Chemistry and the Environment Learning Objectives a. The environment consists of the lithosphere, the atmosphere, and the hydrosphere. b. The lithosphere serves as the source for raw materials and energy resources such as fossil fuels. c. Depletion of traditional fuel sources is leading to the need for alternative/renewable fuels. d. Solid waste disposal is a growing burden on the lithosphere. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 2 Learning Objectives (cont) e. The atmosphere is suffering from increased levels of pollutants. f. Increasing atmospheric CO2 levels have been linked to global warming through an enhancement of the greenhouse effect. g. The Earth’s sunscreen, the ozone layer, has been damaged by chlorofluorocarbons. h. During the hydrologic cycle, rainwater can pick up many pollutants. i. Acid rain can also result from the reaction of H2O with atmospheric SO3 and NO2. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 3 Outline • Overview of the Environment a. Lithosphere 1. The solid surface of the Earth b. Atmosphere 1. The gaseous layer of air surrounding the Earth c. Hydrosphere 1. The aqueous part of the Earth Copyright © Houghton Mifflin Company. All rights reserved. 15 | 4 Outline • The Lithosphere a. Traditional Energy Resources 1. Traditional sources of energy have included biomass and fossil fuels. 2. More recently, nuclear power has become an option. 3. Supplies of fossil fuels and uranium are limited. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 5 Evolution of fuel use Copyright © Houghton Mifflin Company. All rights reserved. 15 | 6 Composition and Energy Content of Various Fuels Copyright © Houghton Mifflin Company. All rights reserved. 15 | 7 Global Reserves of Fuels Copyright © Houghton Mifflin Company. All rights reserved. 15 | 8 Carbon and Heat Content by Type of Coal Copyright © Houghton Mifflin Company. All rights reserved. 15 | 9 Coal mining often leaves environmental disaster in its wake Copyright © Houghton Mifflin Company. All rights reserved. 15 | 10 The refining and separation process Copyright © Houghton Mifflin Company. All rights reserved. 15 | 11 Outline • The Lithosphere (cont) b. Alternative Sources of Energy 1. Depletion of traditional sources of energy such as petroleum has led to the development of alternative sources of energy. 2. Renewable energy sources can be replenished on a short time scale; e.g., solar power and biomass. 3. Example: photovoltaic cells (PVCs), which convert solar energy into electricity. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 12 Schematic of a “pressurized water” type of nuclear reactor Copyright © Houghton Mifflin Company. All rights reserved. 15 | 13 Different types of semiconductors Copyright © Houghton Mifflin Company. All rights reserved. 15 | 14 Photovoltaic Cells Copyright © Houghton Mifflin Company. All rights reserved. 15 | 15 Outline • Lithosphere (cont) b. Alternative Energy Sources (cont) 4. Fuel cells generate electricity through an oxidation-reduction reaction for which the reactants are constantly supplied. 5. An example is the Proton Exchange Membrane (PEM) fuel cell based on the following reaction: 2 H2 + O2 Copyright © Houghton Mifflin Company. All rights reserved. 2 H2O + energy 15 | 16 In a PEM fuel cell, H2 is split into H+ and electrons Copyright © Houghton Mifflin Company. All rights reserved. 15 | 17 Outline • The Lithosphere (cont) c. Land Pollution 1. Solid waste disposal is a growing problem. 2. The Environmental Protection Agency (EPA) recommends that we “reduce, reuse, and recycle.” Copyright © Houghton Mifflin Company. All rights reserved. 15 | 18 Solid Waste Generated by Americans in 2003 Copyright © Houghton Mifflin Company. All rights reserved. 15 | 19 Composting Copyright © Houghton Mifflin Company. All rights reserved. 15 | 20 Municipal solid waste recycling rates, 1960-2003 Source: EPA Copyright © Houghton Mifflin Company. All rights reserved. 15 | 21 The Atmosphere Copyright © Houghton Mifflin Company. All rights reserved. 15 | 22 The atmosphere is divided into five layers. It is thickest near the surface and thins out with height until it eventually merges with space. 1) The troposphere is the first layer above the surface and contains half of the Earth's atmosphere, which we breathe. Weather occurs in this layer. 2) Many jet aircraft fly in the stratosphere because it is very stable. Also, the ozone layer absorbs harmful rays from the Sun. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 23 Atmosphere, continued 3) Meteors or rock fragments burn up in the mesosphere. 4) The thermosphere is a layer with auroras. It is also where the space shuttle orbits. 5) The atmosphere merges into space in the extremely thin exosphere. This is the upper limit of our atmosphere. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 24 Copyright © Houghton Mifflin Company. All rights reserved. 15 | 25 Composition of Dry Air at Sea Level Copyright © Houghton Mifflin Company. All rights reserved. 15 | 26 Outline • The Atmosphere a. The Nitrogen Cycle 1. The atmosphere at sea level is comprised of 78% N2 and 21% O2. 2. The nitrogen cycle is the exchange of nitrogen atoms between the living and non-living parts of the environment. 3. During nitrogen fixation, atoms from atmospheric N2 are incorporated into biologically useful nitrogencontaining molecules. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 27 The Nitrogen Cycle Copyright © Houghton Mifflin Company. All rights reserved. 15 | 28 Nitrogen-Fixation Reactions Copyright © Houghton Mifflin Company. All rights reserved. 15 | 29 Outline • The Atmosphere (cont) b. Air Pollutants 1. Pollutants (chemicals in the wrong place at the wrong concentration) can occur naturally or from human activity. 2. EPA’s six major air pollutants are SO2, particulate matter (PM), CO, NOx, O3, and Pb. 3. Depending on atmospheric conditions, pollution can result in industrial smog or photochemical smog. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 30 EPA’s Principal (Primary) Air Pollutants Copyright © Houghton Mifflin Company. All rights reserved. 15 | 31 Secondary pollutants are formed in the atmosphere through chemical and photochemical reactions from the primary pollutants examples include: sulfuric acid H2SO4 - can cause respiratory problems nitrogen dioxide NO2 - gives air a brownish coloration ozone O3 - colorless gas, has a sweet smell, is an oxidizing agent, irritates the eyes Copyright © Houghton Mifflin Company. All rights reserved. 15 | 32 Photochemical Smog Copyright © Houghton Mifflin Company. All rights reserved. 15 | 33 Sunlight + emissions from cars and power plants = photochemical smog N2 + O2 2NO Created by forest fires and the combustion engine NO + O2 NO2 (a corrosive brown gas) 4 NO2 + 2H2O + O2 4 HNO3 (nitric acid) Copyright © Houghton Mifflin Company. All rights reserved. 15 | 34 LA. smog: • requires clear, sunny skies • NOx + ROG + sunlight --> O3 + NO2 • ROG are reactive organic gases from unburned gasoline • NOx are oxides of nitrogen Copyright © Houghton Mifflin Company. All rights reserved. 15 | 35 Review the Components of Photochemical Smog Copyright © Houghton Mifflin Company. All rights reserved. 15 | 36 Industrial Smog The Source: Burning Coal Thermal Inversion, in which a blanket of warm air above a low lying layer of cooler air traps pollutants (SO2, CO, NO2) near the ground. Production of Sulfur compounds that arise from coal combustion originates with the release of sulfur within the coal as sulfur dioxide: S + O2 SO2 Which is a choking gas in its own right, reacts further with atmospheric O2, which forms sulfur trioxide and combines with water vapor to form sulfuric acid (H2SO4) 2SO2 + O2 SO3 + H2O H2SO4 Contributes to acid rain Copyright © Houghton Mifflin Company. All rights reserved. 15 | 37 A thermal inversion caused air pollution in London in the 1950s Thermal inversion occurs when a layer of warm air settles over a layer of cooler air that lies near the ground. The warm air holds down the cool air and prevents pollutants from rising and scattering. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 38 Air pollution at the Great Smoky Mountains National Park Copyright © Houghton Mifflin Company. All rights reserved. 15 | 39 Strategies to Reduce Photochemical Smog Reduce the number of automobiles on the road More efficient gasoline-dispensing systems to reduce the release of hydrocarbons into the atmosphere and catalytic converters to improve the efficiency of combustion, gas-electric hybrid vehicles, reduced tailpipe emissions, and fuel efficiency. Strategies to Reduce Industrial Smog Cut down on PM and sulfur compounds Scrubbers that pass emission gases through water and filters that act like vacuum cleaners and remove sulfur compounds through a chemical treatment with limestone (CaCO3): CaCO3(s) + SO2(g) CaSO3(s) + CO2(g) Copyright © Houghton Mifflin Company. All rights reserved. 15 | 40 Declining mean blood lead levels for U.S. children age 5 and younger Source: EPA Thomas Midgley Jr. invented Chlorofluorocarbons (CFCs) and tetraethyl lead Credit: Kettering University Copyright © Houghton Mifflin Company. All rights reserved. 15 | 42 Outline • The Atmosphere (cont) c. Global Climate Change (Global Warming) 1. The greenhouse effect is a warming of the Earth by a layer of gases that trap the sun’s energy. 2. Human activity appears to be causing an increase in the amount of atmospheric CO2. 3. Increased atmospheric CO2 appears to be enhancing the greenhouse effect, leading to an increase in average global temperatures. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 43 CO2 levels are still increasing in the atmosphere Source: National Oceanic and Atmospheric Administration (NOAA). Copyright © Houghton Mifflin Company. All rights reserved. 15 | 44 The Earth's atmosphere acts like the glass in a greenhouse Copyright © Houghton Mifflin Company. All rights reserved. 15 | 45 Rising global temperatures Source: NASA Copyright © Houghton Mifflin Company. All rights reserved. 15 | 46 Aerosols can block out solar radiation Copyright © Houghton Mifflin Company. All rights reserved. 15 | 47 Outline • The Atmosphere (cont) d. Ozone Depletion 1. Ozone forms the Earth’s sunscreen. 2. Chlorofluorocarbons, formerly used as propellants and refrigerants, break down in the upper atmosphere to form free radicals that degrade the ozone layer. CF2Cl2 + UV light Cl• + O3 ClO • + O CF2Cl + Cl• ClO • + O2 Cl• + O2 Copyright © Houghton Mifflin Company. All rights reserved. 15 | 48 Ozone hole over Antarctica, October 1979 Copyright © Houghton Mifflin Company. All rights reserved. 15 | 49 Ozone hole over Antarctica, October 1986 Copyright © Houghton Mifflin Company. All rights reserved. 15 | 50 Ozone hole over Antarctica, October 2005 Copyright © Houghton Mifflin Company. All rights reserved. 15 | 51 Outline • The Hydrosphere a. Hydrologic Cycle 1. Movement of water between the atmosphere, the lithosphere, and the hydrosphere 2. During the hydrologic cycle, water may pick up many pollutants. 3. An example is acid rain (pH < 5.6), resulting from formation of H2SO4 and HNO3 when water reacts with atmospheric combustion products SO2 and NO2. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 52 Average Daily Water Use per American Source: Data from the American Water Works Association. Copyright © Houghton Mifflin Company. All rights reserved. 15 | 53 Hydrologic Cycle Copyright © Houghton Mifflin Company. All rights reserved. 15 | 54 Hard-water deposits inside pipes and kettles Copyright © Houghton Mifflin Company. All rights reserved. 15 | 55 EPA's Permissible Mineral Levels in Water Copyright © Houghton Mifflin Company. All rights reserved. 15 | 56 Ion-exchange columns for removing Ca2+ and Mg2+ ions Copyright © Houghton Mifflin Company. All rights reserved. 15 | 57 Handheld water purifier Copyright © Houghton Mifflin Company. All rights reserved. Removal of both biological and chemical contaminants 15 | 58 Possible sources of contamination in the hydrologic cycle Water pollution Copyright © Houghton Mifflin Company. All rights reserved. 15 | 59 Acid rain is most severe in the Mid-Atlantic states Copyright © Houghton Mifflin Company. All rights reserved. 15 | 60 Acid Rain Acid rain is when the rain has a pH of 5.6 or lower due to the presence of atmospheric carbon dioxide, which reacts with water to form dissolved carbonic acid (H2CO3). CO2 + H2O H2CO3 SO2 further reacts with atmospheric O2, which forms sulfur trioxide and combines with water vapor to form sulfuric acid (H2SO4) 2SO2 + O2 SO3 + H2O H2SO4 Copyright © Houghton Mifflin Company. All rights reserved. 15 | 61 The Effect of Acid Rain on calcium carbonate over time Picture taken before acid rain at the Field Museum in Chicago in 1920 Copyright © Houghton Mifflin Company. All rights reserved. Picture taken after acid rain at the Field Museum in Chicago in 1990 15 | 62 Erosion increases in the absence of vegetation Credit: Alamy Copyright © Houghton Mifflin Company. All rights reserved. 15 | 63 A healthy lake (top) and one that is suffering from eutrophication Eutrophication occurs when a body of water is rich in nutrients that lead to an explosion of vegetation and algae at the expense of other aquatic life. Algae formed at the surface of the lake Copyright © Houghton Mifflin Company. All rights reserved. 15 | 64 An oiled bird after the Exxon Valdez accident Credit: AP/Wide World Photos Copyright © Houghton Mifflin Company. All rights reserved. 15 | 65