EACR 1257: BUILDING SCIENCE COURSE OUTLINE: 1. HEAT IN BUILDING 2. LIGHTING IN BUILDING 3. ACOUSTICS IN BUILDING REFERENCE: ENVIRONMENTAL SCIENCE IN BUILDING BY RANDALL MCMULLAN MSC, CPHYS, MCIGB, MLNSP FOURTH EDITION, 1998 1. HEAT a. Principles of Heat - Nature of heat - Heat transfer - Gases and vapours - Refrigerators and heat pumps c. Energy Use Condensation - Thermal comfort - Heat losses - Heat gains buildings - Heat balance - Energy consumption - Energy regulations b. Thermal Insulation - Insulating materials - V-values - Thermal bridging - Structural temperatures d. Ventilation, Humidity and - Ventilation - Humidity - Condensation in - Condensation conditions Principles of Heat A good thermal environment is a major aspect in the successful performance of a building. Both human beings and their buildings interact with the heat that surrounds them and they also contribute to this heat. Topics that are relevant to thermal design include the requirements of human comfort, the types of heat loss and heat gain by buildings, and the nature of moisture in the air. Before these topics are considered, this chapter describes the basic nature of heat, its measurement, and its effects. The properties of gases and their effects, such as refrigeration, are also studied. NATURE OF HEAT Heat energy The modern definition of heat that follows is a simple statement, but the truth of the statement was not obvious in the past and confused ideas about the nature of heat are still common. HEAT (H or Q) is a form of energy UNIT: joule (J). The joule is the standard SI unit of energy as used for measuring any other form of energy. Other units of energy still found in use include the following units: • calorie, where 1 cal = 4.187 J • kilowatt hour, where 1 kWh = 3.6MJ • British Thermal Unit, where 1 BTU = 1.055 kJ Heat energy is an internal molecular property of a material. Other forms of energy include mechanical energy, electrical energy, and chemical energy. These other forms of energy can all be converted to thermal energy. For example, the mechanical energy of moving surfaces is converted to heat by friction; electric currents flowing in conductors produce heat; and combustion (burning) converts the chemical energy contained in materials to heat. Thermal energy often forms an intermediate stage in the production of other forms of energy. Most electrical energy, for example, is produced by means of the thermal energy released in the combustion of fuels. The thermal energy radiated from the Sun is also the origin of most energy used on Earth including the fossil fuels, such as coal Power Power is a measure of the rate at which work is done, or at which energy is converted from one form to another. Power (P) = Heat energy (H)/ time (t) UNIT: watt (W) By definition, 1 watt = 1 joule/second. The watt is often used in the measurement of thermal properties and it is useful to remember that it already contains information about time and there is no need to divide by seconds. Temperature Temperature is not the same thing as heat. A red-hot spark, for example, is at a much higher temperature than a pot of boiling water; yet the water has a much higher heat 'content' than the spark and is more damaging. TEMPERA TURE is the condition of a body that determines whether heat shall flow from it UNIT: degree Kelvin (K) See also the definitions of temperature scales. Heat flows from objects at high temperature to objects at low temperature. When there is no net heat transfer between two objects they are at the same temperature. Thermometers The human body is sensitive to temperature but it is unreliable for measuring temperature. The brain tends to judge temperature by the rate of heat flow in or out of the skin. So for example, a metal surface always 'feels' colder than a plastic surface even though a thermometer may show them to be at the same temperature. A thermometer is an instrument that measures temperature by making use of some property of a material that changes in a regular manner with changes in temperature. Properties available for such use include changes in size, changes in electrical properties such as resistance, and changes in light emissions. Some of the more common types of thermometer are described below. a. Mercury-in-glass thermometers Mercury-in-glass thermometers use the expansion of the liquid metal mercury inside a narrow glass tube. The mercury responds quickly to changes in temperature and can be used between -39°C and 357°C, which is the range between the freezing point and the boiling point of mercury. b. Alcohol-in-glass thermometers Alcohol-in-glass thermometers use coloured alcohol as the liquid in the glass tube. Alcohol expands more than mercury and can be used between -112°C and 78°C, which is the range between the freezing point and boiling point of alcohol. c. Thermoelectric thermometers Thermoelectric thermometers use the electric current generated in a thermocouple, which is made by joining two different metals such as iron and constantan alloy. The current quickly varies with temperature and can be incorporated in remote or automatic control systems. d. Resistance thermometers Resistance thermometers use the change in electrical resistance which occurs when a metal changes temperature. Pure platinum is commonly used and the changes in its resistance can be measured very accurately by including the thermometer in an electrical circuit. e. Optical pyrometers Optical thermometers measure high temperature by examining the brightness and colour of the light emitted from objects at high temperatures. The light varies with temperature and is compared with a light from a filament at a known temperature. Temperature scales In order to provide a thermometer with a scale of numbers, two easily obtainable temperatures are chosen as upper and lower fixed points. The interval between these two points on the thermometer is then divided into equal parts, called degrees. The properties of water are used to define two common fixed points - the temperature at which ice just melts and the temperature of steam from boiling water - where both are measured at normal atmospheric pressure. Celsius scale The Celsius temperature scale numbers the temperature of the melting point of ice as 0, and the boiling point of water as 100. CELSIUS TEMPERATURE (°c) is a point on a temperature scale defined by reference to the melting point of ice and the boiling point of water UNIT: degree Celsius (°c) Degrees Celsius are also used to indicate the magnitude of a particular change in temperature, such as an increase of 20°c. The less correct term 'centigrade' is also found in use. Thermodynamic scale Considerations of energy content and measurement of the expansion of gases lead to the concept of an absolute zero of temperature. This is a temperature at which no more internal energy can be extracted from a body and it occurs at - 273.16 °c . The absolute (or thermodynamic) temperature scale therefore numbers this temperature as zero. The other fixed point for the thermodynamic scale is the triple point of water; the temperature at which ice, water, and water vapour are in equilibrium (0.01 DC). • THERMODYNAMIC TEMPERATURE (T) Is a point on a temperature scale defined by reference to absolute zero and to the triple point of water UNIT: degree Kelvin (K) The degree Kelvin is the formal SI unit of temperature but the degree Celsius is also used in common practice. The interval of a degree Kelvin is the same size as a degree Celsius, therefore a change in temperature of 1 K is the same as a change in temperature of 1 °c. The general relationship between the two temperature scales is given by the following formula. T = (θ) + 273 where T = Thermodynamic temperature (K) (θ) = Celsius temperature (°c). Heat capacity The same mass of different materials can 'hold' different quantities of heat. Hence water must be supplied with more heat than the oil in order to produce the same rise in temperature. Water has a greater heat capacity than oil; a property that is not to be confused with other thermal properties such as conductivity. The heat capacity of a particular material is measured by a value of specific heat capacity, and table 1.1 gives values for a variety of materials. The SPECIFIC HEAT CAPACITY (c) of a material is the quantity of heat energy required to raise the temperature of 1 kg of that material by 1 degree Kelvin (or 1 degree Celsius) UNIT: J/kg K (or J/kg °c) Table 1.1 Specific heat capacities Material Specific heat capacity J/kgK Water 4190 Concrete and brickwork 3300 Ice 2100 Paraffin and oil 2100 Wood 1700 Aluminum 910 Marble 880 Glass 700 Steel 450 Copper 390 2100 Note: The values for particular building materials vary. Application of heat capacity (water) The heat capacity of water is higher than the heat capacities of most other substances, so water is a good medium for storing heat. The temperatures on the planet Earth are stabilised by the huge quantities of heat energy stored in the oceans and the presence of this water around islands, such as the British Isles, prevents seasonal extremes of temperature. In summer the water absorbs heat and helps to prevent air temperatures rising; in winter the heat stored in the water is available to help prevent temperatures falling. Heat exchange devices, such as boilers and heating pipes, also make use of the high heat capacity of water for transferring heat from one place to another. Density The heat capacities of different materials are compared on the basis of equal masses. However, the same mass of different materials may occupy different volumes of space, depending upon their densities. Density (e) = Mass (M)/ Volume (V) UNIT: kilogram per cubic metre (kglm Heavyweight masonry materials, such as brick, concrete, and stone, have high densities. This means that relatively small volumes of these materials have a large mass and therefore provide a relatively high heat capacity within a small volume. An electric storage heater, for example, contains bricks which are heated by cheap rate electricity and then hold this heat for use later in the day. The heat storage provided by the brick, concrete, and stone used in construction is particularly relevant to the thermal behaviour of buildings, as will be discussed later. Change of state All matter is made from small particles called atoms and for most materials the smallest particle that exists independently is a group of atoms which are combined to form a molecule. The spacing of the molecules in a substance and the forces between them determine the phase, or state of matter, of that substance. In the normal ranges of temperature and pressure there are three possible states of matter and they have the basic characteristics given below. Solid state: The molecules are held together in fixed positions; the volume and shape are fixed. • Liquid state: The molecules are held together but have freedom of movement; the volume is fixed but the shape is not fixed. • Gas state: The molecules move rapidly and have complete freedom; the volume and shape are not fixed. The state of a substance depends upon the conditions of temperature and pressure which act on the substance. Consider, for example, the common forms of iron, water, and oxygen. At certain temperatures a material will undergo a change of state and in this change its energy content is increased or decreased. The absorption of heat by a solid or a liquid can produce the following changes of state: Liquefaction SOLID Vaporisation LIQUID GAS (Melting) (Boiling, Evaporation) The release of heat from a gas or a liquid can produce the following changes of state: Condensation GAS Solidification LIQUID SOLID Fusion Sensible and latent heat