Module 47 Photochemical Smog and Acid Rain

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Presentation transcript:

Module 47 Photochemical Smog and Acid Rain After reading this module, you should be able to Explain how photochemical smog forms and why it is still a problem in the United States. Describe how acid deposition forms and why it has improved in the United States and become worse elsewhere.

Photochemical smog remains an environmental problem in the United States The formation of this photochemical smog is complex and still not well understood. A number of pollutants are involved and they undergo a series of complex transformations in the atmosphere. Greenhouse Gases

The Chemistry of Ozone and Photochemical Smog Formation Tropospheric ozone and photochemical smog formation. (a) In the absence of VOCs, ozone will form during the daylight hours. (b) After sunset, the ozone will break down. (c) In the presence of VOCs, ozone will form during the daylight hours. The VOCs combine with nitrogen oxides to form photochemical oxidants, which reduce the amount of ozone that will break down later and contribute to prolonged periods of photochemical smog.

Thermal Inversions Thermal inversion A situation in which a relatively warm layer of air at mid-altitude covers a layer of cold, dense air below. Inversion layer The layer of warm air that traps emissions in a thermal inversion. The warm inversion layer traps emissions that then accumulate beneath it.

Thermal Inversions Continued Thermal inversions that create pollution events are particularly common in some cities, where high concentration of vehicles exhaust and industrial emissions are easily trapped by the inversion layer. Temperature Inversion

Thermal Inversions A thermal inversion. (a) Under normal conditions, where temperatures decrease with increasing altitude, emissions rise into the atmosphere. (b) When a mid-altitude, relatively warm inversion layer blankets a cooler layer, emissions are trapped and accumulate.

Acid deposition has improved in the United States Acid deposition occurs when nitrogen oxides and sulfur oxides are released into the atmosphere and combine with atmospheric oxygen and water. These form the secondary pollutants nitric acid and sulfuric acid. The secondary pollutants further break down into nitrate and sulfate, and hydrogen ions (H+) which cause the acid in acid deposition. Acid deposition has been reduced in the United States as a result of lower sulfur dioxide and nitrogen oxide emissions.

How Acid Deposition Forms and Travels Formation of acid deposition. The primary pollutants sulfur dioxide and nitrogen oxides are precursors to acid deposition. After transformation to the secondary pollutants—sulfuric and nitric acid— dissociation occurs in the presence of water. The resulting ions—hydrogen, sulfate, and nitrate—cause the adverse ecosystem effects of acid deposition.

Effects of Acid Deposition Acid deposition has many harmful effects: Lowering the pH of lake water Decreasing species diversity of aquatic organisms Mobilizing metals that are found in soils and releasing them into surface waters Damaging statues, monuments, and buildings Acid Rain: Smoky Mountains Appalachian Trail: Acid Rain