Syllabus topics (RTMNU)
- 1.1 Atmosphere: Major zones, importance, composition of air.
- 1.2 Hydrosphere: Global distribution of water, Physico-chemical characteristics of water.
- 1.3 Lithosphere: formation of soil, Causes of soil erosion.
- 1.4 Renewable and non-renewable energy sources.
1.1 Atmosphere: Major zones, importance and composition of air
The atmosphere is the layer of gases surrounding the Earth, held by gravity. It extends to about 500–1000 km, but about 99% of its mass lies within 30–32 km of the surface.
Composition of dry air (by volume)
| Gas | Approx. % | Role |
|---|---|---|
| Nitrogen (N₂) | 78.08 | Dilutes oxygen; source of nitrogen for nitrogen-fixing bacteria |
| Oxygen (O₂) | 20.95 | Respiration, combustion; forms ozone |
| Argon (Ar) | 0.93 | Inert gas |
| Carbon dioxide (CO₂) | about 0.04 (≈ 420 ppm) | Photosynthesis; greenhouse gas |
| Others | traces | Ne, He, CH₄, Kr, H₂, O₃, N₂O |
Air also contains variable amounts of water vapour (0–4%) and suspended particles (dust, pollen, smoke).
Major zones (based on temperature)
| Zone | Height (approx.) | Temperature trend | Key features |
|---|---|---|---|
| Troposphere | 0–12 km (8 km at poles, 16–18 km at equator) | Falls with height (≈ 6.5 °C per km) | All weather – clouds, rain, wind; contains most water vapour; upper limit tropopause |
| Stratosphere | 12–50 km | Rises with height | Ozone layer (about 15–35 km) absorbs UV rays; calm, used by jet planes; upper limit stratopause |
| Mesosphere | 50–80/85 km | Falls; coldest layer (about −90 °C) | Meteors burn up here |
| Thermosphere (with ionosphere) | 85–500 km | Rises sharply (above 1000 °C) | Ionised gases reflect radio waves; aurora |
| Exosphere | Above 500 km | — | Very thin air merging with space; satellites |
Importance of atmosphere
- Provides O₂ for respiration and CO₂ for photosynthesis.
- The ozone layer filters harmful ultraviolet (UV-B, UV-C) rays.
- Keeps the Earth warm (natural greenhouse effect, average ≈ 15 °C instead of about −18 °C).
- Controls weather and climate; distributes heat and moisture; part of the water cycle.
- Protects from meteors; reservoir of nitrogen for the nitrogen cycle.
1.2 Hydrosphere: Global distribution of water and its physico-chemical characteristics
The hydrosphere includes all water on Earth – oceans, seas, rivers, lakes, ground water, ice and water vapour. About 71% of the Earth’s surface is covered by water.
Global distribution
| Source | % of total water |
|---|---|
| Oceans and seas (salt water) | ≈ 97.5 |
| Fresh water – total | ≈ 2.5 |
| — in ice caps and glaciers | ≈ 69% of fresh water |
| — ground water | ≈ 30% of fresh water |
| — lakes, rivers, soil moisture, atmosphere, living beings | ≈ 1% of fresh water |
So less than 1% of all water is easily available for human use.
Physical characteristics
- Temperature: affects dissolved oxygen and metabolism; water has high specific heat, so water bodies change temperature slowly.
- Density: maximum at 4 °C, so ice floats and aquatic life survives below the ice in winter.
- Colour, turbidity and transparency: suspended particles reduce light penetration (measured by Secchi disc).
- Taste and odour; total solids (dissolved and suspended); electrical conductivity (indicates dissolved salts).
Chemical characteristics
- pH: natural fresh water 6.5–8.5 is suitable for life.
- Dissolved oxygen (DO): 5–8 mg/L in clean water; below 4 mg/L harms fish.
- Free CO₂: from respiration and decay; high CO₂ means pollution.
- Hardness: due to Ca²⁺ and Mg²⁺ salts – temporary (bicarbonates, removed by boiling) and permanent (sulphates, chlorides).
- Alkalinity, chlorides, nitrates, phosphates (excess nutrients cause eutrophication).
- BOD and COD: measure organic pollution; clean water BOD < 3 mg/L.
1.3 Lithosphere: Formation of soil and causes of soil erosion
The lithosphere is the solid outer layer of the Earth (crust and upper mantle). Soil is its thin, loose top layer made of mineral particles, organic matter (humus), water, air and living organisms.
Formation of soil (pedogenesis)
- Weathering of parent rock:
- Physical – temperature changes, freezing–thawing, wind and water break rock into pieces.
- Chemical – oxidation, hydration, carbonation and solution change minerals.
- Biological – lichens, mosses, roots and burrowing animals break and mix rock material.
- Humification: dead plants and animals decompose into dark humus.
- Translocation and horizon formation: water moves materials down (eluviation) and deposits them (illuviation), forming layers – O (organic), A (top soil), B (sub soil), C (weathered parent rock) and R (bed rock).
Factors of soil formation: parent material, climate, organisms, topography (relief) and time. It takes hundreds of years to form about 2.5 cm of top soil.
Soil erosion
Soil erosion is the removal of the fertile top soil by wind, water or human activity faster than it can form.
- Natural causes: heavy rain and floods (sheet, rill and gully erosion), strong winds in dry areas, landslides, waves along the coast.
- Human causes: deforestation, overgrazing, faulty farming (ploughing up and down slopes, shifting cultivation), mining, construction and road building.
- Effects: loss of fertility, siltation of rivers and dams, floods, desertification.
- Control (in brief): afforestation, contour ploughing, terrace farming, strip cropping, wind breaks (shelter belts), check dams, controlled grazing.
1.4 Renewable and non-renewable energy sources
| Point | Renewable | Non-renewable |
|---|---|---|
| Meaning | Replenished naturally; practically inexhaustible | Formed over millions of years; limited stock, cannot be replaced in human time |
| Examples | Solar, wind, hydro, tidal, geothermal, biomass/biogas | Coal, petroleum, natural gas (fossil fuels), nuclear fuels (uranium) |
| Pollution | Little or none | CO₂, SO₂, NOₓ, smoke, radioactive waste |
| Cost | High set-up, low running cost | Cheaper set-up, rising fuel cost |
Renewable sources – key points
- Solar energy: solar cookers, heaters, photovoltaic cells; India’s National Solar Mission.
- Wind energy: windmills/turbines; Tamil Nadu, Gujarat lead in India.
- Hydroelectric: energy of falling water; but large dams displace people and flood forests.
- Tidal and wave energy: uses the rise and fall of sea tides (Gulf of Khambhat, Gulf of Kutch have potential).
- Geothermal: heat from inside the Earth (Puga valley, Ladakh).
- Biomass and biogas: wood, crop waste, cow dung; biogas (mainly methane) from anaerobic digestion.
Non-renewable sources – key points
- Coal: main source of thermal power in India (Jharia, Raniganj, and Chandrapur–Wardha fields in Vidarbha).
- Petroleum and natural gas: transport fuel, LPG, CNG (Mumbai High, Assam).
- Nuclear energy: fission of uranium-235; Tarapur (Maharashtra), Kudankulam; no CO₂ but radioactive waste and accident risk.
Conclusion: shifting from fossil fuels to renewable energy reduces pollution and global warming and gives energy security.
Likely exam questions
- (Long, 8 marks) Describe the major zones of the atmosphere and the composition and importance of air.
- (Long, 8 marks) Explain the formation of soil and the causes of soil erosion.
- (Short, 4 marks) Write a note on the global distribution of water.
- (Short, 4 marks) Describe any four physico-chemical characteristics of water.
- (Short, 4 marks) Distinguish between renewable and non-renewable energy sources with examples.