Physical Chemistry Lecture 30 Gibbs’s Phase Rule, Activity Components and phases Component -- a compound in a solution whose amount can be independently varied Example: Aqueous NaCl solution 2 components, NaCl and H2O Phase – a macroscopic piece of matter that is homogeneous with respect to physical attributes Example: a system of oil and vinegar has two liquid phases because oil and vinegar (an aqueous acetic acid solution) are immiscible How many components? How many phases? Equilibrium mixture of N2O4 (g) and NO2 (g) c = 1 because the equilibrium links the concentrations of the two species p = 1 (All gases are miscible.) COCl2 + CO + Cl2 at equilibrium with no excess CO or Cl2 c = 1 because the equilibrium is determined by decomposition of phosgene p = 1 (All gases are miscible.) COCl2 + CO + Cl2 at equilibrium with excess CO added (i.e. the concentrations of CO and Cl2 are unequal) c =2 because there are three materials but only one relationship between their concentrations p=1 How many components? How many phases? NH4Cl solid sits in an evacuated chamber. After a while, some ammonia and HCl appear in the gas phase above it. c = 1 because there is an equilibrium relationship AND the number of moles of NH3 and HCl must be equal. (Why?) p = 2, solid and gas NH4Cl (s) in contact with an arbitrary amounts of NH3 (g) and HCl (g) in a chamber c = 2 (There are three materials, but there is an equilibrium expression between them that links the concentrations.) p = 2, solid and gas Gibbs’s phase rule Applies to multicomponent systems Describes the number of degrees of freedom, f f = number of intensive variables required to specify the state Homogeneous single-component system has two degrees of freedom, T and P Depends on the number of components, c, and the number of phases present, p f = c − p + 2 How many degrees of freedom? Equilibrium gas phase containing N2O4 and NO2 f=1 – 1 + 2 = 2 Phosgene, CO and Cl2 (with CO and Cl2 derived from decomposition exclusively) f=1 – 1 + 2 = 2 Phosgene, CO and Cl2, with excess CO added f=2 – 1 + 2 = 3 NH4Cl, initially in an evacuated chamber, with NH3 and HCl present from decomposition f=1 – 2 + 2 = 1 Water, water vapor and ice in equilibrium f=1 - 3 + 2 = 0 Triple point of water Phase rule applied to H2O F=2 Points in the regions F=1 Points that are on a boundary line F=0 Point at an intersection Triple point There are several points where H2O has f = 0 There are many phases of water I count six points at which f = 0 on this graph for H2O Other materials, like CO2 have triple points From P. Atkins, Physical Chemistry Equilibrium activity in solution θ µ liq (aliq , T ) = µ liq (T ) + RT ln aliq For any liquid system Gas-phase activity is easily defined Solution activity defined with the concept of µ liq (aliq , T ) = µ gas (a gas , T ) phase equilibrium Activity in solution is determined relative to the activity of the vapor aliquid = exp(− (µ liqθ − µ θgas )/ RT ) = K (T ) a gas with which it is in equilibrium Phase equilibrium with an ideal-gas phase Generally activities in phases are related by equilibrium condition Vapor pressure is a measure of the gasphase activity in ideal limit Ideal-gas-limit activity depends on the gasphase standard state aliq ideal gas limit liq a = K a gas P = K θ P Summary Gibbs’s phase rule allows estimation of phase equilibrium Number of components and phases gives the number of degrees of freedom, f Related to the regions, lines and points on a phase diagram Determination of number of degrees of freedom depends on equilibrium requirements Care in expressing the requirements essential Equality of chemical potentials in two phases relates the equilibrium activities of materials in the two phases