Definition: Photochemical smog is a mixture of primary and secondary pollutants, primarily featuring photochemical ozone as its main component.
Components: Contains over 100 chemicals, including volatile organic compounds (VOCs) and nitrogen oxides (NOx).
Formation Process:
VOCs and NOx react in the presence of UV light and oxygen, leading to the formation of tropospheric ozone.
This process is a photochemical reaction, making tropospheric ozone a secondary pollutant.
Health Effects: Resulting smog can cause irritated eyes and throats, particularly on sunny days in urban areas.
Major cities known for dense photochemical smog include:
Argentina: Buenos Aires
Brazil: Sao Paulo
Mexico: Mexico City
China: Beijing, Shanghai
Australia: Sydney
USA: Salt Lake City, Denver, Los Angeles
Great Smog of London (1952): Resulted in 4,000 deaths over five days following earlier smog events in 1880 and 1911.
Other significant smog incidents:
Industrial smog disasters killed approximately 2,500 people in 1956, '57, and 1962.
The Clean Air Act of 1956 in the UK improved air quality regulations.
The Killer Smog of Donora (1948): 20 deaths and 7,000 illnesses in a Pennsylvania town due to emissions from industrial plants.
NYC Smog (1963): Injured and sickened thousands.
Photochemical Smog vs. Industrial Smog:
Photochemical Smog: Results from chemical reactions involving primary pollutants and sunlight.
Industrial Smog: Formed from sulfur dioxide and soot particulates due to the burning of fossil fuels like coal and oil.
Chemical Reactions:
Sulfur dioxide reacts with oxygen to form sulfur trioxide, which further reacts with water vapor, creating sulfuric acid leading to acid rain.
SPM (Suspended Particulate Matter) gives industrial smog its gray color.
Emissions Control: Developed countries enforce rigorous emissions control policies for cleaner air in industrial plants, favoring tall smokestacks and pollution controls.
Developing countries, e.g., Ukraine, India, and China, still struggle with heavy industrial smog due to inadequate regulations.
The Clean Air Act of 1970 in the USA set emission standards for vehicles and industries, with amendments in 1977 and 1990.
Influenced by:
Type of fuels used
Quantity of industrial activities
Population density
Regional topography and climate
Mitigating Factors:
Precipitation helps cleanse air by coagulating pollutants.
Wind can dilute and remove polluted air, but urban buildings and mountains can obstruct airflow.
Normal Conditions: Warm air containing pollutants mixes with cool air above, dispersing them.
Inversion Conditions: A temperature inversion traps pollutants near the ground when a layer of warm air overlays cooler air, leading to smog accumulation.
Types of Inversion:
Subsidence Inversion: Occurs when warm air at high altitudes moves over a cooler region, trapping pollutants.
Radiation Inversion: Happens when ground-level air cools more rapidly than air above, creating a warm layer that keeps pollutants trapped.
Geographical Impact: Regions with surrounding mountains or valleys, like Los Angeles and Mexico City, are prone to prolonged inversions during summer months, exacerbating smog issues.
Urban infrastructure (e.g., asphalt, concrete) absorbs heat, contributing to higher temperatures in cities:
Leads to enhanced photochemical reactions and greater smog formation.
Mitigation Strategies:
Implementing green roofs
Stricter vehicle emissions policies
Increasing green spaces and tree conservation.
Key Takeaway: Prolonged thermal inversions can increase pollution residence time due to geographical features.
Remarkable events of photochemical smog stress the importance of understanding and addressing air pollution for public health.