# Demonstrate understanding of aspects of heat

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1 Demonstrate understanding of aspects of heat Heat Transfer Temperature - temperature is a measure of the average kinetic energy of the particles making up an object (measured in C or K) 0 K = -273 o C (absolute zero temperature at which all molecular motion ceases). 273 K = 0 o C, 373 K = 100 o C. To convert K to o C subtract 273; To convert o C to K add 273! A temperature change of 1 degree Kelvin (1 K) is the same as a temperature change of 1 degree celcius or centigrade (1 C) Heat - heat is a measure of the total energy of an object (measured in joules) Heat energy - thermal energy. It is transferred from one thing to another thing because of the temperature difference between them. Direction of energy flow is always from a warmer to a cooler thing. Heat won t transfer between objects at the same temperature. Latent heat - is the term used to describe energy which causes a change of state/phase without change of temperature. During a phase change, the heat energy goes into the work of breaking bonds and separating molecules, rather than increasing the temperature. The Specific Latent Heat of a Substance (L) is the quantity of energy needed to change the state of 1 kg of a substance without a change in temperature. The specific latent heat of fusion is the amount of heat required to convert 1 kg of a solid into the liquid without a change in temperature. The specific latent heat of vaporisation is the amount of heat required to convert 1kg of a liquid into the vapour without a change in temperature. The specific latent heat of fusion of ice at 0 o C, for example, is J kg -1. This means that to convert 1 kg of ice at 0 o C to 1 kg of water at 0 o C, J of heat must be absorbed by the ice. Conversely, when 1 kg of water at 0 o C freezes to give 1 kg of ice at 0 o C, J of heat will be released to the surroundings. Specific heat capacity. The specific heat capacity of a substance is the quantity of energy needed to change the temperature of 1 kg of the substance by 1 C. The specific heat capacity of water is high compared with most other substances: c water = 4200J kg -1 C -1 The greater the specific heat capacity of a substance, the more energy must be transferred to it or taken from it to change the temperature of a given mass of it.

3 o Some of the heat efficiency features of a barbeque include the burner box cover, the shiny steel hood and its wooden stand. Traps air reducing heat loss by convection AND reflects heat back minimising heat loss by radiation Minimises heat loss by convection and radiation to the surroundings. Insulator not much heat lost from the plate by conduction to the frame. Insulation insulation reduces unwanted energy transfer (and can keep warm things warm or cold things cool). Most insulating materials work by trapping air within fibres, or bubbles or similar cavities in a material like fibre glass or polystyrene. Air is a poor conductor of heat and the layer of air is a barrier to the transfer of heat. Insulation cuts down the loss of heat by reducing the effect of conduction & convection. Thermal expansion o Expansion is due to an increase in the average distance between atoms in the substance. o The atoms themselves do not expand; they simply move further away from their neighbours. (NEVER say particles expand in the exam!) o The expansion occurs due to the increased kinetic energy of the particles involved which them vibrate more and move further apart. o Some effects and applications of expansion and contraction in everyday life include riveting, gaps in bridges, overhead power and telephone lines, and thermostats. o Not all materials expand by the same amount for the same temperature change. E.g. bimetallic strip. Metal 2 expands more (has a higher coefficient of thermal expansion) than Metal 1 in the diagram below so the strip bends. Metal 1 Metal 2 HEAT

4 Q = mcδt o What this means is: Heat energy received or given out = mass of substance x specific heat capacity x temperature change: o Q = energy (in J) o m = mass (kg) o c = specific heat capacity (J/(kg o C), also written J kg -1 o C -1 ) o ΔT is the temperature change ( o C) The value of c is the same if you are cooling rather than heating the substance. In other words you get as much heat back out of the substance when you cool it as you put in when you heated it. Q = ml The Specific Latent Heat of a Substance (L). This is the quantity of energy needed to change the state of 1 kg of a substance without a change in temperature, units J kg -1. For water, the specific latent heat of fusion, L = J kg -1. The specific latent heat of vaporisation is rather higher, L = 2.3 x 106 J kg -1. The latent heat of vaporisation is therefore almost 7 times the latent heat of fusion; this indicates more energy is needed to separate the molecules in going from water to steam than to break up the lattice structure in going from ice to water. o Liquid to gas and vice versa latent heat of vaporisation (d) o Solid to liquid and vice versa latent heat of fusion (b) o Solid to gas and vice versa latent heat of sublimation (you don t often come across that) a, c and e Heat energy goes to change the temperature. Specific heat capacity equations apply. b and d Heat energy goes to change the state. Specific latent heat equations apply. P = E / t P = power in W, E = energy in J, t = time, in s. Eg 1. A 2 kw electric jug. 2 kw = 2000 W = 2000 J s -1. Eg 2. Power output of nuclear reactor is 120 kw. 120 kw = W = J s -1. o Power = energy / time o Time = energy / power SOME EXPLANATIONS Onshore & Offshore Breezes During the day, the ground heats up more quickly than the sea; this occurs because water has a larger specific heat capacity. The air in contact with the warm ground is heated by conduction. That air expands, becoming less dense than the surrounding cooler air. As a result, the warm air rises and other air moves horizontally (winds) to fill the space - creating an onshore sea breeze. Cooler air descends, and a convection current is set up, which transfers heat away from the land. Cooler air over sear Land warmed by the sun warms the air next to it Cool sea breeze At night, the ground loses its heat more quickly, and the water surface is warmer than the land. As a result, the breeze is offshore.

5 The Thermos Flask The thermos flask is designed to minimise heat transfer by conduction, convection and radiation. It is used to store either hot or cold liquids for long periods of time. It has a double wall of glass with a silvered inner wall. The space between the walls is evacuated to minimise heat transfer by conduction and convection. By reflecting most of the radiant heat, the silvered surface minimises heat transfer by radiation. The plastic or cork stopper in its neck prevents heat loss by convection and conduction. Satellites It is necessary to protection the sensitive electronic instruments in orbiting space satellites. In half of its orbit around the Earth, a satellite is exposed to intense radiation from the Sun, and in the other half it is in the Earth's cold shadow. Without protection, its interior would be subjected to tremendous extremes of heating and cooling. The interior of the satellite is wrapped with blankets of highly reflective aluminium foil. The foil's shiny surface reflects away much of the Sun's radiation while the satellite is in the unshaded part of the orbit, and helps retain interior heat while the satellite is in the Earth's shadow. Wool sweaters and down jackets These garments keep us warm by trapping the warmer air in regions close to our bodies and hence reducing heat loss by convection and conduction. What keeps us warm is not the clothing itself but the air trapped in the clothing.

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