Chemistry II Chapter 12 Solutions Thirsty Solutions Thirsty Solutions • homogeneous mixtures composition may vary from one sample to another appears to be one substance, though really contains multiple materials • most homogeneous materials we encounter are actually solutions e.g., air, sea water, blood, tea, coffee, ‘alcohol’ • nature has a tendency toward spontaneous mixing generally, uniform mixing is more energetically favorable Thirsty Solutions • solute is the dissolved substance seems to “disappear” “takes on the state” of the solvent • solvent is the substance solute dissolves in does not appear to change state • when both solute and solvent have the same state, the solvent is the component present in the highest percentage • solutions in which the solvent is water are called aqueous solutions Thirsty Solutions • nature has a tendency toward spontaneous mixing generally, uniform mixing is more energetically favorable Thirsty Solutions Thirsty Solutions Seawater is a more concentrated solution than body fluids. As a result when seawater flows through the digestive tract it draws water out of the surrounding tissues – leads to dehydration Types of Solutions and Solubility Solute Phase Solvent Phase gas gas liquid solutions gas liquid solid liquid liquid liquid soda (CO2 in H2O) vodka (C2H5OH in H2O) seawater (NaCl in H2O) solid solutions solid liquid Solid solid brass (Zn in Cu), steel, plastics Hg/Au Amalgam Solution Phase gaseous solutions Example air (mostly N2 & O2) Types of Solutions and Solubility soluble - when one substance (solute) dissolves in another (solvent) Insoluble - when one substance does not dissolve in another • the maximum amount of solute that can be dissolved in a given amount of solvent is called the solubility • solubility depends on – tendency towards mixing, and the types of intermolecular attractive forces • the solubility of one substance in another varies with temperature and pressure Types of Solutions and Solubility Nature’s Tendency towards Mixing: Entropy • Chemical systems tend toward lower PE e.g. two opposite charged particles attract • Solution formation does not necessarily lower the PE of the system the difference in attractive forces between atoms of two separate ideal gases vs. two mixed ideal gases is negligible yet the gases mix spontaneously • the gases mix because the energy of the system is lowered through the release of entropy • entropy is the measure of energy dispersal throughout the system • energy has a spontaneous drive to spread out over as large a volume as it is allowed Types of Solutions and Solubility The Effect of Intermolecular Forces • energy changes in the formation of most solutions also involve differences in intermolecular forces • The intermolecular forces in the solute and solvent may promote or prevent solution formation Types of Solutions and Solubility The Effect of Intermolecular Forces Types of Solutions and Solubility The Effect of Intermolecular Forces Relative interactions Solvent-Solute > Solute-to-Solute and Solvent-to-Solvent Solvent-Solute = Solute-to-Solute and Solvent-to-Solvent Solution Forms Solvent-Solute < Solute-to-Solute and Solvent-to-Solvent Solution May or May Not Form Solution Forms • when the Solvent-Solute attractions are weaker than the sum of the solute-to-solute and solvent-to-solvent attractions, the solution will only form if the energy difference is small enough to be overcome by the entropy Types of Solutions and Solubility The Effect of Intermolecular Forces Examples: • e.g. pentane (C5H12) and heptane (C7H16) – both have dispersion forces between their molecules AND there are dispersion forces between pentane and heptane molecules • All 3 interactions are of similar size – solvent-solute = solute-solute = solvent-solvent • they are soluble or miscible liquids Types of Solutions and Solubility The Effect of Intermolecular Forces Examples: • e.g. hexane (C6H14) and water (H2O) – water molecules has strong H-bonds to each other but cannot bond to hexane • Energy required to separate H2O molecules is too great, H2O interactions >>>> H2O/Hexane interactions • solvent-solute < solute-solute and solvent-solute < solvent-solvent • they are insoluble or immiscible liquids Types of Solutions and Solubility The Effect of Intermolecular Forces • Chemist’s Rule of Thumb – • • Like Dissolves Like a chemical will dissolve in a solvent if it has a similar structure to the solvent when the solvent and solute structures are similar, the solvent molecules will attract the solute particles at least as well as the solute particles to each other Classifying Solvents Solvent Class Structural Feature Water, H2O polar O-H Methyl Alcohol, CH3OH polar O-H Ethyl Alcohol, C2H5OH polar O-H Acetone, C3H6O polar C=O Toluene, C7H8 nonpolar C-C & C-H Hexane, C6H14 nonpolar C-C & C-H Diethyl Ether, C4H10O nonpolar C-C, C-H & C-O, (nonpolar > polar) Carbon Tetrachloride nonpolar C-Cl, but symmetrical Draw the above molecules Example 12.1a predict whether the following vitamin is soluble in fat or water OH OH H2C C H H C O C C C HO OH Vitamin C O Example 12.1b predict whether the following vitamin is soluble in fat or water O H C C CH3 HC C C HC C CH C H C O Vitamin K3 Energetics of Solution Formation • • • Separation of Solute must overcome IMF or ion-ion attractions in solute requires energy, ENDOTHERMIC ( + DHsolute) Separation of Solvent must overcome IMF of solvent particles requires energy, ENDOTHERMIC (+ DHsolvent) Interaction of Solute & Solvent attractive bonds form between solute particles and solvent particles “Solvation” or “Hydration” (where water = solvent) releases energy, EXOTHERMIC (- DHmix) DHsoln = DHsolute + DHsolvent + DHmix • • • DHmix depends on what you are mixing. If molecules can attract each other DHmix is large and negative. If molecules can’t attract DHmix is small and negative Energetics of Solution Formation DHsolute + DHsolvent < DHmix overall process will be exothermic DHsolute + DHsolvent > DHmix overall process will be endothermic Energetics of Solution Formation Heats of Hydration • for aqueous ionic solutions, the energy added to overcome the attractions between water molecules and the energy released in forming attractions between the water molecules and ions is combined into a term called the heat of hydration attractive forces in water = H-bonds attractive forces between ion and water = ion-dipole DHhydration = DHsolvent + DHmix = heat released when 1 mole of gaseous ions dissolves in water DHsoln = DHsolute + [DHsolvent + DHmix] ΔHsoln = ΔHsolute + ΔHhydration (+ve) (-ve) 24 Energetics of Solution Formation Heats of Hydration • |ΔHsolute| < |ΔHhydration| ΔHsoln = -ve = exothermic reaction, e.g. KOH KOH(s) → K+(aq) + OH-(aq) • |ΔHsolute| > |ΔHhydration| ΔHsoln = +ve = endothermic reaction, e.g. NH4NO3 NH4NO3(s) → NH4+(aq) + NO3-(aq) • ΔHsoln = -57.56 kJ/mol ΔHsoln = +25.67 kJ/mol |ΔHsolute| = |ΔHhydration| ΔHsoln ~ 0, e.g. NaCl NaCl(s) → Na+(aq) + Cl-(aq) ΔHsoln = +3.88 kJ/mol Energetics of Solution Formation Heats of Hydration ΔHsol’n = Δ Hsolute (+ve) + Δ Hhydration (-ve) Energetics of Solution Formation Heats of Hydration Which is NH4NO3, which is KOH? Solution Equilibrium • • • • the dissolution of a solute in a solvent is an equilibrium process initially, when there is no dissolved solute, the only process possible is dissolution shortly, solute particles can start to recombine to reform solute molecules – but the rate of dissolution >> rate of deposition and the solute continues to dissolve eventually, the rate of dissolution = the rate of deposition – the solution is saturated with solute and no more solute will dissolve Solution Equilibrium Solubility Limit • At dynamic equilibrium a solution has the maximum amount of solute dissolved in it - said to be saturated depends on the amount of solvent depends on the temperature and pressure of gases • a solution that has less solute than saturation is said to be unsaturated • a solution that has more solute than saturation is said to be supersaturated Solution Equilibrium How Can You Make a Solvent Hold More Solute Than It Is Able To? • solutions can be made saturated at non-room conditions – then allowed to come to room conditions slowly • for some solutes, instead of coming out of solution when the conditions change, they get stuck in-between the solvent molecules and the solution becomes supersaturated • supersaturated solutions are unstable and lose all the solute above saturation when disturbed e.g., shaking a carbonated beverage Adding Solute to a Supersaturated Solution of NaC2H3O2 http://www.youtube.com/watch?v=uy6eKm8IRdI Solution Equilibrium Temperature Dependence of Solubility of Solids in Water • solubility is generally given in grams of solute that will dissolve in 100 g of water • for most solids, the solubility of the solid increases as the temperature increases when DHsolution is endothermic • solubility curves can be used to predict whether a solution with a particular amount of solute dissolved in water is saturated (on the line), unsaturated (below the line), or supersaturated (above the line) Solution Equilibrium Factors Affecting the Solubility of Gases in Water • solubility is generally given in moles of solute that will dissolve in 1 Liter of solution • Gases have generally lower solubility than ionic or polar covalent solids because most are nonpolar molecules • for all gases, the solubility of the gas decreases as the temperature increases the DHsolution is exothermic because you do not need to overcome solute-solute attractions Solubility of Gases in Water at Various Temperatures 0.4 Solubility, g in 100 g water 0.35 0.3 0.25 CO2 acetylene 0.2 0.15 0.1 0.05 0 0 10 20 30 40 50 60 70 80 90 100 110 Temperature, °C Solubility of Gases in Water at Various Temperatures Solubility, g in 100 g water 0.008 0.007 0.006 0.005 N2 O2 0.004 0.003 0.002 0.001 0 0 10 20 30 40 50 60 70 Temperature, °C 80 90 100 110 Solution Equilibrium Factors Affecting the Solubility of Gases in Water Pressure • the larger the partial pressure of a gas in contact with a liquid, the more soluble the gas is in the liquid 35 persrst At lower pressure CO2 is less soluble and bubbles out of solution Solubility of Gases in Water at Various Pressures (temp = 20°C) Solubility, g in 100 g water 0.25 0.2 0.15 O2 CO2 0.1 0.05 0 0 200 400 600 Partial Pressure 800 1000 1200 Solution Equilibrium Factors Affecting the Solubility of Gases in Water Henry’s Law • the solubility of a gas (Sgas) is directly proportional to its partial pressure, (Pgas) Sgas = kHPgas Often written KH = [X] / P • kH is called Henry’s Law Constant Ex 12.2 – What pressure of CO2 is required to keep the [CO2] = 0.12 M at 25°C? Expressing Solution Concentration • solutions have variable composition • to describe a solution, need to describe components and relative amounts • the terms dilute and concentrated can be used as qualitative descriptions of the amount of solute in solution concentration = amount of solute in a given amount of solution Expressing Solution Concentration Molarity, M • moles of solute per liter of solution • used because it describes how many molecules of solute in each liter of solution • if a sugar solution concentration is 2.0 M, 1 liter of solution contains 2.0 moles of sugar, 2 liters = 4.0 moles sugar, 0.5 liters = 1.0 mole sugar Molarity, C (M) = moles of solute, n (mol) liters of solution, V (L) n = CV Preparing 1 L of a 1.00 M NaCl Solution Expressing Solution Concentration Molarity, M Dilution • often, solutions are stored as concentrated stock solutions • to make solutions of lower concentrations from these stock solutions, more solvent is added the amount of solute doesn’t change, just the volume of solution moles solute in solution 1 = moles solute in solution 2 • the concentrations and volumes of the stock and new solutions are inversely proportional C1∙V1 = C2∙V2 Expressing Solution Concentration Molarity, M e.g. find the volume of 12 M HCl required to make 1.0 L of 1.0 M HCl C1∙V1 = C2∙V2 Expressing Solution Concentration Molarity and Dissociation • the molarity of the ionic compound allows you to determine the molarity of the dissolved ions CaCl2(aq) → Ca+2(aq) + 2 Cl-(aq) • A 1.0 M CaCl2(aq) solution contains 1.0 moles of CaCl2 in each liter of solution 1 L = 1.0 moles CaCl2, 2 L = 2.0 moles CaCl2 • Because each CaCl2 dissociates to give one Ca+2 = 1.0 M Ca+2 1 L = 1.0 moles Ca+2, 2 L = 2.0 moles Ca+2 • Because each CaCl2 dissociates to give 2 Cl- = 2.0 M Cl 1 L = 2.0 moles Cl-, 2 L = 4.0 moles Cl- Expressing Solution Concentration Molality, m • moles of solute per 1 kilogram of solvent defined in terms of amount of solvent, not solution like the others • does not vary with temperature because based on masses, not volumes Molality, (m) = moles of solute (mol) mass of solvent (kg) Expressing Solution Concentration Parts by Mass (percent, pph) • parts of solute in every 100 parts solution • mass percent = mass of solute in 100 parts solution by mass if a solution is 0.9% by mass, then there are 0.9 grams of solute in every 100 grams of solution or 0.9 kg solute in every 100 kg solution Mass of Solute, g Mass Percent 100% Mass of Solution, g Mass of Solute Mass of Solvent Mass of Solution Expressing Solution Concentration Using Concentrations as Conversion Factors • concentrations show the relationship between the amount of solute and the amount of solvent 12%(m/m) sugar(aq) means 12 g sugar 100 g solution or 12 kg sugar 100 kg solution; or 12 lbs. 100 lbs. solution 5.5%(m/v) Ag in Hg means 5.5 g Ag 100 mL solution 22%(v/v) alcohol(aq) means 22 mL EtOH 100 mL solution • The concentration can then be used to convert the amount of solute into the amount of solution, or vice versa Preparing a Solution • need to know amount of solution and concentration of solution • calculate the mass of solute needed start with amount of solution use concentration as a conversion factor 5% by mass 5 g solute 100 g solution “Dissolve the grams of solute in enough solvent to total the total amount of solution” Example – How would you prepare 250.0 g of 5.00% by mass glucose solution (normal glucose)? Expressing Solution Concentration Parts by Mass (parts per million, ppm) • grams of solute per 1,000,000 g of solution • mg of solute per 1 kg of solution • 1 liter of water = 1 kg of water ppm = mass solute (g) mass solution (g) ppm = mass solute (mg) mass solution (kg) ppm = mass solute (mg) volume solution (L) x 106 Solution Concentrations Mole Fraction, XA • the mole fraction is the fraction of the moles of one component in the total moles of all the components of the solution • total of all the mole fractions in a solution = 1 • unitless • the mole percentage is the percentage of the moles of one component in the total moles of all the components of the solution = mole fraction x 100% mole fraction of A = XA = moles of components A total moles in the solution Ex 12.4a – What is the molarity of a solution prepared by mixing 17.2 g of C2H6O2 with 0.500 kg of H2O to make 515 mL of solution? Given: 17.2 g C2H6O2, 0.500 kg H2O, 515 mL soln. Find: M Concept Plan: g C2H6O2 mol C2H6O2 mol M M L mL soln. L soln. Relationships: M = mol/L, 1 mol C2H6O2 = 62.07 g, 1 mL = 0.001 L C2H Solve: 0.2717mol 1 mol C6OH2 O 17.2 g C 2 H 6O 2 M 2 6 20.2771 mol 62.07 g C 2 H 6O 2 0.515 L 0.001 L mL M 0.515 L M 5150.538 1 mL Check: the unit is correct, the magnitude is reasonable Ex 12.4d – What is the mole percent of a solution prepared by mixing 17.2 g of C2H6O2 with 0.500 kg of H2O to make 515 mL of solution? Given: 17.2 g C2H6O2, 0.500 kg H2O, 515 mL sol’n Find: C Concept Plan: g C2H6O2 mol C2H6O2 % mol A 100% mol total g H2O mol H2O C% Relationships: C = molA/moltot, 1 mol C2H6O2 = 62.07 g, 1 mol H2O = 18.02 g 1 mol O 2H O Solve: 2 H 6C 0.27 71Cmol 17 . 2 g C H O % 2 6 2 62.07 g C H 2O 6 02.2771 mol 100% 0.2771 mol C2 H 6O2 2 6 227.75 mol H 2O .500 kg H 2% O 0% 0.989 1000 g 1 mol H 2O 27.75 mol H 2O 1 kg 18.02 g H 2O Check: the unit is correct, the magnitude is reasonable Converting Concentration Units • assume a convenient amount of solution given %(m/m), assume 100 g solution given %(m/v), assume 100 mL solution given ppm, assume 1,000,000 g solution given M, assume 1 liter of solution given m, assume 1 kg of solvent given X, assume you have a total of 1 mole of solutes in the solution • determine amount of solution in non-given unit(s) if assume amount of solution in grams, use density to convert to mL and then to L if assume amount of solution in L or mL, use density to convert to grams • determine the amount of solute in this amount of solution, in grams and moles • determine the amount of solvent in this amount of solution, in grams and moles • use definitions to calculate other units Colligative Properties • Colligative properties – property that depends on the number or particles in solution not the type of particle • e.g. Vapor pressure lowering Freezing point depression Boiling point elevation Osmotic pressure Colligative Properties Vapor Pressure Lowering • What is the effect of a nonvolatile solute on the VP of a pure liquid? liquid vapor equilibrium of solvent particles Colligative Properties Vapor Pressure Lowering • the VP of a solution is lower than the VP of the pure solvent the solute particles replace some of the solvent molecules at the surface Addition of a nonvolatile solute ( ) reduces the rate of vaporization, decreasing the amount of vapor Eventually, equilibrium is re-established, but a smaller number of vapor molecules – therefore the vapor pressure will be lower Colligative Properties Vapor Pressure Lowering • a concentrated solution will draw solvent molecules toward it due to the natural drive for materials in nature to mix • similarly, a concentrated solution will draw pure solvent vapor into it due to this tendency to mix • the result is reduction in the conc. of the solution VP solution <<< VP pure solvent Colligative Properties Vapor Pressure Lowering Raoult’s Law • the VP of a volatile solvent above a solution is equal to its mole fraction of its normal vapor pressure, P° Psolvent in solution = solvent∙P° since the mole fraction of the solvent is always less than 1, the vapor pressure of the solvent in solution will always be less than the vapor pressure of the pure solvent Colligative Properties Vapor Pressure Lowering e.g. water at 25 °C contains 0.90 mol water and 0.10 mol sucrose Pure water has VP 23.8 torr, P soln = H2O∙P°H2O = 0.90 x 23.8 torr = 21.4 torr VP of solution is lowered in proportion to mole composition of the solvent, VP is 90% of the VP of pure solvent Colligative Properties Vapor Pressure Lowering Ionic Solutes and Vapor Pressure • according to Raoult’s Law, the effect of solute on the vapor pressure simply depends on the number of solute particles • when ionic compounds dissolve in water, they dissociate – so the number of solute particles is a multiple of the number of moles of formula units • the effect of ionic compounds on the vapor pressure of water is magnified by the dissociation since NaCl dissociates into 2 ions, Na+ and Cl, one mole of NaCl lowers the vapor pressure of water twice as much as 1 mole of C12H22O11 molecules would • the van’t Hoff factor, i, is the ratio of moles of solute particles to moles of formula units dissolved, e.g. NaCl, i = 2 Effect of Dissociation Dissociation is not ideally complete due to ion pair formation Colligative Properties Vapor Pressures of Solutions Containing a Volatile Solute • • when both the solvent and the solute can evaporate, both molecules will be found in the vapor phase the total VP above the solution will be the sum of the VPs s of the solute and solvent for an ideal solution Ptotal = Psolute + Psolvent • the solvent decreases the solute VP in the same way the solute decreased the solvent’s Psolute = solute∙P°solute and Psolvent = solvent∙P°solvent Colligative Properties Vapor Pressures of Solutions Containing a Volatile Solute Ideal vs. Nonideal Solution • in ideal solutions, the made solute-solvent interactions are equal to the sum of the broken solute-solute and solvent-solvent interactions ideal solutions follow Raoult’s Law • effectively, the solute is diluting the solvent • if the solute-solvent interactions are stronger or weaker than the broken interactions the solution is nonideal Vapor Pressure of a Nonideal Solution • when the solute-solvent interactions are stronger than the solute-solute + solventsolvent, the total vapor pressure of the solution will be less than predicted by Raoult’s Law because the vapor pressures of the solute and solvent are lower than ideal • when the solute-solvent interactions are weaker than the solute-solute + solventsolvent, the total vapor pressure of the solution will be larger than predicted by Raoult’s Law Colligative Properties Freezing Point Depression and Boiling Point Elevation • the melting/freezing point of a solution is lower than the melting/freezing point of the pure solvent Allows salt to melt ice even if ambient temp is below freezing Colligative Properties Freezing Point Depression and Boiling Point Elevation VP of soln. is shifted downward Net effect: lower mpt, higher bpt Depends on amount of solute not type = colligative property Colligative Properties Freezing Point Depression • the difference between the freezing point of the solution and freezing point of the pure solvent is directly proportional to the molal concentration of solute particles FPsolvent – FPsolution) = DTf = m∙Kf • m = molality of solution (mol solute/kg solvent) • the proportionality constant is called the Freezing Point Depression Constant, Kf the value of Kf depends on the solvent the units of Kf are °C/m Kf Colligative Properties Freezing Point Depression and Boiling Point Elevation • the boiling point of a solution is higher than the boiling point of the pure solvent Colligative Properties Freezing Point Depression and Boiling Point Elevation • the difference between the bpt. of the solution and bpt. of the pure solvent is directly proportional to the molal concentration of solute particles BPsolution – BPsolvent) = DTb = m∙Kb • the proportionality constant is called the Boiling Point Elevation Constant, Kb the value of Kb depends on the solvent the units of Kb are °C/m For water Kb = 0.512 °C/m Colligative Properties Osmosis • osmosis is the flow of solvent through a semi-permeable membrane from • solution of low concentration to solution of high concentration the amount of pressure needed to keep osmotic flow from taking place is called the osmotic pressure • the osmotic pressure, P, is directly proportional to the molarity of the solute particles R = 0.08206 (atm∙L)/(mol∙K) P = MRT Where M = molarity, T = temperature Colligative Properties of Strong Electrolyte Solutions • Ionic solutions: DTf = i m∙Kf DTb = i m∙Kb P = i MRT Use the van’t Hoff factor, i e.g. which has the highest bpt? 1 M sugar solution, 1 M NaCl solution or 1 M MgCl2 solution?