CEE 680 Lecture #38 4/3/2020 Print version Updated: 3 April 2020 Lecture #38 Precipitation and Dissolution: Metal Carbonates & Hydroxides (Stumm & Morgan, Chapt.7) Benjamin; Chapter 8.7 ‐ 8.15 David Reckhow CEE 680 #38 1 Metal Carbonates Example of ligands that exist in different forms Consider CaCO 3 in a closed system Six species: Ca +2 , H + , OH ‐ ‐ 2 , HCO 3 ‐ , H 2 CO 3 * CO 3 Need six equations K 1 , K 2 , K w CO 3 -2 K so Ca +2 ENE CaCO 3 MBE David Reckhow CEE 680 #38 2 1
CEE 680 Lecture #38 4/3/2020 Calcium Carbonate K 2 [ Ca ] so K so 2 [ CO ] 3 K so C 2 T MBE [ Ca 2 ] C [ H CO * ] [ HCO ] [ CO 2 ] T 2 3 3 3 combining K 2 1 [ Ca ] so 2 [ Ca ] 2 2 [ H ] [ H ] 1 K K K 1 2 2 K [ Ca 2 ] so 2 David Reckhow CEE 680 #38 3 0 -1 Ca+2 -2 - HCO 3 -3 +/-0.5 slope -4 +/-1 slope -5 -6 Log C -2 -7 CO 3 -8 * H 2 CO 3 -9 -10 -11 Dissolution of CaCO 3 in -12 pure water -13 -14 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 pH David Reckhow CEE 680 #38 4 2
CEE 680 Lecture #38 4/3/2020 0 OH - -1 Problem - HCO 3 Ca+2 -2 -3 H+ -4 What is the pH of -5 CaCO3 in pure solution? -6 Log C -7 -2 CO 3 * H 2 CO 3 -8 -9 -10 -11 -12 -13 -14 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 pH David Reckhow CEE 680 #38 5 0 OH - -1 Solution - HCO 3 Ca+2 -2 -3 Use ENE H+ -4 -5 2 2 2 [ Ca ] [ H ] [ HCO ] 2 [ CO ] [ OH ] 3 3 -6 Log C -7 -2 CO 3 * H 2 CO 3 -8 -9 -10 -11 -12 -13 -14 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 pH David Reckhow CEE 680 #38 6 3
CEE 680 Lecture #38 4/3/2020 Analytical Solution Start with ENE and substitute 2 2 2 [ Ca ] [ H ] [ HCO ] 2 [ CO ] [ OH ] 3 3 K K 2 so [ H ] C 2 C w 1 T 2 T [ H ] 2 K K K K 2 so [ H ] so 2 so w 1 2 [ H ] 2 2 2 K K [ H ] so 2 2 w 0 1 2 [ H ] 2 S&M, equation #30 For CaCO 3 : pH=9.91 Pg. 376 David Reckhow CEE 680 #38 7 With other acy/alk CaCO 3 system with addition of: Strong acid (C A ) Strong base (C B ) 2 2 C 2 [ Ca ] [ H ] [ HCO ] 2 [ CO ] [ OH ] C B 3 3 A K K so w [ H ] 2 2 C C 1 2 A B [ H ] 2 S&M, equation #31 Pg. 376 David Reckhow CEE 680 #38 8 4
CEE 680 Lecture #38 4/3/2020 K [ Ca 2 ] so [ CO 2 ] 3 CaCO 3 in open system K so C 2 T K [ Ca 2 ] so 0 Applying the open system C T : K p 2 H CO 2 And substituting into the ENE: 2 2 2 [ Ca ] [ H ] [ HCO ] 2 [ CO ] [ OH ] 3 3 K p K p K K H CO H CO 2 so 0 [ H ] 2 w 2 2 1 2 K p [ H ] 2 H CO 0 0 2 K p K p K K H CO H CO 2 so 0 [ H ] 2 w 0 2 2 1 2 K p [ H ] 2 H CO 0 0 2 The pH is calculated to be: pH = 8.27 Quite similar to surface water processes David Reckhow CEE 680 #38 9 Open System Assuming equilibrium with a constant partial pressure of CO 2 (10 ‐ 3.5 atm) Stumm & Morgan, 1996, Figure 7.10, pg. 379 David Reckhow CEE 680 #38 10 5
CEE 680 Lecture #38 4/3/2020 Open system with other acy/alk CaCO 3 system with addition of: Strong acid (C A ) Strong base (C B ) 2 2 C 2 [ Ca ] [ H ] [ HCO ] 2 [ CO ] [ OH ] C B 3 3 A K p K p K K H CO H CO 2 so 0 [ H ] 2 w C C 2 2 1 2 A B K p [ H ] 2 H CO 0 0 2 David Reckhow CEE 680 #38 11 Carbonate dissolution Pathways Not covered in class Stumm & Morgan, 1996, Figure 7.12, pg. 385 David Reckhow CEE 680 #38 12 6
CEE 680 Lecture #38 4/3/2020 To next lecture David Reckhow CEE 680 #38 13 7
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