Gases: Properties and Behaviour Gas Laws Partial Pressures Kinetic Theory and Ideal Gases Real Gases Diffusion and Effusion Learning objectives Describe properties of gases and define ideal gas Describe the physical basis for pressure Identify units of pressure and convert between units Describe and apply the main gas laws Apply gas laws to stoichiometric problems Describe and apply law of partial pressures Features of gases Gases are always miscible Gases are compressible Gases exert pressure Gases are mostly nothing: less than 0.1 % of the volume is occupied by molecules (contrast 70 % for solids and liquids) The ideal gas law assumes molecules occupy zero percent Molecular interactions Strength of interactions between molecules determines the state Strong attractions make for high melting point (ionic solids) Weaker interactions between molecules occur in liquids (covalent molecules) Molecular interactions in gases are negligible Air is more than one removed from nothing Gases are mostly empty space: molecules occupy <0.1 % volume 1,000 times less dense than solids and liquids Emptiness allows complete mixing The Ideal gas The ideal gas is defined as follows Interactions between molecules are nonexistent Volume occupied by molecules is zero Collisions There are two types of collision Between the molecules and the container Between molecules In the ideal gas these collisions are perfectly elastic (no energy loss) Collisions between billiard balls mirrors the collisions between the molecules of an ideal gas Origins of pressure Pressure is force per unit area: F/A Force is rate of change of momentum: F = ma = d(mv)/dt Molecules colliding with the walls of the container exchange momentum Units of pressure The S.I. unit of pressure is the pascal (Pa) 1 Pa = 1 N/m2, where N is the S.I. unit of force 1 N = 1 kgm/s2 The weight of the air exerts pressure – atmospheric pressure This pressure is about 100,000 Pa Older is better 101 kPa is an inconvenient way of measuring pressure Traditional units are still used in preference to the SI system Atmospheres, cm (or mm) of Hg and torr are the most common Bar is becoming more widespread (1 bar = 100 kPa) How do I measure the atmosphere? Let me count the ways 1 atmosphere = 760 mm Hg = 76.0 cm Hg 14.70 psi 760 torr 1.013 bar 29.9 in Hg 101.3 kPa Standard temperature and pressure (STP) Standard conditions allow direct comparison of properties of different substances Standard temperature is 273 K (0ºC) Standard pressure is 760 mm Hg At STP, 1 mole of any ideal gas occupies 22.414 L Balancing act Weight of air supports equal weight of mercury (or other liquid) Mercury being dense, column is 76 cm equivalent to same weight of atmosphere (several miles high) 76 cm (760 mm) Hg = 1 atm Manometers measure pressure in a container (A) If pressure inside bulb < atmospheric, atmosphere pushes down more. (B) If pressure inside bulb > atmospheric, column is pushed towards open end. Gas Laws Physical properties of gases were among the first experiments performed in the “modern” scientific era, beginning in the 17th century All gases exhibit similar physical properties even if their chemical properties differ widely Properties can be summarized in a few simple laws Variables are pressure, volume, temperature and quantity. Keep one (or two) constant and vary the others Gas laws: experience in math form The properties of gases can be described by a number of simple laws The laws establish quantitative relationships between different variables They are largely intuitively obvious and familiar The four variables Pressure (P) Volume (V) Temperature (T in Kelvin) Number of molecules (n in moles) Variables and constants In the elementary gas laws two of the four variables are kept constant Each law describes how one variable reacts to changes in another variable All the simple laws can be integrated into one combined gas law Boyle’s law The first experimental gas law Pressure increases, volume decreases (T, n constant) 1 P V Mathematical form The volume of a fixed amount of an ideal gas varies inversely with pressure at constant temperature PV = constant P α 1/V 120 P vs 1/V Pressure (atm) 100 80 60 40 20 0 0 1 2 3 1/Volume (1/L) 4 5 Getting some exercise An exercise ball at pressure (Pa) = 1000 mm Hg has volume (Va) = 60 L When sat on, new volume (Vb) = 40 L. What is new pressure? P V PV a a b b PaVa (1000mmHg )(60 L) Pb 1500mmHg Vb 40 L Check: P increases as V decreases Note: doesn’t matter what units provided they are consistent Example Charles’ Law Pressure and amount constant As temperature increases, the volume increases Mathematical form The volume of a fixed amount of an ideal gas varies directly with absolute temperature at constant pressure VαT V/T = constant NOTE: Temperature must be in Kelvin (ºC + 273) At absolute zero there is no motion and the residual volume is that of the atoms – which is assumed to be zero 45 V vs T 40 35 Volume (L) 30 25 20 15 10 5 0 0 100 200 300 Temperature (K) 400 500 600 Example Avogadro’s Law Pressure and temperature constant Increase the amount, the volume increases Summary of gas laws Mathematical form The volume of an ideal gas varies directly with its molar amount at constant T and P Vαn V/n = constant Same volume of any gas contains same number of moles at constant T,P The standard molar volume at 273 K and 1 atm is 22.414 L Comparison with reality Standard molar volume of 22.41 L compares with experimental values of common real gases Agreement shows that these ideal gas laws can be widely applied for real gases Less ideal gases (NH3) agree better than some more ideal gases (Ar) Putting them together: the ideal gas law PV = nRT R is the gas constant = 0.0821 L-atm/mol-K Note units of R. R also appears in thermodynamic calculations, but with different units and numerical value (8.315 J/K-mol). Use the one appropriate to the calculation • Units of pressure – atm • Units of temperature – K • Units of volume – L Standard temperature and pressure: T = 0 ºC and P = 1 atm Example The combined gas law Allows us to calculate change in one variable for changes in the three other variables PV R nT Boyle Charles Combined Gas Law Amonton Avogadro Applications A system at initial conditions Xa changes to new conditions Xb PV PV a a b b naTa nbTb If we know three of the variables in state b, the fourth can be obtained In most of these problems na = nb PaVa PbVb Ta Tb The “simple” laws are derived from the combined law In case variable does not change its value, a = b Example: if T and n are unchanged, PV PV a a b b naTa naTa Boyle’s law is obtained: PV k Example Stoichiometry and gas reactions: Mole relationships in different states Solids: mass and molar mass Solutions: volume and molarity Gases: volume and ideal gas law Calculate volume of gas produced (product) or consumed (reactant) in a reaction at given conditions of P and T Calculate molar mass or density of a gas using ideal gas law Example Mixtures of gases: partial pressures Dalton’s law states that, in a mixture of gases, each gas behaves independently of the others and exerts the same pressure that it would by itself The total pressure exerted is the sum of the individual (partial) pressures of the components of the mixture P = P1 + P2 + P3 +… Example Partial pressure and the ideal gas law In a mixture of gases, pressure exerted by component i ni RT Pi V Where ni is number of moles of component i Total pressure is then: (n1 n2 n3 ...) RT Ptot Pi V i Mole fraction and the ideal gas law Mole fraction (Xi) is ratio of moles of component i to total number of moles ntot ni ni ni Xi (n1 n2 n3 ...) ntot ni i But n = PV/RT V Pi Pi RT Xi V Ptot Ptot RT ntot ni i Mole fractions and partial pressures The partial pressure exerted by any gas is equal to its mole fraction times the total pressure Pi X i Ptotal What is the partial pressure of each component in this mixture if total pressure is 600 mm Hg? Visual summary of the gas laws