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