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Composition and layers of the atmosphere, major air pollutants and their sources, acid rain, smog, the greenhouse effect and global warming, ozone layer depletion, and ways to control air pollution.
The atmosphere is the layer of gases around the Earth held by gravity. Dry air by volume is about 78% nitrogen, 21% oxygen, 0.9% argon and about 0.04% carbon dioxide, with traces of neon, helium, methane and hydrogen. Air also holds a variable amount of water vapour, dust and other particles.
Layers of the atmosphere from the ground upward:
Air pollution is the presence of harmful substances in air at levels that damage health, plants, buildings or climate. Pollutants may be primary, released directly (CO, SO₂), or secondary, formed in the air by reactions of primary pollutants (ozone, smog, acid rain). Sources are natural (volcanoes, dust storms, forest fires) and human (vehicles, factories, burning of crop residue and waste).
Main pollutants and their effects:
Acid rain is rain with a pH below 5.6. Normal rain is slightly acidic, about pH 5.6, because of dissolved carbon dioxide. SO₂ and nitrogen oxides oxidize and dissolve in water to give sulphuric and nitric acids: SO₂ + ½O₂ → SO₃ and SO₃ + H₂O → H₂SO₄. Acid rain damages forests, kills fish in lakes, and corrodes marble and metals. Marble: CaCO₃ + H₂SO₄ → CaSO₄ + H₂O + CO₂.
Smog is a mixture of smoke and fog. Classical smog comes from coal smoke and SO₂ with fog. Photochemical smog forms in strong sunlight when nitrogen oxides and hydrocarbons react to give ozone and other irritants such as PAN. It causes eye irritation, cough, and breathing trouble. Heavy smog in winter has been a serious problem in Lahore and other cities of Punjab.
The greenhouse effect is the natural warming of Earth. Sunlight passes through the air and warms the ground. The ground then gives off infrared heat, and greenhouse gases (CO₂, CH₄, N₂O, water vapour, CFCs) absorb a part of it and send it back. Without it, Earth would be about 33 °C colder on average. The danger is the extra warming from more greenhouse gases.
Global warming is the rise in the average temperature of Earth due to the increase of greenhouse gases from burning fossil fuels, cutting forests, farming and industry. Effects include melting of glaciers and ice caps, rise of sea level, more floods and heat waves, and changes to farming. Pakistan has glaciers in the north and has felt serious floods and heat waves.
The ozone layer is a region in the stratosphere, about 15 to 35 km above the ground, where ozone (O₃) absorbs most harmful ultraviolet-B and UV-C radiation. Ozone is formed when UV splits O₂ into atoms which combine with O₂: O₂ → 2O and O + O₂ → O₃.
CFCs destroy ozone. In the stratosphere, UV breaks CFCs to release chlorine atoms. Cl + O₃ → ClO + O₂ and then ClO + O → Cl + O₂. The chlorine atom is regenerated, so one atom can destroy thousands of ozone molecules. The loss of ozone, mainly over the polar regions, lets in more UV, which can cause skin cancer, cataracts and damage to crops. The Montreal Protocol (1987) phased out CFCs.
Control of air pollution:
Study tip: Learn the composition of air and the order of layers with one fact each. For pollution questions, use a fixed pattern: pollutant, source, effect, control. Practise writing the chlorine ozone reactions and the acid rain equations.
Say the meaning first, then open the card to check.
The envelope of gases surrounding the Earth.
A pollutant released directly into air from a source.
Rain with a pH below 5.6 caused by acidic oxides in the air.
Smog formed by sunlight acting on nitrogen oxides and hydrocarbons.
A gas that absorbs infrared radiation and warms the Earth.
The rise in the average temperature of the Earth due to extra greenhouse gases.
A stratospheric layer rich in O₃ that absorbs UV rays.
Chlorofluorocarbon, a compound that destroys ozone.
A device in a vehicle exhaust that converts harmful gases into safer ones.
| Name | Formula | What it means |
|---|---|---|
| Ozone formation | O₂ → 2O; O + O₂ → O₃ | Steps in the stratosphere |
| Acid rain | SO₃ + H₂O → H₂SO₄ | Formation of sulphuric acid |
| Ozone destruction | Cl + O₃ → ClO + O₂ | Chlorine from CFCs attacks ozone |
| ppm | ppm = (part / whole) × 10⁶ | Parts per million concentration |
These are the kind of questions asked for 2, 3 and 5 marks. Try each one before opening the answer.
Carbon dioxide in air dissolves in rain water to form weak carbonic acid, so normal rain has a pH of about 5.6. When SO₂ and nitrogen oxides also dissolve to form sulphuric and nitric acids, the pH falls below 5.6 and it is called acid rain.
CO binds to haemoglobin in the blood about 200 times more strongly than oxygen does, forming carboxyhaemoglobin. Blood then carries less oxygen. It causes headache, dizziness and, at high levels, death. It is colourless and odourless, so it is hard to notice.
Sunlight passes through the atmosphere and warms the ground. The warm ground gives out infrared radiation. Gases such as CO₂, methane and water vapour absorb part of this heat and send some of it back to the ground. This keeps Earth warm enough for life. More greenhouse gases from human activity trap extra heat and cause global warming.
In the stratosphere UV breaks the C−Cl bond in CFCs and gives chlorine atoms. A chlorine atom reacts with ozone: Cl + O₃ → ClO + O₂. Then ClO reacts with an oxygen atom: ClO + O → Cl + O₂. Chlorine is regenerated, so it acts as a catalyst and one atom can destroy many ozone molecules.
Effects: more skin cancer and cataracts, and damage to crops and plankton. To reduce vehicle pollution: fit catalytic converters and use cleaner fuels such as CNG.
It is a brown haze formed in sunlight when nitrogen oxides and hydrocarbons from vehicles react to form ozone, PAN and other irritants. It irritates eyes and lungs.
Answer: 105 dm³
Answer: 400 ppm
Answer: 32 g of SO₂