Air quality issues The Atmosphere Atmospheric layers The atmosphere is composed of layers as shown in the diagrams below: Layers of the atmosphere Temperature profile of atmosphere Stratosphere The stratosphere is the layer above the troposphere. Here the temperature increases slightly versus height. Contained in the lower part of the stratosphere is the ozone layer. This ozone absorbs ultraviolet (UV) radiation: O3 + hν → O2 + O → O3 Thus the ozone protects the Earth from dangerous ultraviolet radiation. If it wasn't for this layer life could not exist -- too much radiation would reach the surface. Mesosphere The mesosphere is where most meteors burn up in the atmosphere. It also has some interesting, but poorly understood, phenomena such as noctilucent clouds, blue jets, and sprites. Thermosphere In the thermosphere, the temperature starts to increase again due to solar radiation. An important part of the thermosphere is the ionosphere, a region where the solar radiation is strong enough to split electrons off atoms to form ions. A spectacular aspect of the ionosphere are the auroras Aurora Borealis Aurora video (timelapse) Another important aspect of the ionosphere is that it allows radio waves to travel long distances. The waves refract off the ionosphere directing them back to Earth. Radio wave propagation by the ionosphere Atmospheric composition Composition of the atmosphere The numbers in the diagram consider a dry atmosphere. Water vapor accounts for 0-4%. Air Pollution Primary air pollutants pollutants emitted directly Secondary air pollutants pollutants created from reactions between primary air pollutants Criteria air pollutants 6 pollutants regulated by the US Environmental Protection Agency (USEPA) carbon monoxide particulate matter sulfur dioxide nitrogen dioxide ozone lead Sulfur Dioxide and Acid Rain Sulfur Dioxide Sulfur is oxidized to sulfur dioxide: S + O2 → SO2 This can then be combined with water in the atmosphere to form sulfur dioxide: 2SO2 + 02 + 2H20 → H2SO4 Source: burning of sulfur-containing compounds including coal and oil smelting of metal ores Cu2S + O2 → 2Cu + SO2 (metal ore) Doe Run's lead smelter in Herculaneum, Missouri,USA Direct Effect Absorbed by moist respiratory tissue causing restriction of airway - especialy severe in people with asthma Environmental Effect Acid Deposition Acid Deposition The fallout of sulfuric acid either in rain or as dry particles is called acid deposition or, more commonly, acid rain. Effects: Destruction of concrete and stone structures Acid rain events on a stone monument Acidification of forests, rivers, and lakes Some lakes have natural buffering, but many do not. Acidified water causes death of fish and other organisms. It also causes damage to trees and other plants. Acid rain damage on woodlands in Czech Republic Nitrogen dioxide, ozone, and smog Nitrogen Dioxide Nitric oxide (NO) and nitrogen dioxide (NO2) are formed from high temperature combustion. [1] low temperature combustion: CH4 + O2 + N2 → CO2 + H2O + N2 high temperature combustion: CH4 + O2 + N2 → CO2 + H2O + NO NO + O2 → NO2 Nitric oxide and nitrogen dioxide are together called NOx (read as nox). Health Effects: lung irritation increases susceptibility to lung disease The flask contains nitrogen dioxide. It is was give the characteristic brownish color to smog Ozone Nitrogen dioxide reacts with sunlight to form nitric oxide and atomic oxygen. This oxygen reacts quickly with molecular oxygen (O2) to form ozone. Ozone can then react with nitric oxide to regenerate nitrogen dioxide. NO2 + hν → NO + O O + O2 → O3 O3 + NO → NO2 + O2 Note The ozone formed here is tropospheric ozone ("bad ozone"), not to be confused with stratospheric ozone ("good ozone") Health Effects: lung problems eye irritation Environment Effects: damage to plants and trees Photochemical Smog Tropospheric ozone reacts with organic chemicals to produce photochemical smog. Smog is a toxic soup of NOx, ozone, peroxyacyl nitrates (PANs), aldehydes, and other organic chemicals. Smog in Kuala Lumpur, Malaysia Thermal inversions Under certain conditions a layer of warm air can occur above cold air. This causes any pollutants to be trapped and not dispersed.