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The kinetic theory of gases and the gas laws
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Kinetic theory/ideal gas
We can understand the behaviour of gases using a very simple model, that of an “ideal” gas. The model makes a few simple assumptions;
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You should know these by now!
Ideal gas assumptions The particles of gas (atoms or molecules) obey Newton’s laws of motion. You should know these by now!
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Ideal gas assumptions The particles in a gas move with a range of speeds
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Ideal gas assumptions The volume of the individual gas particles is very small compared to the volume of the gas
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Ideal gas assumptions The collisions between the particles and the walls of the container and between the particles themselves are elastic (no kinetic energy lost)
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Ideal gas assumptions There are no forces between the particles (except when colliding). This means that the particles only have kinetic energy (no potential)
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Ideal gas assumptions The duration of a collision is small compared to the time between collisions.
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P = F/A Pressure – A reminder
Pressure is defined as the normal (perpendicular) force per unit area P = F/A It is measured in Pascals, Pa (N.m-2)
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Pressure – A reminder What is origin of the pressure of a gas?
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Pressure – A reminder Collisions of the gas particles with the side of a container give rise to a force, which averaged of billions of collisions per second macroscopically is measured as the pressure of the gas Change of momentum
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The behaviour of gases
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The behaviour of gases http://phet. colorado
When we heat a gas at constant volume, what happens to the pressure? Why? Let’s do it!
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The behaviour of gases http://phet. colorado
When we heat a gas at constant volume, what happens to the pressure? Why? P α T (if T is in Kelvin)
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The behaviour of gases When we compress (reduce the volume) a gas at constant temperature, what happens to the pressure? Why? Let’s do it!
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The behaviour of gases When we compress (reduce the volume) a gas at constant temperature, what happens to the pressure? Why? pV = constant
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The behaviour of gases When we heat a gas a constant pressure, what happens to its volume? Why?
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The behaviour of gases When we heat a gas a constant pressure, what happens to its volume? Why? V α T (if T is in Kelvin)
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Explaining the behaviour of gases
In this way we are explaining the macroscopic behaviour of a gas (the quantities that can be measured like temperature, pressure and volume) by looking at its microscopic behaviour (how the individual particles move)
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p α 1/V or pV = constant The gas laws
We have found experimentally that; At constant temperature, the pressure of a fixed mass of gas is inversely proportional to its volume. p α 1/V or pV = constant This is known as Boyle’s law
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The gas laws At constant pressure, the volume of a fixed mass of gas is proportional to its temperature; V α T or V/T = constant This is known as Charle’s law If T is in Kelvin
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The gas laws At constant volume, the pressure of a fixed mass of gas is proportional to its temperature; p α T or p/T = constant This is known as the Pressure law If T is in Kelvin
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T1 T2 The equation of state By combining these three laws
pV = constant V/T = constant p/T = constant We get pV/T = constant Or p1V1 = p2V2 T1 T2 Remember, T must be in Kelvin
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An example At the top of Mount Everest the temperature is around 250K, with atmospheric pressure around 3.3 x 104 Pa. At seas level these values are 300K and 1.0 x 105 Pa respectively. If the density of air at sea level is 1.2 kg.m-3, what is the density of the air on Mount Everest? “Physics”, Patrick Fullick, Heinemann
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An example Take 1kg of air at sea level
At the top of Mount Everest the temperature is around 250K, with atmospheric pressure around 3.3 x 104 Pa. At seas level these values are 300K and 1.0 x 105 Pa respectively. If the density of air at sea level is 1.2 kg.m-3, what is the density of the air on Mount Everest? Take 1kg of air at sea level Volume = mass/density = 1/1.2 = 0.83 m3. Therefore at sea level p1 = 1.0 x 105 Pa, V1 = 0.83 m3, T1 = 300K.
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An example Therefore at sea level
At the top of Mount Everest the temperature is around 250K, with atmospheric pressure around 3.3 x 104 Pa. At seas level these values are 300K and 1.0 x 105 Pa respectively. If the density of air at sea level is 1.2 kg.m-3, what is the density of the air on Mount Everest? Therefore at sea level p1 = 1.0 x 105 Pa, V1 = 0.83 m3, T1 = 300K. At the top of Mount Everest p2 = 3.3 x 104 Pa, V2 = ? m3, T1 = 250K.
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An example Density = mass/volume = 1/2.1 = 0.48 kg.m-3.
At the top of Mount Everest the temperature is around 250K, with atmospheric pressure around 3.3 x 104 Pa. At seas level these values are 300K and 1.0 x 105 Pa respectively. If the density of air at sea level is 1.2 kg.m-3, what is the density of the air on Mount Everest? Therefore at sea level p1 = 1.0 x 105 Pa, V1 = 0.83 m3, T1 = 300K. At the top of Mount Everest p2 = 3.3 x 104 Pa, V2 = ? m3, T1 = 250K. p1V1/T1 = p2V2/T2 (1.0 x 105 Pa x 0.83 m3)/300K = (3.3 x 104 Pa x V2)/250K V2 = 2.1 m3, This is the volume of 1kg of air on Everest Density = mass/volume = 1/2.1 = 0.48 kg.m-3.
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pV = constant T
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T The equation of state Experiment has shown us that pV = nR
Where n = number of moles of gas and R = Gas constant (8.31J.K-1.mol-1) Remember, T must be in Kelvin
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Sample question A container of hydrogen of volume 0.1m3 and temperature 25°C contains 3.20 x 1023 molecules. What is the pressure in the container? K.A.Tsokos “Physics for the IB Diploma” 5th Edition
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Sample question A container of hydrogen of volume 0.1m3 and temperature 25°C contains 3.20 x 1023 molecules. What is the pressure in the container? # moles = 3.20 x 1023/6.02 x 1023 = 0.53 K.A.Tsokos “Physics for the IB Diploma” 5th Edition
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Sample question A container of hydrogen of volume 0.1m3 and temperature 25°C contains 3.20 x 1023 molecules. What is the pressure in the container? # moles = 3.20 x 1023/6.02 x 1023 = 0.53 P = RnT/V = (8.31 x 0.53 x 298)/0.1 = 1.3 x 104 N.m-2 K.A.Tsokos “Physics for the IB Diploma” 5th Edition
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Questions! Page 84 Questions 15,16,17 and 18 Page 85 Question 19
Answers:Answers
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