Problem 8.11 from Text Solution to Problem 8.11 Solution to Problem 8.11 Cont
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Problem 8.11 from text The normal boiling point of iodomethane, CH3I, is 42.43 ˚C and its vapor pressure at 0 ˚C is 140 torr. Calculate (a) standard enthalpy of vaporization (ΔH°vap) of iodomethane (b) standard entropy of vaporization (ΔS°vap) of iodomethane (c) the vapor pressure of CH3I at 25 ˚C Solution to problem 8.11 (a) The data given in the problem actually supplies the vapor pressure of at two temperatures (0 and 42.43˚C, or 273.15 and 315.58 K), so the easiest equation to use is: ln (P2/P1) ≈ - (ΔH°/R)(1/T2 - 1/T1) 760 !H˚ vap $ 1 1 ln = " # & 140 8.314 J mol -1K-1 % 315.58 K 273.15 K' -1 !H˚ vap= +28.6 kJ mol Solution to problem 8.11 cont. (b) Now we can use the basic expression ΔG° = ΔH° - TΔS° to solve for ΔS°. Since ΔG at boiling point is zero, ΔS°vap = (ΔH°vap/Τb) " 28600 J -1 !S˚ = $ = + 90.6 J K vap # 315.58 K% Solution to problem 8.11 (c) Use again: ln (P2/P1) ≈ - (ΔH°/R)(1/T2 - 1/T1) P 28600 J 1 1 ln 298 K = ! " # ! % 1 atm 8.314 J mol -1K-1 $ 298.15 K 315.58 K& P298 K = 0.529 atm = 402 torr Sample Problem CaCO3(s) CaO(s) + CO2(g) limestone lime Given: -23 ΔH° = + 178 kJ; at 25 ˚C, KP = 1.39 × 10 Give an estimate for KP at 800 ˚C. Solubility Equilibrium (Chap. 11) The process is in equilibrium when rate of ions (or molecules) leaving the solid = rate returning to the solid. That is, when dissolution rate = precipitation rate Solubility Product, Ksp (Sec. 11.10) y+ x- AxXy(s) x X (aq) + y X (aq) 2+ - (eg., BaCl2(s) Ba (aq) + 2 Cl (aq)) What is the form for the equilibrium constant? activities of products K = (at equilibrium) eq activities of reactants Write the equilibrium constant expression. Colligative Properties Depend solely on relative numbers of solvent and solute molecules in solutions, not on their chemical identity. The specifics of intermolecular interactions are not important for determining these properties Typical examples: Boiling point elevation and freezing point depression Osmosis and osmotic pressure Osmosis - The process Cross-sectional ∆h ∆V = A∆h area = A π = Osmotic Pressure, h (due to this “hydrostatic head”) Pure Solution Solvent Semi-permeable membrane Cross-sectional ∆h ∆V = A∆h area = A π = Osmotic Pressure, h (due to this “hydrostatic head”) Osmotic Pure Solution Solvent Pressure Semi-permeable membrane ρ = density of solvent ≈ density of solution (if very dilute) hA = Vsolution - Vsolvent = Volume of “hydrostatic head” ρ(Vsolution - Vsolvent) = ρ(hA) = mass of solvent in the “hydrostatic head” π = Osmotic Pressure = Force/Area = (mass × g)/Area (g = gravitational constant) [ρ(hA)] × g π = = ρhg A Osmosis Pure solvent “moves into” a solution when the solution and solvent are separated by a semipermeable membrane Why? Entropy increases when solvent moves through the membrane into the solution because the solute molecules then have a greater volume to move in. (See sections 7.3 and 7.6). Entropy change when solution volume increases by ∆V V V+∆V ∆V n moles of solute molecules expand into available solvent like a gas expands into a vacuum. ΔS = nRln[(V+∆V)/V] = nRln[1+(∆V/V)] Since V >> ∆V, ln[1+(∆V/V)] ≈ ∆V/V ∆S = nR(∆V/V) ⇒ T∆S = (nRT/V)∆V The solvent in the ΔV element must be “lifted” by height h. Cross-sectional ∆h ∆V = A∆h area = A π = Osmotic Pressure, h (due to this “hydrostatic head”) Equivalent Pure work needed Solution Solvent Semi-permeable to do the membrane “lifting” is (ρ∆V)gh. Entropy Gain vs Enthalpy Cost No more solvent will move from the pure solvent into the solution when ∆G for that process is no longer negative: ∆G = ∆H - T∆S The enthalpy cost from “lifting” the solvent” in the volume element ∆V is: ∆H = (ρ∆V)gh, But π = ρgh, ∴ ∆H = π∆V We already found T∆S = (nRT/V)∆V So, when ∆G = 0, π = nRT/V Other Useful Forms n π = nRT/V = [ /V]RT n [ /V] = moles solute per liter solution If we know mass (grams) of solute per liter, cm, then we transform to mol g mol ( /L) ~ ( /L)( /g) n c [ /V] = ( m/M) M = molar mass (“mol. weight”) c π = ( m/M)RT If the solute dissociates, a factor “i” accounts the actual number n of particles: π = i[ /V]RT Example: Determination of Polymer Molecular Weight 7 !/cm 6 atm 10-4 " 5 gm/L 4 3.3 " 10-4 30 2 4 6 8 10 cm , gm/L “Real-life” data for polyvinylchloride dissolved in cyclohexanone at 40 ˚C. What is the average molecular weight?.