Kinetic Theory of Gases Connect microscopic properties (kinetic energy and momentum) of molecules to macroscopic “state” properties of a gas (temperature and pressure). Molecular Speeds 1 3 K = mv 2 = kT 2 2 Since 3 1 1 3 K = mv 2 and PV = NkT ∴ K = mv 2 = kT 2 2 2 Temperature is a measure of the average kinetic energy (internal energy?) of the gas. For constant volume, pressure increases directly proportional to an increase in average kinetic energy (temperature) AND an increase in the number of molecules. Ideal Gas Law Using moles PV = nRT vp ⇒ 2kT df (v) = 0 ⇒ vp = m dv mv 2 ⎛ m ⎞ 2 2 − 2 kt f (v) = 4πN ⎜ ⎟ v e ⎝ 2πkT ⎠ ∞ ∫0 Note v= f (v)dv = N 1 ∞ 8kT ∫ vf (v)dv = πm N 0 vrms = 1 ∞ 2 3kT v f (v)dv = ∫ 0 N m Real Gasses Using molecules PV = NkT n = number of moles N = number of molecules R = universal gas constant k = Boltzmann’s constant = 8.315 J / (mol-K) 3kT = vrms m Distribution of molecular speeds, But v2 = The Maxwell-Boltzmann distribution 1 2 ⎛1 ⎞ PV = Nmv 2 = N ⎜ mv 2 ⎟ 3 3 ⎝2 ⎠ ⇒ = 1.38 x 10-23 J / K “Real” gases do not follow the ideal gas law precisely. However, at low pressure and temperatures “not too close” to the liquefaction point, the ideal gas law is quite accurate and useful for “real” gases. Pressure not too high Not near liquefaction point Why the “breakdown”? This is called the Equation of State. Why “Ideal”? •Dilute, Volume of Molecules is ~ Zero •No Attractions Between Molecules •Temperature must be in Absolute Units, K Reasonable Near liquefaction Intermolecular forces matter P-V Diagram Each line is at a constant temperature Solid = Real, Dashed = Ideal Point c is the critical point, curve C is critical temp. 1 Phase Diagrams Vapor Pressure Since the liquid has a distribution of molecular speeds Some molecules will “escape” Since the gas has a distribution of molecular speeds Some molecules will be “recaptured” Triple Point is important as a reference standard What happens above the critical point? At equilibrium: saturated vapor pressure (SVP) What is the temperature on a day when the partial pressure of water is 530 Pa and the relative humidity is 40.0%? Liquid temperature = SVP temperature Boiling occurs Law of partial pressures The total pressure of a mixture of gasses = the sum of vapor pressure of the constituent gasses This is temperature dependent. Vapor pressure “explains” boiling Condensation The gas will exert a “vapor” pressure Vapor Pressure Evaporation PT = P1 + P2 + … Relative Humidity RH = partial pressure of H 2 O × 100% SVP of H 2O Dew Point: Temperature at which unsaturated air will become saturated. 2 Real Gasses - Better Approximations Ideal Gas nRT V First Order Clausius Equation of State (EoS) P= P= nRT V − nb Second Order Van der Waals P= nRT a − V − nb (V / n )2 Random Walk - Diffusion On average, the diffusing substance will move from a region of high concentration to a region of low concentration. Why? J = DA Mean Free Path Molecular concentration Assume the other molecules are not moving, then the number of molecules in the cylinder is NC = N N Vcyl = π (2r ) 2 v Δt V V Mean Free Path is average distance between collisions lM = d v Δt 1 = = NC N π (2r ) 2 v Δt N 4πr 2 V V If you account for the movement of the other molecules lM = 1 N 4 2πr 2 V A student walks across a field that is 60 m x 40 m. Estimate the student’s mean free path if there are (a) 10, (b) 100, (c) 300 other students on the field. C1 − C2 Δx J = Rate of Diffusion D = Diffusion Constant (gas dependent) A = Cross-Sectional Area 3 Heat Heat What is heat? It is a measure of internal energy. It is a measure of the “closeness” of thermal equilibrium. What happens when two systems that are not in thermal equilibrium come in contact? Since heat is the “flow” of energy from one system to another, the standard SI unit is the joule J “Traditional” unit is the calorie (cal) 1 cal is the heat needed to raise 1g of water from 14.5°C to 15.5°C Used to measure energy content of food Conversion 4.186 J = 1 cal, 4.186 x 103 J = 1 kcal British Thermal Unit (Btu) 1 kcal = 3.97 Btu When the temperature of system changes, there has been heat flow Q Heat capacity connects heat flow to temperature change: Q = CΔT A kilocalorie (kcal) or Calorie (Cal) is 1000 cal Heat will only flow from the system with the higher temperature to the system with the lower temperature Heat will only flow from the system with the higher average internal energy to the system with the lower average internal energy Total internal energy does not matter. Heat Capacity Units Heat (Q) is the “flow” or “transfer” of energy from one system to another Often referred to as “heat flow” or “heat transfer” Requires that one system must be at a higher temperature than the other Energy will be transferred from the higher temperature system to the lower energy system until thermal equilibrium is reached – that is they have the same temperature. Heat What is heat? What do we know about temperature? What do we mean when we say something is hot or cold? Is “heat” the same as temperature? Heat capacity C depends on the material and also on the quantity of material present. Eliminate quantity dependence by introducing specific heat c and molar heat capacity c′: Q = mcΔT m = mass Q = nc′ΔT n = number of moles 4 Specific Heats and Molar Heat Capacities Measuring Heat Capacities Calorimeter System is adiabatically isolated from the environment Net Q = 0 from or into the device Heat lost = heat gained Conservation of energy An axe head consisting of 1.8 kg of iron is left outdoors one cold winter’s night and is brought indoors when the outside temperature is a brisk 240K. The room into which it is brought is initially at a nice, comfortable 293K and 1.0 atm of pressure. The volume of the room, which is well insulated, is 38 m3. Assuming that the axe head comes to thermal equilibrium with the air in the room, by how much is the temperature of the room lowered? (Ignore the thermal interaction with furniture, walls, and so forth. Use cair = 0.172 cal/g-K and 28.8 g/mol for the molecular weight of air.) 5
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