Presentation Slides for Air Pollution and Global Warming: History, Science, and Solutions Chapter 10: Acid Deposition By Mark Z. Jacobson Cambridge University Press (2012) Last update: February 23, 2012 The photographs shown here either appear in the textbook or were obtained from the internet and are provided to facilitate their display during course instruction. Permissions for publication of photographs must be requested from individual copyright holders. The source of each photograph is given below the figure and/or in the textbook. History of Acid Deposition 1200s. Coal used in lime kilns and forges produces sulfur and nitrogen oxides that result in sulfuric and nitric acid deposition. 1750s. Expanded use of the steam engine at the beginning of the Industrial Revolution increases sulfuric and nitric acid deposition. 1783. French Academy of Sciences offers a prize to a person who finds the most efficient and economical method to produce soda ash Na2CO3(aq), which along with animal fat, is used to make soap. 1789. Nicolas LeBlanc develops two-step soda ash process. The Rise of Alkali Factories Soda ash + Animal fat = Soap www.nutritionfx.com Img.alibaba.com Keetsa.com LeBlanc Process High temperature 2NaCl(s) + H2SO 4(aq) Na2SO 4(aq) + 2HCl(g) Sodium Sulfuric Sodium Hydrochloric chloride (salt) acid sulfate acid High temperature Na2SO 4(aq) + 2C + CaCO 3(s) Na2CO3(aq) + CaS(s) + 2CO 2(g) Sodium Carbon Calcium Sodium Calcium Carbon sulfate from carbonate carbonate sulfide dioxide charcoal from chalk (10.1) - (10.2) Sulfuric acid produced by burning sulfur and saltpeter in water 7S(s)+6KNO3(s)+4H2O(aq) --> 3K2S(s)+6NO(g)+4H2SO4(aq) Byproducts of Leblanc Process HCl(g) evaporated H2SO4(g) NO(g), which produces HNO3(g) Soot (C) CO2(g) --> widespread acid deposition due mostly to HCl(g) CaS(s), yellow-gray powder, forms hydrogen sulfide and gypsum CaS(s) + H2O(aq) --> CaO(s) + H2S(g) CaS(s) + O2(g) + 3H2O(aq) --> CaSO4-2H2O(s) + H2(g) Piles of gypsum (galligu) still exist near old soda-ash factories. Gypsum/Galligu Piles Halton Borough Council, UK Gypsum/Galligu Piles www2.halton.gov.uk The Rise of Alkali Factories Widnes in Cheshire, 1800s, under cloud of LeBlanc Process Halton Borough Council, UK History of Acid Deposition 1791. LeBlanc patents technique 1793. Loses patent to the state during French Revolution 1806. LeBlanc commits suicide 1838. Liverpool landowner files complaint against an alkali factory: destroyed crops and interfered with hunting. Early 1860s. William Gossage, who built alkali factory in 1830, develops scrubber for HCl(g) by converting a windmill into a tower, filling tower with brushwood, and letting water drip down the brush as smoke rose from the bottom. HCl Scrubber Today www.engpro.com History of Acid Deposition 1861. Ernst Solvay (1838-1922) develops another way to form soda ash, but it replaces Leblanc process only by 1880s. 1863. Due to devastation from Alkali factories and Gossage’s scrubber, the 1863 Alkali Act passes in the U.K. France. Regulation takes the form of planning laws controlling location of alkali factories. 1866, 1868. Inventions allow chlorine to be recycled for bleaching powder. 1881. U.K. Alkali Act is modified since significant pollution of other chemicals from alkali factories still occurs. Solvay Process 1861. Solvay rains a salt made of sodium chloride and ammonium down a tower over an upcurrent of CO2(g). Only inputs: limestone, salt. Only byproduct: calcium chloride. Production of carbon dioxide CaCO3(s) + heat --> CaO(s) + CO2(g) Production of sodium bicarbonate NaCl(s)+NH3(g)+CO2(g)+H2O(aq)-->NaHCO3(aq)+NH4Cl(s) Production of sodium carbonate, recycling of carbon dioxide 2NaHCO3(aq) + heat --> Na2CO3(aq) + H2O(aq) + CO2(g) Recycling of ammonia 2NH4Cl(s) + CaO(s) --> 2NH3(g) + CaCl2(s) + H2O(aq) Robert Angus Smith (1817-1884) Library and Information Centre, Royal Society of Chemistry Acidity Measure of the concentration of hydrogen ions (H+) in solution pH = -log10[H+] [H+] = molarity (M, moles of H+ per liter of solution) Higher [H+] --> lower pH --> more acidic solution (10.3) Acidity In dilute water, the only source of H+ is H2O(aq) Liquid water H+ + OHHydrogen Hydroxide ion ion [H+][OH-] = 10-14 M2 --> [H+]=[OH-]=10-7 M --> pH = -log10[10-7M] = 7 (10.4) Acid/Base Acid Substance that, when added to a solution, dissociates, increasing [H+], decreasing pH Strong acid: Substances that dissociate readily (e.g., H2SO4, HCl, HNO3) Weak acids: Substances that dissociate less readily (e.g., H2CO3) Base (alkalis) Substances that, when added to a solution, reduce [H+], increasing pH. (e.g., NH3(aq), Ca(OH)2(aq)) pH Scale Acid rain, fog (2-5.6) pH 0 1 2 Battery Lemon acid juice (1.0) (2.2) 3 Natural rainwater (5-5.6) 4 Apples (3.1) Vinegar CH3COOH(aq) (2.8) More acidic 5 6 Sea water (7.8-8.3) 7 8 9 10 Distilled water (7.0) Milk (6.6) Baking soda NaHCO3(aq) (8.2) 11 12 13 14 Ammonium Lye hydroxide NaOH(aq) NH4OH(aq) (13.0) (11.1) Slaked lime Ca(OH)2(aq) (12.4) More basic or alkaline Figure 10.3 pH of Food Lime Lemon Apple Apple juice Tomato juice Buttermilk Banana Cheddar cheese Beef Cabbage Asparagus Milk Crab Egg white 1.9 2.1-2.2 2.9-3.3 4.0 4.4 4.5 4.6 5.3 5.5 5.7 5.9 6.4-6.6 7.0 8.0 Acid Dissociation Addition of acid to solution increases [H+], decreasing pH Carbonic acid CO2(aq) + H2O(aq) Dissolved Liquid carbon dioxide water H2CO3(aq) Dissolved carbonic acid H+ + HCO32H+ + CO32Hydrogen Bicarbonate Hydrogen Carbonate ion ion ion ion Sulfuric acid H2SO4(g) Sulfuric acid gas H2SO4(aq) Dissolved sulfuric acid H+ + HSO4Hydrogen Bisulfate ion ion 2H+ + SO42Hydrogen Sulfate ion ion (10.5) - (10.6) Acid Dissociation Hydrochloric acid HCl(g) HCl(aq) H+ + ClHydrogen Chloride Hydrochloric Dissolved ion ion acid gas hydrochloric acid Nitric acid HNO3(g) Nitric acid gas HNO3(aq) Dissolved nitric acid H+ + NO3Hydrogen Nitrate ion ion (10.7) - (10.8) S(IV) and S(VI) Families S(IV) Family Sulfur dioxide SO2(g,aq) S(VI) Family S O O O O Sulfurous acid H2SO3(aq) S HO OH O Bisulfite ion HSO3- S HO Sulfite ion SO32- Table 10.1 O O S O O Sulfuric acid H2SO4(g,aq) O Bisulfate ion HSO4- O Sulfate ion SO42- S OH OH O S O OH O O S O O Mechanisms of Converting S(IV) to S(VI) Why is converting to S(VI) important? It allows sulfuric acid to enter or form within cloud drops and aerosol particles, increasing their acidity Mechanisms 1. Gas-phase oxidation of SO2(g) to H2SO4(g) followed by condensation of H2SO4(g) 2. Dissolution of SO2(g) into liquid water to form H2SO3(aq) and its dissociation products, which convert chemically to H2SO4(aq) and its dissociation products. Gas-Phase Oxidation of S(IV) to S(VI) + OH(g), M SO 2(g) HSO3(g) Sulfur dioxide Bisulfite + O2(g) HO2(g) + H2O(g) SO 3(g) H2SO 4(g) Sulfur trioxide Sulfuric acid (10.9) Aqueous-Phase Oxidation of S(IV) Step 1. S(IV) dissolution and dissociation SO2(g) SO2(aq) Sulfur dioxide gas Dissolved sulfur dioxide SO 2(aq) + H2O(aq) H2SO 3(aq) Dissolved Liquid sulfur water dioxide Sulfurous acid H+ + HSO3Hydrogen Bisulfite ion ion 2H+ + SO32Hydrogen Sulfite ion ion (10.10) - (10.11) Aqueous-Phase Oxidation of S(IV) Step 2. S(IV) oxidation by hydrogen peroxide in solution HSO3- + H2O2(aq) + H+ Bisulfite Dissolved ion Hydrogen peroxide SO42- + H2O(aq) + 2H+ Sulfate ion Alternate Step 2. S(IV) oxidation by ozone in solution SO 32- + O3(aq) Sulfite ion Dissolved ozone SO 42- + O2(aq) Sulfate Dissolved ion oxygen (10.12) - (10.13) Production of Nitric Acid Gas M OH(g) + NO2(g) Hydroxyl Nitrogen radical dioxide HNO3(g) Nitric acid (10.14) Effects of Acid Deposition Lakes and streams Lake pH decreased 1 pH unit between the 1950s and 1960s in Scandinavia. 25,000 out of 90,000 lakes in Sweden were acidified in the 1970s. 17,000 of these were due to anthropogenic pollution. Fish and microorganisms are sensitive to pH. Plants Acids damage trees at their roots and erodes cuticle wax. Acidified water carries away minerals. Acids release metals Al3+, Fe3+ from the minerals Al(OH)3(s), Fe(OH)3(s). Metals are toxic to roots. Prunerov Power Plant, Sulfur Triangle, 2005 www.chmi.cz Dead Norway Spruce, Bohemian Forest, Czech Republic, 2005 www.chmi.cz Dead Norway Spruce, Nacetin Forest, Czech Republic, 1995 www.chmi.cz Dead Spruce, Mt. Mumlava, Czech Republic www.chmi.cz Acidified forest near Most, Czechoslovakia (1987) Owen Bricker, United States Geological Survey Acidified Forest, Oberwiesenthal, Germany (1991) Stefan Rosengren/Naturbild Acidified Creek, New South Wales, 2007 www.ramsar.org Neutralizing Acids Add ammonium hydroxide to a lake NH4OH(aq) + H+ Ammonium Hydrogen hydroxide ion NH4+ + H2O(aq) Ammonium Liquid ion water Add slaked lime to a lake Ca(OH)2(aq) + 2H+ Calcium Hydrogen hydroxide ion Ca2+ + 2H2O(aq) Calcium Liquid ion water Calcium carbonate is a natural neutralizing agent in soil CaCO3(s) + 2H+ Calcium Hydrogen carbonate ion Ca2+ + CO2(g) + H2O(aq) Calcium Carbon Liquid ion dioxide water gas (10.15) - (10.17) Liming of a Lake in Sweden Tero Niemi / Naturbild Neutralizing Acids Sea salt is a natural neutralizing agent near the coast NaCl(s) + H+ Sodium Hydrogen chloride ion Na+ + HCl(g) Sodium Hydrochloric ion acid Ammonia is a neutralizing agent NH3(aq) + H+ Dissolved Hydrogen ammonia ion NH4+ Ammonium ion (10.19) - (10.20) Visibility Trend Sulfur Triangle Stjern et al. (2011) 1994 U.S. Rainwater pH 2009 U.S. National Atmospheric Deposition Program/National Trends Network Effects of Acid Deposition Materials The addition of sulfuric acid to marble or limestone produces gypsum, which forms a crust that creates pits when rain loosens the crust. Crusting of marble and limestone CaCO3(s) + 2H+ Ca2+ + CO2(g) + H2O(aq) Calcium Hydrogen Calcium Carbon Liquid carbonate ion ion dioxide water gas CaSO 4-2H2O(s) Ca2+ + SO42- + 2H2O(aq) Calcium Sulfate Liquid Calcium sulfate ion ion water dihydrate (gypsum) (10.17) - (10.18) Cathedral of Learning, Pittsburgh, 1930 and 1934 University Archives, University of Pittsburgh Sandstone Figure in 1908 and 1968, Westphalia, Germany Herr Schmidt-Thomsen Recent Regulation of Acid Deposition 1970. U.S. Clean Air Act Amendments 1977. U.S. National Atmospheric Deposition Program 1979. Geneva Convention on Long-Range Transboundary Air Pollution 1985. Sulfur Protocol 1988. Nitrogen Oxide Protocol 1990. U.S. Clean Air Act Amendments 1994. Second Sulfur Protocol Methods of Controlling Emission Use of low-sulfur coal Remove sulfur from high-sulfur coal Advanced scrubbers (e.g., flue-gas desulfurization)