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Water Science Electroneutrality, pH, Alkalinity, Acidity Reversible Equations Carbonate Equilibrium System Examples Rain Ocean pH Acid Rain Acid Mine Drainage.

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Presentation on theme: "Water Science Electroneutrality, pH, Alkalinity, Acidity Reversible Equations Carbonate Equilibrium System Examples Rain Ocean pH Acid Rain Acid Mine Drainage."— Presentation transcript:

1 Water Science Electroneutrality, pH, Alkalinity, Acidity Reversible Equations Carbonate Equilibrium System Examples Rain Ocean pH Acid Rain Acid Mine Drainage naturescrusaders.files.wordpress.com

2 Water Electroneutrality Balanced: ∑ Cations = ∑ Anions ∑ C C x e C = ∑ C A x e A C C = moles / liter of cation c (one mole = 6.02x10 23 ) e C = number of charges per molecule of cation C A subscript is for anions Pure water: [H + ] = [OH - ] Natural water: [H + ] = [OH - ] + [HCO 3 - ] + 2[CO 3 -2 ] blog.ssis.edu.vn/

3 pH - reporting H + concentration pH = - log {H + } {} = activity, the effective concentration pH = - log [H + ] for dilute solutions [] = Molar concentration (moles/Liter) [H + ] = 10 -pH

4 Why do we care about pH? Biological systems Extremes are disruptive Corrosivity Equilibrium relationships involving H +

5 Good pH ranges Freshwater... Marine... Drinking... Soda?

6 Alkalinity Capacity of water sample to neutralize an... Capacity of a water sample to take H + without significant change in... Common ions that give water alkalinity HCO 3 -, CO 3 2- & OH -

7 Acidity Capacity of water to take OH - without significant pH change Opposite of Alkalinity Capacity of water sample to neutralize a base Common ion: H + For Acid Mine Drainage Acidity =~f(Fe 2+, Fe 3+, Al, Mn, and H + ) csmphotos.files.wordpress.com

8 pH, Alkalinity & Acidity Waters with same pH can have different amounts of Alkalinity or Acidity Chemicals may be present that can react with or release H + or OH - The lower the alkalinity (or acidity), the easier it is to change pH

9 Reversible Reactions aA + bB ↔ cC + dD A & B can react to form C and D C & D can react to form A and B After sufficient time has passed, equilibrium is reached Equilibrium can be perturbed by adding more reactant or product

10 Reversible Reactions: Gas - Solution At equilibrium Gaseous chemical dissolves Dissolved chemical volatilizes At equal rate Henry’s Law Example… Gas Dissolved

11 Reversible Reactions In Solution At equilibrium Reactants become products Products become reactants At equal rate Example…

12 Reversible Reactions: Solution - Precipitate At equilibrium Precipitate is formed Precipitate is dissolved At equal rates Example…

13 Equilibrium Equation aA + bB ↔ cC + dD K is constant at given temperature & relatively low concentration

14 Example - Pure Water What is water?... Reversible equation?... Equilibrium equation?... At 25 C, K w =... Even if other sources of H + (acids) or OH - (bases) are present Which substance predominates?...

15 pH of Pure 25 C? Follow these steps Write down species... Write electroneutrality eq... Write equilibrium equation.. Solve equations...

16 Now, add… OH - ? (add a strong base) Systems finds new equilbrium, with less H + and more OH - pH goes up H + ? (add a strong acid, precipitate iron,…) Systems finds new equilbrium, with more H + and less OH - pH goes down. Either way, [H + ] [OH - ] = K w still holds

17 Precipitation of Limestone CaCO 3 -2 ↔ Ca +2 + CO 3 -2 [Ca +2 ] [CO 3 -2 ] = K sp K sp = Solubility product Do not include precipitate in equilibrium equation [Ca +2 ] [CO 3 -2 ] < K sp ?... [Ca +2 ] [CO 3 -2 ] > K sp ?...

18

19 Carbonate Equilibrium System (CES) Keeps natural waters in good pH range Common Chemicals Carbon Dioxide, CO 2 Carbonic Acid, H 2 CO 3 Bicarbonate, HCO 3 - Carbonate, CO 3 -2 Solids containing Bicarbonate, Carbonate, Hydroxide, and (though rarely) certain Oxides (CaO),…

20 Main Sources CO 2 from atmosphere Byproduct of biological or chemical reactions combustion Solids containing carbonate e.g., limestone Byproduct of sea life CO 2 g CO 2 aq H 2 CO 3 HCO 3 CO 3 Solid CO 3,… Atmosphere Solution Precipitate

21 CES Reactions Reversible CO 2 g ↔ CO 2 aq CO 2 aq + H 2 O ↔ H 2 CO 3 H 2 CO 3 ↔ H + + HCO 3 - HCO 3 - ↔ H + + CO 3 -2 Ca +2 + CO 3 -2 ↔ CaCO 3 Equilibrium (at 25  C) CO 2 aq = CO 2 g / 1637 atm [H 2 CO 3 ] / [CO 2 aq] = 1.58 x [H + ] [HCO 3 - ] / [H 2 CO 3 *] = 4.47x10 -7 M [H + ] [CO 3 -2 ] / [HCO 3 - ] = 4.68x M [Ca +2 ] [CO 3 -2 ] = 3.80 x M 2 Where CO 2 g is in atm & CO 2 aq is in mole fraction

22 Carbonate System & pH Typical Natural Water with 100 mg/L alkalinity as CaCO 3 pH 100 mg/L as CaCO CO 2 CO 3 HCO 3 OH

23 Carbonate System Scenarios Open / Closed Open - in equilibrium with atmosphere open container, streams & shallow lakes, upper ocean Closed - not in equilibrium Closed tank, quick reactions, deep regions of water bodies, soil gases Homogeneous / Heterogeneous Homogeneous – in equilibrium with CO 3 solids Heterogeneous– not in equilibrium with CO 3 solids Closed & heterogeneous bottom of stratified lake with floor of limestone water treatment unit with soda ash / acid or base / CO 2 & some CaCO 3 precipitates

24 Example - Natural pH of Rain CO 2 in atmosphere naturally “shifts” pH of rain from 7 to ? Open system No solid source of CO 3 CO 2 g CO 2 aq H 2 CO 3 HCO 3 - CO 3 - H+H+ H+H+ Lowers pH

25 Atmosphere Nitrogen atm Oxygen atm Argon atm CO atm When this example was created. It’s now atm ( ppm) Misc atm TOTAL atm

26 Solution: pH of Rain (1) Atmosphere to raindrop - Henry’s Law: CO 2 aq = CO 2 g / 1637 atm Convert to M: [CO 2 aq] = CO 2 aq x M w M w = molar density of water = mol/l

27 Solution: pH of Rain (2) Reaction with water forms carbonic acid - Equilibrium Equation: [H 2 CO 3 aq] = 1.58x10 -3 M [CO 2 aq] [H 2 CO 3 * aq] = [CO 2 aq] + [H 2 CO 2 aq]

28 Solution: pH of Rain (3) Dissociation of carbonic acid - Equilibrium Equation: [H + ] [HCO 3 - ] = 4.47 x M [H 2 CO 3 *] Two unknowns? Use electroneutrality: [H + ] = [OH - ] + [HCO 3 - ] + 2[CO 3 -2 ] Rain water is acidic, so [OH - ] & [CO 3 -2 ] will be small giving [H + ] ≈ [HCO 3 - ], leading to…

29 Solution: pH of Rain (4) pH = - log [H+] = -log (2.13x10 -6 ) =… Check assumptions? Use equilibrium equations: [OH - ] = M 2 / [H + ] = M 2 / 2.13x10 -6 M = 4.68x10 -9 M (small, OK)) [CO 3 -2 ] = 4.68x M [H + ] / [HCO 3 - ] = 4.68x M 2.13x10 -6 M / 2.13x10 -6 M = 4.68x M (small, OK)

30 pH of Rain CO 2 in atmosphere goes up?... Use this method for different conditions? Need to check assumptions about relative concentration of [OH - ] & [CO 3 -2 ]

31 Atmospheric CO 2 & Ocean pH Oceans can be CO 2 sink or source Currently: sink, taking ~ 30% of anthropocentric CO 2 Primary mechanisms Carbonate equilibrium system (Henry’s Law,…) Biological Pump Living creatures take up carbon, some are trapped in sea bed Too much CO 2 ? pH drop of oceans could effect sea organisms From 1751 to 1994 surface ocean pH estimated to have dropped from ~ 8.18 to 8.10

32 Ocean pH Change ~half Anthropogenic CO 2 has been absorbed by ocean so far Currently absorbing ~1/3 22 M tons / day Could drop to 7.6 Drastic effect on shell-forming organisms National Geographic (2014) “Ocean Acidification”, ocean.nationalgeographic.com.

33 Acid Rain Rain with pH below 5.7 Most prevalent cause: SO x produced from burning coal SO x reacts with water to form sulfuric acid Sulfuric acid dissolves into atmospheric water and dissociates into H - and SO 4 -2

34 Precipitation pH downwind of Ohio Valley power plants

35 Sulfur Cap & Trade Program

36 CES, Alkalinity, Acid Rain’s Effect Carbonate solids Common source of alkalinity in natural waters (as they dissolve) Lakes and streams with alkalinity can accept acid rain without big pH changes Alkalinity buffers acid rain Acid rain can damage water bodies that don’t have alkalinity

37 Acid Mine Drainage

38 Red Oak Mine Site

39 Mine Side View Water Infiltration Anaerobic Conditions Low pH High Acidity High metals FeS 2 + O 2 + H 2 O → Fe 2+ + SO H + Fe 2+ + O 2 + H + → Fe 3+ + H 2 O Fe 3+ + H 2 O → Fe(OH) 3 ↓ + H + Presence of limestone will buffer the mine water, resisting pH change Even lower pH Oxidation of organic matter can lead to high concentrations of CO 2 in mine headspace pH – 4.4 (low) [drops to ~2 after seep] Acidity 434 ppm CaCO 3 (high) Partial Pressure CO 2 in mine headspace - ~6% [200x higher than atmosphere]

40 Red Oak Seep seep discharge

41 Plan View Not to scale

42 Red Oak Remediation Post injection, seep characteristics were pH - 6.3, Alkalinity mg/L as CaCO3, Fe- 120 mg/l; however, this level of treatment lasted only 15 months.


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