K
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Heat transfer
Heat will transfer between bodies until they reach an equilibrium
CONDUCTION;
CONVECTION;
RADIATION
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Heat transfer
CONDUCTION
Transfer of heat energy through a material without the molecules
changing their positions
Heat transferred as molecules in one part heated, then heat moves toother parts
Metals best conductors (high in free electrons)
Poor conductors include liquids and gasses, so porous materials with
high air content, good insulators in buildings
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Heat Transfer
Measurement of thermal conductivity
Conduction can be measured
ThermalConductivitymeasure of rate at which heat is conducted. Relates to:-
Coefficient of thermal conductivity - Usually k or
Measured in W/mK i.e. the coefficient of thermal conductivity is heat flow in Watts
across 1m thickness of material for temp diff. of1K(1 C) and a surface area of1m
Resistivity (r)reciprocal of k-value ie r = 1/k or1/
Because reciprocal, r measured in mK/W
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Heat Transfer
CONVECTION
Transfer of heat energy through a material by the bodily movement of particles
Will only happen in fluids (i.e. liquids and gasses). Will not happen in solids
Convection occurs when the fluid e.g. air, is heated;
It then expands Heated (expanded) air is less dense, so cooler fluid displaces the warmer air causing
the latter to rise
New air then also heated and process repeated
Gives rise to a convection current
Convection currents in a room
Air is poor conductor but whole room can be heated by a
single heater, using Convection as the mode of heat transfer
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Heat Transfer
RADIATION
In outer space, convection and conduction are not possible, so how is the Earth
warmed by the sun?
Radiation - Defined as the transfer of heat energy by electromagnetic waves
Simple rules
Dull black surfaces have the highest absorption and emission of radiant heat
Shiny silver surfaces have the lowest absorption and emission of radiant heat
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Heat transfer
THE GREENHOUSE EFFECT
Sun emits short wavelength radiation
It passes through atmosphere and glass
Inside Greenhouse, heat absorbed by plants which then re-radiate heat
Re-radiated heat is of longer wavelength, which dont easily penetrate glass
Re-radiated heat is therefore trapped, causing internal temp. to rise
Planet Earth behaves in the same way.
Increase in GH gasses eg C0
Implies greater level of re-radiated heat is retained
Contribution to global warming
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Thermal Effects
LEARNING
Need for building insulation
Types of materials used
Calculate R-values and U-values
Compare types used in different parts
Assess the building for insulation quality
Building codes related to insulation
Assess bldg elements for relative insulation values
Cause and effect of thermal bridging
Temp profiles and prediction of condensation Why different structures respond to temperature changes at different rates ?
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Thermal Effects CONTENTS THERMAL INSULATION
materials;
insulators;
thermal conductivity;
INSULATION VALUES -
thermal transmittance (U-value);
elemental U-values; thermal resistance (R- value);
u-value adjustment
THERMAL BRIDGING
Bridge effects;
pattern staining;
combining U-values
STRUCTURAL TEMPERATURES
response times;
temperature gradients
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Thermal insulation
General
Retain heat inside for as long as possible
Conserves energy & reduces costs
Less energy use implies less CO (and other)
Implies reduced global warming
Good insulation will achieve this
Will also reduce heating effect in the summer
Consider a tent no insulation: hot in summer & very cold in winter
Large buildings sometimes more costly to cool than heat
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Thermal insulation
General (contd)
Condensation is a significant problem in poorly insulated properties particularly
where surface temperatures are low
Good thermal insulation will keep internal surface temperatures above the dew-
point and therefore reduce the condensation effect
Well placed insulation reduces time for a room to heat up e.g. when unoccupiedduring the day
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Thermal Insulation
INSULATING MATERIALS DESIGN to oppose transfer of heat between areas at different temperatures
Vacuum is perfect insulator against conduction not practical, so consider gasses
Atoms spaced well apart and low densities almost as good
Air is the active ingredient used in many insulation materials
E.g. mineral wool; aerated concrete
Cannot use air alone since no strength and moving air would also carry heat through
convection. (Air is trapped within min. wool)
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Condensation of water vapour
poor ventilation of rooms/thermal bridges
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Thermal insulation
MATERIALS (contd)
To restrict radiantheat, use surfaces that do not absorb or emit
radiant heat
Which are??
Shiny surfaces that reflect electromagnetic waves E.g. Aluminium foil
But Aluminium is a very good conductor!
However foil is so thin, very little conductive effect
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Thermal Insulation
Rigid preformed materials
Flexible materials
Loose fill materials
Materials formed on-site
Reflective materials
e.g. aerated concrete blocks
e.g. mineral wool quilts
e.g. expanded polystyrene granules
e.g. foamed polyurethane
e.g. aluminium foil
TYPES OF THERMAL INSULATOR
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Thermal Insulation
PROPERTIES
Good insulator
Suitable strength
Moisture resistance
Fire resistance
Pest and fungi resistance
Harmless to humans and environment
Compatible with adjacent materials
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Thermal Insulation
THERMAL CONDUCTIVITY
Remember:
thermal conductivity
(rate of conduction of heat)
k or
Units: W/mK
Values ofkcan vary due to differences in density, thickness, moisture content,
degeneration of the material, but for our purposes, we will assume a set density for a
particular material, as shown in Table 2.1
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Thermal Insulation
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Thermal Insulation
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Thermal Insulation
RESISTIVITY
Remember:
Reciprocal of conductivity (an alternative measurement for conduction)
r = 1/k
NB: not to be confused with Resistance (R) see later slides
THERMAL TRANSMITTANCE (U-VALUE)
U-value is usually the performance value defined in the Building Codes
(Building Regulations)
Applied to walls; floors and roofs in their composite form
e.g. the U-value of walls < 0.25 W/mK
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Insulation
values
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Emissivity and Absorption
Ability of a material to give off or absorb radiant heat
Relates to the surface of the material
Rough black absorbs and emits most heat
Shiny silver absorbs and emits least heat
All materials compared with a black body
EMISSIVITY fraction of energy radiated by a body compared to that radiated
by a black body at the same temperature
ABSORPTIVITY fraction of radiant energy absorbed by a body compared with
that absorbed by a black body etc
A "black body" is a theoretical perfect
absorber, which absorbs radiation of all
wavelengths falling on it. It reflects no light at
normal temperatures and thus appears black.
However, like ideal gas in kinetic theory, it is a
theoretical model and we may find in reality
only "Almost perfect black bodies".
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Emissivity and Absorption
Examples: Aluminium Emissivity 0.05 Absorption 0.2
Dark bricks Emissivity 0.9 Absorption 0.6
Generally, colour has an important effect on heat absorbed by the building via the
high temp. radiation from the sun.
Colour has little effect on the heat emitted from buildings (low temp. radiation)
Low E Glass
Transmits maximum light; rejects max. Solar energy; and reflects max. room temp
energy back into the room
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Insulation Values
THERMAL TRANSMITTANCE U VALUE
Different materials conduct heat at different rates
In a cavity, also heat transfer via convection and radiation
Also have to account for surfaces, because radiation and convection will be
affected by surface colour and exposure to weather
Combination of all these factors provides us with the overall thermal
transmittance or U-value
The higher the U-value the more heat flows through so a good U-value is a
low one as you want to keep heat inside the building or outside depending on
the climate you live in.
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Insulation Values
U-Value is a measure of the overall rate of heat transfer, by allmechanisms under standard conditions, through a particular
section of construction
Unit: W/mK
U values have a linear relationship with heat loss ie wall with U-value 0.3 W/mK loses heat at half the rate of a
wall with U-value of0.6 W/mK
Also, cost of replacement heat will be half!!
The technical explanation of the U-value
The U-value physically describes how much thermal energy in Watts[W] is transported through a building component with the size of 1
square meter [m] at a temperature difference of 1 Kelvin [K] (=1C).
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Elemental U-values
Insulation properties will vary,
depends on moisture content
U-values calculated assuming
standard values for mc and rates of
heat transfer at surfaces and in
cavities see slide on Standard
thermal resistances Building Regulations and Scottish
Codes use U-values as targets and
limits for thermal insulation and
energy use
U-value standard values
common basis for comparison (seetable 2.3)
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Elemental U-values
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Elemental U-values
Note: Values indicative only manufacturers details must be consulted for accurate assessment
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Thermal Resistance (R)
U-values calculated from the R-values of the various parts
that make up an element e.g. a wall
Thermal resistance (R)is a measure of the opposition to
heat transfer by a component in say a wall
Unit: mK / W
Three types of thermal resistance
Material resistance
Surface resistance
Airspace resistance
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Thermal Resistances,R
Thermal Resistance, R [m2K/W] A measure of the opposition to heat transfer offered by a particular component in a
building element.
Thermal resistance of homogeneous layers
Design thermal values can be given as either design thermal conductivity or design thermal
resistance. If thermal conductivity is given, we can obtain the thermal resistance of the layer from
where
d = thickness of material (m)
k = thermal conductivity of material (W/mK)
R= thermal resistance (m2 K/W)
k
dR!
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Thermal Resistance
MATERIAL RESISTANCES
Resistance Rdepends on the thermal conductivity (k)
and its thickness (d)
R = d/k
Also, R= r x d
Where r is the resistivity (as opposed to Resistance)
Remember, r = 1 / k
i.e. the reciprocal of the conductivity value
(When calculating U-values, we are usually told the k value i.e.
ThermalConductivity)
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Thermal Resistance
SURFACE RESISTANCES
Have to be factored into the U-value calculations as well
Usually given as a set of standard values (see table 2.4 below)
AIRSPACE RESISTANCES
Ditto
And ditto
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Thermal Resistance
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Thermal Resistance
Total Thermal Resistance
Calculate individual resistance of various components
Add them together
Get Total Thermal resistance - RT or R
Analogy Total Resistance is similar to adding electrical resistance inseries
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Thermal Resistance
Once we have RT (or R), only a simple step away from establishingthe U-Value !!!!!!
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Calculation of U-values
U-value is the reciprocal of Total Thermal Resistance ie
U = 1 / R
Where
U = U-value (W / m K)
R= sum of thermal resistances of all components in the element (eg
surface resistances; air space resistances; brick resistance; plaster
resistance; all forming a solid brick wall)
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Insulation Values U-values
Where:
U - thermal transmittance of overall structure ( W/m2 C)
Rsi,Rso - inside and outside thermal resistances (m2 C/W)
R1,R2 - thermal resistance of structural elements (m2 C/W)
Ra - thermal resistance of airspace (m2 C/W)
si 1 2 a so
1U =
R + R + R + ..... + R + R
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Calculation of U-values
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Calculation of U-values
Adjustments to U-values Typically we might have a 1930s as built cavity wall
We can calculate its existing U-value as described already,
perhaps 1.6 W/m K
What if we wanted to thermally upgrade the wall? What insulation would be needed to upgrade the U-value to a
target of say 0.3 W/m K
Calculation process is simply the reverse of what we have done
already