1 / 18

III. Colligative Properties

Solutions. III. Colligative Properties. A. Definition. Colligative Property property that depends on the number (amount) of solute particles in the solution & not in the nature of the solute particles. Colligative Properties. Vapor Pressure Lowering Boiling Point Elevation

mari
Download Presentation

III. Colligative Properties

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Solutions III. Colligative Properties

  2. A. Definition • Colligative Property • property that depends on the number (amount) of solute particles in the solution & not in the nature of the solute particles

  3. Colligative Properties • Vapor Pressure Lowering • Boiling Point Elevation • Freezing Point Depression • Osmotic Pressure

  4. Vapor Pressure Lowering • Vapor Pressure- pressure exerted by the vapor/gas above the liquid • VP of sol’n < VP of solvent P = P1º-P1 = X2P1º where: P1º = V.P. of solvent X2 = mole frxn of solute P1 = V.P. of solution

  5. Boiling Point Elevation • Boiling Point- the temperature at which the vapor pressure equals the external atmospheric pressure. • B.P. of sol’n > B.P. of solvent Tb= Tb-Tbº = i Kbm Tbº = B.P. of solvent Kb = molal B.P. constant Tb = B.P. of solution = (0.52 °C/molal for H2O) m = molality of sol’n i = van’t Hoff Factor

  6. van’t Hoff Factor, i i = actual # of particles in sol’n after dissociation # of formula units initially dissolved in sol’n • Nonelectrolytes (covalent) • remain intact when dissolved • 1 particle • Electrolytes (ionic) • dissociate into ions when dissolved • 2 or more particles

  7. Boiling Point Elevation Solute particles weaken IMF in the solvent.

  8. Applications - Fractional Distillation

  9. Freezing Point Depression • Freezing Point- the temperature at w/c a liquid phase is converted to the solid phase • F.P. of sol’n < F.P. of solvent Tf= Tfº - Tf = i Kfm Tfº = F.P. of solvent Kf = molal F.P. constant Tf = F.P. of solution = (1.86 °C/molal for H2O) m = molality of sol’n i = van’t Hoff Factor

  10. Applications • salting icy roads • making ice cream • antifreeze • cars (-64°C to 136°C) • fish & insects

  11. Osmotic Pressure • Osmosis- the selective passage of solvent molecules from a semi-permeable membrane from a dilute solution to more concentrated one. • Osmotic Pressure- pressure needed to prevent osmosis.  = i MRT  = osmotic pressure T = absolute temp M = molarity of sol’n i = van’t Hoff Factor R = 0.082058 L-atm/mol-K

  12. Isotonic sol’n – sol’ns w/ same osmotic pressure / con’c • Hypotonic sol’n – the sol’n w/ lower con’c & osmotic pressure • Hypertonic- the sol’n w/ higher con’c & osmotic pressure

  13. Applications - Reverse Osmosis (Desalination of Water)

  14. NOTES • The effects of Colligative Properties on ELECTROLYTE soln’s are GREATER compared to NON_ELECTROLYTE soln’s.

  15. Calculations 1. What are the B.P. & F.P. of a 2.47 molal sol’n of naphthalene in benzene, (naphthalene does not ionize in benzene), given the ff data for benzene: BP = 80.1 °C Kb = 2.53 °C/molal FP = 5.5 °C Kf = 5.12 °C/molal

  16. Calculations 2. A sol’n containing 0.8330 g of a non-dissociating polymer of unknown structure in 170.0 mL of an organic solvent was found to have an osmotic pressure of 5.30 mmHg at 25°C. Determine the molar mass of the polymer. 3. The freezing point depression of a 0.100 M MgSO4(aq) sol’n is 0.225 °C. Calculate the van’t Hoff Factor of MgSO4(aq) at this con’c.

  17. Calculations 4. How many grams of Urea [(NH2)2CO] must be added to 450 g of H2O to give a sol’n w/ a V.P. of 2.50 mmHg less than that of pure H2O at 30°C. (V.P. of H2O at 30°C is 31.8 mmHg) 5. The average osmotic pressure of seawater is about 30.0 atm at 25°C. Calculate the molar con’c of an aqueous sol’n of Urea [(NH2)2CO], that is isotonic w/ seawater.

More Related