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Air Chemistry: Structure, Composition, Pollution, and Environmental Impact

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Air Chemistry and Earth's Atmosphere

Atmospheric Structure and Composition

The Earth's atmosphere is divided into several distinct layers, each with unique properties and functions. Understanding these layers is essential for grasping the chemistry of air and its environmental implications.

  • Troposphere: The lowest layer, containing most living organisms. Temperature decreases with altitude.

  • Stratosphere: Above the troposphere, contains the ozone layer. Temperature increases with altitude.

  • Mesosphere: Above the stratosphere, where temperatures decrease again.

  • Thermosphere: The uppermost layer, with increasing temperatures due to solar radiation.

Atmospheric layers and temperature profile

The composition of clean, dry air near sea level is primarily nitrogen and oxygen, with trace amounts of other gases.

Component

Percent by Volume

Nitrogen (N2)

78.08

Oxygen (O2)

20.94

Argon (Ar)

0.93

Carbon dioxide (CO2)

0.04

Trace gases

<0.01

Nitrogen Cycle and Atmospheric Chemistry

Nitrogen is the most abundant atmospheric gas, but most organisms cannot use it directly. It must be "fixed"—combined with other elements—before it becomes biologically available.

  • Natural fixation: Lightning converts N2 and O2 into nitrogen oxides, which form nitric acid in rain.

  • Industrial fixation: The Haber–Bosch process produces ammonia (NH3) from nitrogen and hydrogen.

  • Bacterial fixation: Certain bacteria in plant roots convert atmospheric nitrogen into usable forms.

The nitrogen cycle

Example: Lightning fixes nitrogen as follows:

Air Pollution and Smog

Pollution Goes Global

A pollutant is any substance found in the wrong place at the wrong time. Urbanization and globalization have made air pollution a worldwide concern.

Industrial Smog

Industrial smog results from the burning of coal and other industrial activities, producing a mixture of smoke and fog.

Industrial smog from factory chimneys

  • Oxides of Carbon: Burning coal produces carbon dioxide, carbon monoxide, and soot.

  • Oxides of Sulfur: Sulfur in coal forms sulfur dioxide and sulfur trioxide, which react with water to produce sulfuric acid.

  • Particulate Matter (PM): Solid and liquid particles, including unburned minerals, contribute to air pollution.

Types of Smog

Smog can be classified into two main types:

Industrial Smog

Photochemical Smog

Alternative names

Winter smog; sulfurous smog; "London smog"

Summer smog; "Los Angeles smog"

Main initial components

SO2; particulates

NOx; hydrocarbons

Secondary components

SO3; H2SO4

O3; aldehydes; PAN

Main sources

Power plants; factories

Automobiles

Typical weather

Cold; damp; foggy

Warm; dry; sunny

Health and Environmental Effects of Industrial Smog

  • Health: Sulfuric acid and particulates damage lung tissue, leading to pulmonary emphysema.

  • Environmental: Acidic precipitation and particulates harm plants and crops.

Controlling Industrial Smog

Several technologies are used to reduce industrial smog:

  • Electrostatic precipitators: Induce charges on particulates, attracting them to plates for removal.

Electrostatic precipitator diagram

  • Bag filtration: Removes particulates using filters.

  • Cyclone separators: Use spiral motion to deposit heavier particulates.

  • Wet scrubbers: Pass gases through water to remove particulates.

  • Sulfur removal: Sulfur can be removed from coal or neutralized with limestone.

Automobile Emissions and Air Chemistry

Combustion of Gasoline

Gasoline is a mixture of hydrocarbons, with octane (C8H18) as a representative compound. Complete combustion produces carbon dioxide and water:

Carbon Monoxide

Incomplete combustion produces carbon monoxide (CO), a toxic, colorless, odorless gas. CO binds to hemoglobin, preventing oxygen transport in the blood.

U.S. emissions of CO in millions of tonsCO binding to hemoglobin

Nitrogen Oxides

High temperatures in engines cause nitrogen and oxygen to react, forming nitrogen oxides (NOx):

NOx reacts with water to form acids, contributing to smog and acid rain. High concentrations can cause lung damage.

Volatile Organic Compounds (VOCs)

VOCs are hydrocarbons released from gasoline, exhaust, paints, and consumer products. They react with oxygen or ozone to form aldehydes and contribute to smog formation.

Photochemical Smog

Photochemical smog forms when pollutants react with sunlight, producing an amber haze. Pollutant concentrations vary throughout the day.

Development of air pollutants on a sunny day

Solutions to Photochemical Smog

  • Reduce pollutant emissions through improved gasoline storage and catalytic converters.

Acid Rain

Formation and Effects

Acid rain is precipitation with a pH less than 5.6, formed when sulfur and nitrogen oxides react with water to produce acids.

pH scale showing acid rainAcid rain formation and environmental impact

  • Acid rain damages natural and manufactured environments, harming plants, aquatic life, and infrastructure.

Indoor Air Pollution

Sources and Health Effects

Indoor air pollution can be much higher than outdoor levels. Common sources include gas stoves, cigarette smoke, kerosene heaters, mold, and ozone from electronic devices.

  • Cigarette smoke: Contains carcinogens and increases risk of heart disease, lung cancer, miscarriage, and SIDS.

  • Radon: A radioactive noble gas released from rocks and soil, decays by alpha emission, and poses health risks.

Ozone: The Double-Edged Sword

Ozone in the Atmosphere

Ozone (O3) is an allotrope of oxygen. In the troposphere, it is a pollutant; in the stratosphere, it protects life by absorbing ultraviolet radiation.

  • UV radiation splits O2 molecules into oxygen atoms:

Splitting of O2 by UV radiation

  • Oxygen atoms react with O2 to form ozone:

Formation of ozone from O2 and O

Ozone absorbs UV radiation, protecting living organisms.

Ozone Depletion

Chlorofluorocarbons (CFCs) destroy ozone in the stratosphere, leading to the ozone hole, especially over Antarctica.

Ozone hole over Antarctica, October 2017

  • Many countries have banned CFCs, and substitutes have been developed.

Carbon Dioxide and Climate Change

Greenhouse Effect

Carbon dioxide (CO2) is a greenhouse gas that traps heat in the atmosphere, contributing to global warming.

Greenhouse effect diagram

  • Human activities have increased atmospheric CO2, leading to rising global temperatures.

CO2 concentration and global temperature variation

Climate Change and Mitigation

Climate change impacts food production, flooding, and disease. Mitigation requires reducing greenhouse gas emissions through technologies like solar, nuclear, wind, and carbon sequestration.

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