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Chem. 31 – 11/20 Lecture
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Announcements Quiz 5 (last quiz) - Today
Labs Due on Wednesday (can turn in early) Formal Part A 11/22 IC Part 1 11/22 Today’s Lecture Chapter 8 – Advanced Equilibrium Equilibrium problems – modified to account for activity – cont. from last time Real equation for pH and use in calculations Failure of the ICE method with two equilibria The systematic method and its six steps
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Ionic Strength Effects Effects on Equilibrium - Quantitative
Calculate expected [Mg2+] in equilibrium with solid MgCO3 for cases both with and without NaCl. 2nd case summary: [CO32-] = 4.66 x 10-4 M vs. [CO32-] = 1.87 x 10-4 M if assumed m = 0 What about 1st case? Isn’t m = 0 ? No. Initially, yes, but as MgCO3 dissolves the ionic strength increases. This problem must be solved through iterations. Go over iterations
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Ionic Strength Effects Real Equation for pH
pH = -logAH+ = -log(gH+[H+]) Example Problem: Determine the pH of a solution containing M Ba(OH)2
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Second Part to Chapter 8 The Systematic Method
Question: Why can’t we apply the ICE (initial, change, equilibrium) method to any type of equilibrium problem? Answer: That method is best designed for cases where there is only one relevant equilibrium reaction. Examples of failures: Solubility of MgCO3 pH of 5.0 x 10-8 M HCl solution (Show failure of Chem. 1B method) Note: both problems can be solved using ICE method, but problem set up is more complicated
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The Systematic Method Solubility of MgCO3 – Why did it fail?
MgCO3 Mg2+ + CO32- x x Equil. (in ICE) So x = (Ksp)1/2 = 1.87 x 10-4 M (neglecting ionic strength effects) Problem is both ions can react further: CO32- + H2O HCO3- + OH- And HCO3- + H2O H2CO3 + OH- Also, Mg2+ + OH- MgOH+ And Mg2+ + CO32- MgCO3 (aq) Finally, we also have H2O H+ + OH- re-establishing equilibrium Each additional reaction results in greater dissolution To properly solve problem we must consider 6 reactions not just 1 Measured “[CO32-]” from titration = [CO32-] + 0.5[OH-] + 0.5[HCO3-] + [MgCO3] + 0.5[MgOH+] The “further” reactions makes [Mg2+] ≠ [CO32-], so ICE method fails (or needs modification by ICE tables for other reactions) Actual solubility is greater than ICE method finds [Mg2+]total = solubility ~ 3.3 x 10-4 M (from systematic approach) Predicted HCl needed = 3.3 mL (vs. ~3.5 mL) These calculations didn’t include activity which would lead to a ~10% increase in solubility (~3.6 mL HCl needed). In 0.1 M NaCl, I get 6.1 mL HCl needed (close to that observed) enhancements: (% over rxn 1 only) 90% 0% 9% 16%
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The Systematic Method The Six Steps
Write out all relevant reactions Write a “Charge Balance Equation” Write “Mass Balance Equations” Write out all equilibrium equations Check that the number of equations (in 2 to 4 above) = (or maybe >) the number of unknowns (undefined concentrations) Solve for the desired unknown(s) by reducing the equations to one equation with one unknown. Then solve for remaining unknowns Note: the emphasis of teaching the systematic method is steps 1 to 5. Step 6 will be reserved for “easy” problems with 2 to max 3 unknowns
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The Systematic Method pH of 5.0 x 10-8 M HCl
Demonstrate Method on Board
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The Systematic Method Conceptual Approach to Mass Balance Equations
With every source of related species, there should be one mass balance equation (or one set for ionic compounds) Example: Solubility of AgCl in water with M 1,10-phenathroline (Ph) Reactions: 1) AgCl(s) Ag+ + Cl- 2) Ag+ + 2Ph Ag(Ph)2+ Mass Balance equations: if only rxn 1) [Cl-] = [Ag+] w/ rxn 2) [Cl-] = [Ag+] + [Ag(Ph)2+] 1,10-phenathroline Ag+ Ph Ph Ph Ph Ag+ Ag+ Cl- Cl- Ag+ Ag+ Cl- Cl- 2nd Mass Balance Equation: [Ph]o = M = [Ph]Total = [Ph] + 2[Ag(Ph)2+] AgCl(s) Notes: with rxn 1) only, 2 Ag+s = 2 Cl-s; with rxn 2) also, 3 Cls = 2 Ags + 1 Ag(Ph)2 Initially 4 Phs, then 2 Phs + one complex containing 2 Phs (so total # of Phs remains constant)
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The Systematic Method 2nd Example
A student prepares a solution that contains mol of AgNO3 and mol NH3 in water with a total volume of 1.00 L. The AgNO3 is totally soluble, NH3 is a weak base, and Ag+ reacts with NH3 to form Ag(NH3)2+. Assume the Ag+ does not react with water or OH-. Go through the first 5 steps of the systematic method.
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