Air & Air Pollution See what you know • What is in the air? • What is the difference between Global Warming and Climate Change? • What causes Climate Change? • What are the effects of Climate Change? • What caused the hole in the ozone layer? Choosing sides • Whether climate change is occurring or not, isn’t it better to be on the side that believes it is happening? How can changing our ways be a bad thing? Isn’t it better to error on the true side? • Human-caused climate change is happening, ..It is happening faster than anyone predicted even a few years ago, and therefore we need to remind ourselves and negotiators need to remind themselves that the longer we delay, the more we will pay, both in terms of lives and in terms of money. • - Robert Orr, a top UN official The Atmosphere Greenhouse gasses Atmospheric Gases Atmospheric pressure (millibars) Temperature Pressure Thermosphere Mesosphere Heating via ozone Stratopause Stratosphere Altitude (miles) Altitude (kilometers) Mesopause Tropopause Ozone “layer” Heating from the earth Troposphere (Sea level) Temperature (˚C) Pressure = 1,000 millibars at ground level • Inches of Hg • 1 atm = 29.92 Inches of Hg 1atm = 29.92 Inches of Hg 1 atm = 14.696 lb/in2 The Atmosphere in layers Troposphere – – – – Layer in which we live Most weather occurs here 90% of the gasses are here 0-6 mile above N and S Pole • Mount Everest is 5.3 miles tall – 0-10 miles above equator – is made up mostly of nitrogen and oxygen, with smaller amounts of water vapor and CO2 • Stratosphere – 6-10 mile thick – Air traffic due to lack of weather – Ozone layer • Thermosphere – 50 miles to space “Good” Ozone Layer • Ozone (O3) is a gas that occurs both in the Earth's upper atmosphere and at ground level. Ozone can be "good" or "bad" for your health and the environment, depending on its location in the atmosphere. • How much of our atmosphere is ozone? • Ozone that surrounds the earth 12-35 miles above the earth is our first line of defense of the sun’s ultraviolet radiation. UVA, UVB, UVC – This radiation can cause sunburn, skin cancer, cataracts, … • Ozone is constantly created and destroyed Humans need a small amount of ultraviolet radiation to maintain health. Ultraviolet radiation activates vitamin D in the human body, which assists the intestines in absorbing minerals. Humans, as well as other life forms, can tolerate radiation through the UVA range, but radiation with shorter wavelengths, such as UVB and UVC is harmful. Oxygen molecules absorb the shortest and most harmful UVC radiation and ozone absorbs most of the remainder before it reaches the earth’s surface. Ozone, a molecule containing three oxygen atoms, is made when the shortest wavelengths of UVC are absorbed by oxygen and break apart into two oxygen atoms. What Happens to Solar Energy Reaching the Earth? • Solar energy flowing through the biosphere warms the atmosphere, evaporates and recycles water, generates winds and supports plant growth. Figure 3-8 Why is a sunset red? Refraction – of light as it passes through atmosphere and collides with atmospheric gasses. Colors are filtered out and scattered. The Natural Greenhouse Effect • Three major factors shape the earth’s climate: – The sun. – Greenhouse effect that warms the earth’s lower troposphere and surface because of the presence of greenhouse gases. – Oceans store CO2 and heat, evaporate and receive water, move stored heat to other parts of the world. – Natural cooling process through water vapor in the troposphere (heat rises). Major Greenhouse Gases • The major greenhouse gases in the lower atmosphere are water vapor(.04%), carbon dioxide (.0369%), methane(.00018%), and nitrous oxide(.0000315%), ozone (.000005%) – These gases have always been present in the earth’s troposphere in varying concentrations. – Fluctuations in these gases, plus changes in solar output are the major factors causing the changes in tropospheric temperature over the past 400,000 years. Greenhouse Effect • This “greenhouse effect” is vital for our survival. Without heat trapping gasses our planet would be cold and lifeless. • The gasses act like a car that gets hot inside. Albedo - %age of incoming sunlight reflected from a surface Air Pollution – The Big 5 • Air Pollutant is defined as any substance in the air that is concentrated enough to harm living things or to cause damage to man-made objects. • Primary pollutants – released directly into air. • Secondary pollutants – primary pollutants react with other components. Primary Pollutants CO CO2 SO2 NO NO2 Most hydrocarbons - VOCs Most suspended particles Sources Natural Secondary Pollutants SO3 HNO3 H3SO4 H2O2 O3 PANs Most NO3– and SO42– salts Stationary Mobile Fig. 19-3, p. 442 Point Source / Nonpoint Source Human Actions and Our Environment • When the human population was low, there was very little impact to the environment. – Wind, rain, and time were the natural air cleaners. • As the human population increased, time could not clean the air fast enough. • Deforestation removes CO2 cleaners. Human Actions and Our Environment • The burning of fossil fuels -- notably coal, oil and gas -has accounted for about 80 percent of the rise of atmospheric carbon dioxide since the pre-industrial era. Humans have been burning fossil fuel for 400 years adding an enormous unnatural amount of carbon dioxide and other gases in the air. The human impact has changed three major ecosystem cycles. • 1. – – – The chemical cycles Carbon Cycle Nitrogen Cycle Sulfur Cycle – By adding more chemicals we change the cycle Air Pollution – The Big 5 1. Carbon oxides • • 2. High levels can suffocate you blood Put out by automobiles and fires Unburned Hydrocarbons - VOCs • • • 3. Combustion of gas Oil based paint, dry cleaning fluids, petroleum fuels Methane stores 25 x more energy than CO2. Nitrogen Oxides • • • • Nitrogen alone is Ok, but at high temps. It reacts with oxygen to form NOx Makes the sky Brown in smog Photchemical smog – nitrogen and light form “bad “ozone” PANs – Peroxyacyl nitrates Air Pollution – The Big 5 • 4. Sulfur Oxides – Naturally occurring • Volcanoes – Burning of coal, oil, gas (cars) – Cause Lung damage, asthma, and bronchitis – Combines with hydrogen to make Sulphuric Acid (ACID RAIN) • 5. Particulates • - PM10 – smaller than 10 um – human hair is about 50-100 um – Small solid particles or liquid droplets in the air • Light enough to float in air • Dust, lead, mercury, radon, ash from fires, road dust, exhaust, wind erosion, • Lung irritant, stain buildings, reduce visibility Major Air Pollutants • Carbon oxides – CO , CO2: – CO2 (10,000 ppm) will make some people feel drowsy. Exhaling into a bag is about 37,000 ppm. – Carbon oxides are highly toxic gasses that form during the incomplete combustion of carboncontaining materials. – 93% of carbon dioxide (CO2) in the troposphere occurs as a result of the carbon cycle. – 7% of CO2 in the troposphere occurs as a result of human activities (mostly burning fossil fuels). – CO2 is a greenhouse gas Major Air Pollutants • Nitrogen oxides and nitric acid: – Nitrogen oxide (NOx) forms when nitrogen and oxygen gas in air react at the highcombustion temperatures in automobile engines and coal-burning plants. NO can also form from lightening and certain soil bacteria. – Photochemical Smog • NO reacts with air to form NO2. • NO2 reacts with water vapor in the air to form nitric acid (HNO3) and nitrate salts (NO3-) which are components of acid deposition. The Nitrogen Cycle: The first thing that starts the chain of events is that people start driving in the morning. As gasoline is burned, nitrogen (N2) in the atmosphere is also burned, or oxidized, forming nitric oxide (NO) N2 + O2=2NO Hydrocarbons and carbon monoxide (CO) will also be emitted by cars. Hydrocarbons are volatile organic compounds that may include acetaldehyde, formaldehyde, ethylene, and many other compounds. In the air, nitric oxide combines with molecular oxygen to form nitrogen dioxide within a few hours. 2NO + O2--------->2NO2 Nitrogen dioxide absorbs light energy and splits to form nitric oxide and atomic oxygen: NO2-->NO + O Then, in sunlight, the atomic oxygen combines with oxygen gas to form ozone (O3): O+ O2--->O3 If no other factors are involved, ozone and nitric oxide then react to form nitrogen dioxide and oxygen gas. O3 + NO<------>NO2 + O2 This last reaction can go in either direction, depending on temperature and the amount of sunlight. If there is a lot of sunlight, the equation moves to the left, and more ozone is produced. If nothing else gets in the way, an equilibrium is reached, and the ozone level stabilizes. However, there is something else involved. Remember that the cars are also emitting hydrocarbons as well as oxides of nitrogen. Hydrocarbons are the other main ingredient in photochemical smog. When hydrocarbons are present, nitric oxide reacts with them instead of the ozone. This reaction produces a variety of toxic products, such as a volatile compound known as PAN (peroxyacetyl nitrate). NO + hydrocarbons----------------->PAN and various other compounds. Also, NO2 +hydrocarbons------------------>PAN and various other compounds Major Air Pollutants • Volatile organic compounds (VOCs): – Most are hydorcarbons emitted by the leaves of many plants. – About two thirds of global methane CH4 emissions comes from human sources. – Other VOCs include industrial solvents such as trichlorethylene (TCE), benzene, and vinyl chloride, hundreds more. • Long-term exposure to benzene can cause cancer, blood disorders, and immune system damage. Methane CH4 • About 25x stronger GHG than CO2. • 1/3rd of methane emissions come from natural sources, mostly plants, wetlands, termites, anaerobic decomposition. • The rest comes from human sources such as rice paddies, landfills, oil and natural gas wells, and cows (from belching or flatulence). Major Air Pollutants • Ozone (O3): – “bad” ozone - found in troposphere – Is a highly reactive gas that is a major component of photochemical smog. – It can • Cause and aggravate respiratory illness such as asthma • Can aggravate heart disease. • Damage plants What Causes "Bad" Ozone? Ground-level or "bad" ozone is not emitted directly into the air, but is created by chemical reactions VOC + NOx + Sunlight = Ozone (O3) Emissions from industrial facilities and electric utilities, motor vehicle exhaust, gasoline vapors, and chemical solvents are some of the major sources of NOx and VOC. Ozone Action Days • Usually occur days that are: – – – – Relatively Hot Dry Clear Little to no wind • Ozone action days can be predicted Major Air Pollutants • Sulfur dioxide (SO2) and sulfuric acid: – About one-third of SO2 in the troposphere occurs naturally through the sulfur cycle. – Two-thirds come from human sources, mostly combustion (S+ O2 SO2) of sulfurcontaining coal and from oil refining and smelting of sulfide ores. – SO2 in the atmosphere can be converted to sulfuric acid (H2SO4) and sulfate salts (SO42-) that return to earth as a component of acid deposition. Sulfur in from burning of fuels. • Combustion of gas in automobiles releases sulfur. • Burning of coal releases sulfur. The United States creates a great majority of its electricity by burning coal. The Sulfur Cycle Figure 3-32 ACID DEPOSITION • Sulfur dioxides, nitrogen oxides, and particulates can react in the atmosphere to produce acidic chemicals that can travel long distances before returning to the earth’s surface. – Tall smokestacks reduce local air pollution but can increase regional air pollution. Acid Deposition • AKA Acid Rain • Rain cleans the air, but pollutes the water. • Normal rainwater has a pH of 5.6 (slightly acidic). This is because it is exposed to the carbon dioxide in the atmosphere. The carbon dioxide gets dissolved in the rainwater and forms carbonic acid (H{-2}CO{-3}). Acid Rain is anything below 5.6. • Plants like to grown in soil with a pH of 6-7 • What happens to the plants? ACID RAIN Wind Transformation to sulfuric acid (H2SO4) and nitric acid (HNO3) Nitric oxide (NO) Windborne ammonia gas and particles of cultivated soil partially neutralize acids and form dry sulfate and nitrate salts Sulfur dioxide (SO2) and NO Acid fog Dry acid deposition (sulfur dioxide gas and particles of sulfate and nitrate salts) Farm Ocean Lakes in deep soil high in limestone are buffered Wet acid depostion (droplets of H2SO4 and HNO3 dissolved in rain and snow) Lakes in shallow soil low in limestone become acidic Fig. 19-6, p. 448 ACID DEPOSITION • pH measurements in relation to major coal-burning and industrial plants. ACID DEPOSITION • Air pollution is one of several interacting stresses that can damage, weaken, or kill trees and pollute surface and groundwater. ACID DEPOSITION • Acid deposition contributes to chronic respiratory disease and can leach toxic metals (such as lead and mercury) from soils and rocks into acidic lakes used as sources for drinking water. Solutions Acid Deposition Prevention Reduce air pollution by improving energy efficiency Cleanup Add lime to neutralize acidified lakes Reduce coal use Increase natural gas use Increase use of renewable energy resources Add phosphate fertilizer to neutralize acidified lakes Burn low-sulfur coal Remove SO2 particulates & NOx from smokestack gases Remove NOx from motor vehicular exhaust Tax emissions of SO2 Fig. 19-10, p. 452 Major Air Pollutants • Suspended particulate matter (SPM): – Consists of a variety of solid particles and liquid droplets small and light enough to remain suspended in the air. – The most harmful forms of SPM are fine particles (PM-10, with an average diameter < 10 micrometers) and ultrafine particles (PM2.5). – According to the EPA, SPM is responsible for about 60,000 premature deaths a year in the U.S. SPMs • • • • • Lead Mercury Pollen Soil Liquids What is Happening to the "Good" Ozone Layer? Ozone is produced naturally in the stratosphere. But this "good" ozone is gradually being destroyed by man-made chemicals referred to as ozone-depleting substances (ODS), including chlorofluorocarbons (CFCs), hydrochlorofluorocarbons (HCFCs), halons, methyl bromide, carbon tetrachloride, and methyl chloroform. These substances were formerly used and sometimes still are used in coolants, foaming agents, fire extinguishers, solvents, pesticides, and aerosol propellants (propane). Atmospheric pressure (millibars) Temperature Pressure Thermosphere Heating via ozone Mesosphere Stratopause Stratosphere Altitude (miles) Altitude (kilometers) Mesopause Tropopause Ozone “layer” Heating from the earth Troposphere (Sea level) Temperature (˚C) Pressure = 1,000 millibars at ground level Fig. 19-2, p. 440 Ozone • CFC – Chlorofluorocarbons react with an oxygen atom to break down O3 to O2. • 1 chlorine can destroy 100,000 ozone molecules • As ozone is broken down, the ozone layer gets thinner. – This radiation that gets through can cause sunburn, skin cancer, cataracts, … Ultraviolet light hits a chlorofluorocarbon (CFC) molecule, such as CFCl3, breaking off a chlorine atom and leaving CFCl2. Sun Cl UV radiation The chlorine atom attacks an ozone (O3) molecule, pulling an oxygen atom off it and leaving an oxygen molecule (O2). Summary of Reactions CCl3F + UV Cl + CCl2F Cl + O3 ClO + O2 Repeated Cl + O Cl + O2 many times Once free, the chlorine atom is off to attack another ozone molecule and begin the cycle again. A free oxygen atom pulls the oxygen atom off the chlorine monoxide molecule to form O2. The chlorine atom and the oxygen atom join to form a chlorine monoxide molecule (ClO). Fig. 20-18, p. 486 OZONE DEPLETION IN THE STRATOSPHERE • Since 1976, in Antarctica, ozone levels have markedly decreased during October and November. Figure 20-20 Natural Capital Degradation Effects of Ozone Depletion Human Health • Worse sunburn • More eye cataracts • More skin cancers • Immune system suppression Food and Forests • Reduced yields for some crops • Reduced seafood supplies from reduced phytoplankton • Decreased forest productivity for UV-sensitive tree species Wildlife • Increased eye cataracts in some species • Decreased population of aquatic species sensitive to UV radiation • Reduced population of surface phytoplankton • Disrupted aquatic food webs from reduced phytoplankton Air Pollution and Materials • Increased acid deposition • Increased photochemical smog • Degradation of outdoor paints and plastics Fig. 20-21, p. 488 Global Warming • Accelerated warming because of decreased ocean uptake of CO2 from atmosphere by phytoplankton and CFCs acting as greenhouse gases Montréal Protocol • The Montreal Protocol, adopted in 1987, required nations to freeze production levels of CFCs. Additional agreements enacted since 1987 accelerated the CFC phase out timetable to December 31, 1995. • Atmospheric concentrations of chlorofluorocarbons peaked in 1994 and began to decrease in 1995, marking the first time that a atmospheric concentrations of chlorine began to decrease. Chlorine concentrations in July 2002, were about 5% less than the 1994 peak. However, the amount of atmospheric bromine continues to increase, albeit at a slower rate. What Can You Do? Reducing Exposure to UV Radiation • Stay out of the sun, especially between 10 A.M. and 3 P.M. • Do not use tanning parlors or sunlamps. • When in the sun, wear protective clothing and sun– glasses that protect against UV-A and UV-B radiation. • Be aware that overcast skies do not protect you. • Do not expose yourself to the sun if you are taking antibiotics or birth control pills. • Use a sunscreen with a protection factor of 15 or 30 anytime you are in the sun if you have light skin. • Examine your skin and scalp at least once a month for moles or warts that change in size, shape, or color or sores that keep oozing, bleeding, and crusting over. If you observe any of these signs, consult a doctor immediately. Fig. 20-23, p. 490 Topography and Pollution • Geography can effect pollution concentrations. • Mountainous areas tend to trap pollution • Flat areas tend to allow pollution to disperse • Forest Fires in the Los Angeles area. • Winds carry the smoke across the ocean. • Wind can clean the air, but it can also spread it somewhere else. China Air Pollution • A regions air pollution can become a global problem. Temperature Inversion • Cold air is more dense. Sometimes when it sinks below the warm air, it brings the pollution with it. Temperature Inversions • Cold, cloudy weather in a valley surrounded by mountains can trap air pollutants (left). • Areas with sunny climate, light winds, mountains on three sides and an ocean on the other (right) are susceptible to Figure 19-5 How does air quality effect me? • • • • • • • Asthma Emphysema Allergies Heart disease Drink polluted water Colds Pneumonia National Ambient Air Quality Standards (NAAQS) • Sets acceptable concentrations for 6 “criteria” pollutants that: – Threaten public health/the environment over broad areas (non-point) – Are emitted in large quantities – CO, Pb, Nitrogen Oxides, Ozone, Particulate Matter and Sulfur Dioxides HEALTH EFFECTS OF AIR POLLUTION • Your respiratory system can help protect you from air pollution, but some air pollutants can overcome these defenses. Figure 19-14 Air Pollution is a Big Killer • Each year, air pollution prematurely kills about 3 million people, mostly from indoor air pollution in developing countries. – In the U.S., the EPA estimates that annual deaths related to indoor and outdoor air pollution range from 150,000 to 350,000. HEALTH EFFECTS OF AIR POLLUTION Normal human lungs (left) and the lungs of a person who died of emphysema (right). Figure 19-15 Air Pollution is a Big Killer • Spatial distribution of premature deaths from air pollution in the United States. Figure 19-16 Clean Air Act • • • • 1963 - first passage 1970, 1977 and 1990 - amended Involves EPA Sets standards for acceptable levels of sulfur oxides, nitrogen oxides, ozone, carbon monoxide, hydrocarbons, lead, PANs, particulate matter & more. Does not regulate CO2. • Provides pollution credits (subsidies) for industries that utilize pollution-control devices+ • Bush administration has relaxed rules • Does not regulate 2&4 cycle small engines PREVENTING AND REDUCING AIR POLLUTION • Environmental scientists point out several deficiencies in the Clean Air Act: – The U.S. continues to rely on cleanup rather than prevention. – The U.S. Congress has failed to dramatically increase fuel-efficiency standards for automobiles. – Regulation of emissions from motorcycles and twocycle engines remains inadequate. – There is little or no regulation of air pollution from oceangoing ships in American ports. PREVENTING AND REDUCING AIR POLLUTION • Executives of companies claim that correcting these deficiencies would cost too much, harm economic growth, and cost jobs. What Is Being Done About "Bad" Ozone? Under the Clean Air Act, EPA has set protective health-based standards for ozone in the air we breathe. EPA, state, and cities have instituted a variety of multi-faceted programs to meet these healthbased standards. Throughout the country, additional programs are being put into place to cut NOx and VOC emissions from vehicles, industrial facilities, and electric utilities. Programs are also aimed at reducing pollution by reformulating fuels and consumer/commercial products, such as paints and chemical solvents, that contain VOC. PCBs • Polychlorinated biphenyls (PCBs) were widely used as dielectric and coolant fluids. Due to PCBs' environmental toxicity and classification as a persistent organic pollutant, PCB production was banned by the United States Congress in 1979 and by the Stockholm Convention on Persistent Organic Pollutants in 2001. • A number of peer-reviewed health studies have shown an association between exposure to PCBs and non-Hodgkin Lymphoma, a frequently fatal form of cancer • Concerns about the toxicity of PCBs are largely based on compounds within this group that share a structural similarity and toxic mode of action with dioxin. Toxic effects such as endocrine disruption and neurotoxicity are also associated with other compounds within the group. Solutions: Reducing Outdoor Air Pollution • There are a of ways to prevent and control air pollution from motor vehicles. – Because of the Clean Air Act, a new car today in the U.S. emits 75% less pollution than it did pre-1970 cars. – There is an increase in motor vehicle use in developing countries and many have no pollution control devices and burn leaded gasoline. Solutions Motor Vehicle Air Pollution Prevention Mass transit Cleanup Emission control devices Bicycles and walking Less polluting engines Less polluting fuels Improve fuel efficiency Car exhaust inspections twice a year Get older, polluting cars off the road Give buyers large tax write-offs or rebates for buying low-polluting, energy efficient vehicles Stricter emission standards Fig. 19-19, p. 460 Solutions: Reducing Outdoor Air Pollution • There are a of ways to prevent and control air pollution from coal-burning facilities. – Electrostatic precipitator: are used to attract negatively charged particles in a smokestack into a collector. – Wet scrubber: fine mists of water vapor trap particulates and convert them to a sludge that is collected and disposed of usually in a landfill. Electrostatic Precipitator • Can remove 99% of particulate matter • Does not remove hazardous ultrafine particles. • Produces toxic dust that must be safely disposed of. • Uses large amounts of electricity Figure 19-18 Wet Scrubber • Can remove 98% of SO2 and particulate matter. • Not very effective in removing hazardous fine and ultrafine particles. Figure 19-18