Chapter 13: Physical Properties of Solutions, Slides of Law

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Chapter 13: Physical Properties of Solutions Key topics: Molecular Picture (interactions, enthalpy, entropy) Concentration Units Colligative Properties terminology: • Solution: a homogeneous mixture • Solute: the component that is dissolved in solvent -- usually in smaller amount • Solvent: medium (often water) into which solutes are mixed -- usually in greater amount • concentration: describes how much solute there is -- dilute: small amount of solute -- concentrated: large amount of solute -- saturated: contains as much solute as can be dissolved -- unsaturated: can dissolve more solute -- supersaturated: more than saturated, unstable -- solubility: amount of solute dissolved in a given volume of a saturated solution a supersaturated solution can be prepared by forming a saturated solution at a high temperature, and then cooling it (many solutes are more soluble at higher temperature) Addition of a crystal (nucleation site) causes precipitation from a supersaturated solution. Molecular view of a soluble ionic compound in water. Some of the solute will fall out of solution (as a solid) if the solution is disturbed (vibration, dust, etc) Molecular view of the solution process: Ultimately, we can say that any process is governed by ΔG = ΔH - TΔS (Equation 14.10, ΔG < 0 for spontaneity) • ΔH < 0 helps (exothermic, H = enthalpy) • ΔS > 0 helps (increased disorder, S = entropy) • ΔH > 0 (endothermic) is possible if ΔS compensates Schematic depiction of the mixing of solvent and solute. Concentration Units: molarity = M = moles of solute liters of solution molality = m = moles of solute mass of solvent (in kg) For very dilute aqueous solutions, molarity and molality are equal since 1 L of H2O weighs 1 kg. mole fraction of A = A = moles of A sum of moles of all components percent by mass = mass of solute mass of solute + solvent ⇥ 100% = mass of solute mass of solution ⇥ 100% = parts per hundred If we multiply by 106 instead of 100 we get parts per million (ppm); if we multiply by 109 we get parts per billion (ppb). e.g., the drinking water standard for arsenic is 10 ppb (EPA’s Maximum Contaminant Level) Choice of units depends on the purpose of the experiment: w Mole fraction: used for gases and vapor pressures of solutions w Molarity: commonly used since volumes of solutions are easy to measure w Molality: temperature independent w Percent by Mass: temperature independent and we don’t need to know the molar mass Unit Conversions: e.g., Determine the molality of an aqueous solution that is 4.5% urea by mass. Solution: The molar mass of urea is 60.06 g/mol. There are different ways to approach this: we will assume we have 1 kg of water. Then, with the mass of urea as x, 4.5 = x x+ 1kg ⇥ 100 ) 100x = 4.5(x+ 1kg); ) 95.5x = 4.5 kg Which gives x = 47.12 g. The molality is then (47.12 g)/(60.06 g/mol) 1 kg = 0.78m e.g., At 20.0°C, a 0.258 m aqueous solution of glucose (C6H12O6) has a density of 1.0173 g/mL. Calculate the molarity of this solution. Solution: In 1 kg of water, we have 0.258 mol glucose. Also, 0.258 mol glucose weights (0.258 mol)(180.156 g/mol) = 46.48 g. Therefore we have (1 kg) + (46.48 g) = 1046.48 g solution. This occupies (1046.48 g) / (1.0173 g/mL) = 1028.68 mL. Thus the molarity is (0.258 mol) / (1.0287 L) = 0.251 M. Factors that affect solubility: We can sometimes rationalize solubility using Le Chatelier's principle. e.g., dissolving oxygen in water releases heat: O2(g) O2(dissolved) + heat Non-volatile solute interferes with the solvent’s liquid-vapor equilibrium (from chemwiki.ucdavis.edu). Solution: c = (1.3 x 10-3 mol/L • atm)(1 atm x 22/100) = 2.9 x 10-4 mol/L e.g., Calculate the pressure of O2 necessary to generate an aqueous solution that is 3.4 x 10-2 M in O2 at 25ºC. Solution: From the previous problem, we know that a pressure of 0.22 atm O2 gives a solution of 2.9 x 10-4 M. From Henry’s Law, we know that doubling the pressure also doubles the amount of dissolved gas. Therefore, 3.4⇥ 102 2.9⇥ 104 = 117.2 ⇥ 0.22 atm = 25.8 atm Colligative Properties: Properties that depend only on the number of solute particles in solution and not the nature of the solute. 1. Vapor-Pressure Lowering For a non-volatile solute, the vapor pressure of the liquid decreases. Another way to think of it: solute shifts equilibrium to the left solvent (l) solvent (g) Raoult’s Law makes this quantitative: P1 = 1 P o 1 P1 partial pressure of a solvent over a solution 1 mole fraction of the solvent in the solution P o 1 vapor pressure of the pure solvent Note: If there is only one solute, χ1 = (1-χ2) where χ2 is the mole fraction of the solute, and thus P 1 = (1 2 )P o 1 ) P o 1 P 1 = P = 2 P o 1 e.g., Calculate the mass of urea that should be dissolved in 225 g of water at 35ºC to produce a solution with a vapor pressure of 37.1 mmHg. (At 35ºC, P o H2O = 42.2 mmHg) Solution #1: How many moles of water do we have? 225 g 18.02 g/mol = 12.49 mol 1 = P 1 P o 1 = 37.1 mmHg 42.2 mmHg = 0.879 = 12.49 mol water x mol urea + 12.49 mol water Thus moles of urea is 1.72. The mass of urea needed is (1.72 mol)(60.06 g/mol) = 103 g. Ideal hexane-octane solution (from Ross Church). Note that when the solution mole fractions are equal (0.5), the vapor above the solution is enriched in the more volatile species. This is the principle behind fractional distillation. Solution #2: 2 = P P o 1 = 42.2 37.1 42.2 = 0.121 = x mol urea x mol urea + 12.49 mol water If both components are volatile, the vapor will contain both substances, and Raoult’s Law still applies: PA = AP o A PB = BP o B PT = PA + PB (Dalton , s Law of Partial Pressures) PT = AP o A + BP o B 4. Osmotic Pressure Osmosis is the selective passage of solvent molecules through a semipermeable membrane which blocks the passage of solute molecules. It occurs from a more dilute solution to a more concentrated one. quantitative expression: π = MRT π osmotic pressure (atm) M molarity of the solution R gas constant (0.08206 L⋅atm/K⋅mol) T temperature (K) Two solutions of equal concentration have the same osmotic pressure and are said to be isotonic to each other. Osmotic pressure. Beginning with equal levels of pure solvent and solution (left), the solution level rises as a result of the net flow of solvent from left to right. The osmotic pressure π, required to stop osmosis, can be measured directly from the difference in the final liquid levels. Electrolyte Solutions Colligative properties depend only on the number of dissolved particles, not on the type of particle. Therefore, a 0.1 m solution of NaCl has twice the freezing-point depression of a 0.1 m nonelectrolyte solution. Free ions and ion pairs in solution. Ion pairing reduces the number of dissolved particles in solution, affecting the colligative properties. Solution Ions Theoretical ΔTf 1.00 m NaCl Na+, Cl- (1.86)(2.00 m) = 3.72°C 1.00 m (NH4)2SO4 2 NH4 +, SO4 2- (1.86)(2.00 m) = 5.58°C The theoretical freezing-point depression is usually an overestimate because the ions can form pairs. To be quantitative we introduce the van’t Hoff factor i: i = actual number of particles in solution after dissociation number of formula units initially dissolved in solution and we modify the equations for colligative properties: ΔTb = iKb m ΔTf = iKf m π = iMRT Paint (pigment particles in solvent) and milk (fat globules in water) are common examples of colloids. Colloids A colloid is a dispersion of particles of one substance throughout another substance. It is intermediate between a homogenous and heterogeneous mixture. The particle size (1 – 103 nm) is much larger than in solution. Categories: o Aerosols (liquid or solid dispersed in gas) o Foams (gas dispersed in liquid or solid) o Emulsions (liquid dispersed in another liquid) o Sols (solid dispersed in liquid or in another solid) o Gels (liquid dispersed in solid) Tyndall effect. Hydrophilic colloid (a globular protein). One way to distinguish a colloid from a solution is by the Tyndall Effect : the scattering of light by dispersed particles. When the dispersing medium is water, we can classify colloids as hydrophilic or hydrophobic. Hydrophobic colloid stabilized by adsorbed ions. Common example: clay. Emulsification of grease by detergent molecules. An unstable colloid can be stabilized by the addition of an emulsifier. Soaps (sodium stearate) and detergents work by adsorbing to the surface of hydrophobic dirt/grease particles, allowing them to be dispersed in water and removed.