Natural Resources — Class 9 Biological Science
"The air we breathe, the water we drink, the soil that grows our food — these are nature's gifts. But we are USING them faster than the Earth can replenish them. Understanding natural resources is the FIRST step toward saving our planet."
1. About the Chapter
Natural resources are materials from the Earth that are used by living organisms. This chapter covers:
- Air — composition, layers of the atmosphere, importance
- Water — the water cycle, distribution of water on Earth
- Ozone layer — its formation, depletion, and the role of CFCs
- Biogeochemical cycles — how carbon, nitrogen, and oxygen cycle through nature
- Greenhouse effect and global warming — the science behind climate change
- AP's natural resources — the Godavari and Krishna river systems, Eastern Ghats forests
Why This Chapter Matters
- Understanding biogeochemical cycles is CRITICAL for ecology and environmental science
- Ozone depletion and global warming are TWO MAJOR environmental challenges of our time
- AP Board connects this chapter to local environmental issues (coastal resources, forest conservation)
- This topic features in competitive exams (NEET, EAMCET, Group 1) as conceptual questions
2. Air — The Breath of Life
Air is a MIXTURE of gases — it is NOT a compound. The composition of dry air is remarkably CONSTANT.
Composition of Air
| Gas | Percentage by Volume | Role |
|---|---|---|
| Nitrogen (N₂) | 78.08% | Essential for protein synthesis (via nitrogen cycle), dilutes oxygen |
| Oxygen (O₂) | 20.95% | ESSENTIAL for respiration and combustion |
| Argon (Ar) | 0.93% | Inert gas — no significant biological role |
| Carbon dioxide (CO₂) | 0.04% | ESSENTIAL for photosynthesis |
| Other gases | Traces | Neon, Helium, Methane, Krypton, Hydrogen |
| Water vapour | Variable (0-4%) | Crucial for weather and climate |
Layers of the Atmosphere
| Layer | Height Range | Key Features |
|---|---|---|
| Troposphere | 0-12 km | Weather occurs here. Temperature DECREASES with height. Contains 75% of air mass. |
| Stratosphere | 12-50 km | OZONE LAYER is here. Temperature INCREASES with height (ozone absorbs UV). |
| Mesosphere | 50-80 km | Meteors BURN UP here. Temperature decreases. |
| Thermosphere | 80-700 km | Auroras occur here. Temperature VERY HIGH (up to 1500°C) but feels cold due to low density. |
| Exosphere | 700-10,000 km | Outermost layer. Gases ESCAPE into space. |
'About 99% of the Earth's atmosphere is within 30 km of the surface. The Troposphere and Stratosphere together contain MOST of the air.'
3. The Water Cycle (Hydrological Cycle)
The continuous movement of water between the Earth's surface, atmosphere, and back.
Processes in the Water Cycle
- Evaporation: Sun's heat turns surface water into water vapour
- Transpiration: Water vapour released from plant leaves (a plant can transpire hundreds of litres per day!)
- Condensation: Water vapour cools and forms clouds (tiny water droplets)
- Precipitation: Water falls as rain, snow, hail, or sleet
- Runoff: Water flows over land into rivers, lakes, and oceans
- Infiltration: Water seeps into the ground → becomes GROUNDWATER
Distribution of Earth's Water
| Water Source | Percentage |
|---|---|
| Oceans (salt water) | 97.3% |
| Ice caps and glaciers | 2.1% |
| Groundwater | 0.6% |
| Freshwater lakes and rivers | 0.009% |
| Atmosphere | 0.001% |
Key Insight
'Only about 0.3% of Earth's water is easily accessible FRESHWATER (rivers, lakes, shallow groundwater). This tiny fraction must support ALL terrestrial life — including 140 crore+ people in India. WATER CONSERVATION is not optional — it is SURVIVAL.'
AP Context — Water Resources
'Andhra Pradesh is blessed with two MAJOR river systems — the GODAVARI (second longest in India) and the KRISHNA. Major irrigation projects like Nagarjuna Sagar, Srisailam, and Polavaram (under construction) harness these rivers. However, AP faces water SCARCITY in drought-prone areas like Rayalaseema (Anantapur, Kurnool, Kadapa, Chittoor).'
4. Ozone Layer — Earth's Sunscreen
Ozone (O₃) is a molecule made of THREE oxygen atoms. The OZONE LAYER is a region in the STRATOSPHERE (15-35 km) with a high concentration of ozone.
Formation of Ozone
'Ozone is formed when UV radiation from the Sun splits an oxygen molecule (O₂) into TWO oxygen atoms. Each oxygen atom combines with an oxygen molecule to form ozone.'
Step 1: O₂ + UV → 2O (oxygen atoms) Step 2: O + O₂ → O₃ (ozone)
The Ozone Shield
'Ozone absorbs 97-99% of the Sun's HARMFUL ultraviolet (UV-B) radiation. Without the ozone layer, UV radiation would reach the Earth's surface, causing SKIN CANCER, cataracts, damage to immune systems, and harm to crops and marine life.'
Ozone Depletion
CFCs (Chlorofluorocarbons) — used in refrigerators, air conditioners, aerosol sprays, and foam packaging — rise to the stratosphere and BREAK DOWN ozone molecules.
CFC + UV → Cl atoms → Cl + O₃ → ClO + O₂ → Cl regenerated — a single chlorine atom can DESTROY UP TO 100,000 OZONE MOLECULES!
The Ozone Hole
'A THINNING of the ozone layer was detected over ANTARCTICA in the 1980s. This 'ozone hole' is most severe during the Antarctic spring (September-October). A similar but smaller thinning has been observed over the ARCTIC.'
International Action — The Montreal Protocol (1987)
An international treaty to phase out CFC production. One of the MOST SUCCESSFUL environmental agreements in history. 'The ozone layer is SLOWLY recovering — scientists estimate it will fully heal by 2060-2070. This shows that GLOBAL ACTION can solve environmental problems.'
5. Biogeochemical Cycles
Biogeochemical cycles describe the PATHWAYS through which chemical elements move between living organisms (BIO) and the non-living environment (GEO).
5.1 The Carbon Cycle
Carbon is the BUILDING BLOCK of life — all organic molecules contain carbon.
Key Processes:
- Photosynthesis: Plants take CO₂ from atmosphere + H₂O → Glucose + O₂ (REMOVES CO₂)
- Respiration: All organisms break down glucose → release CO₂ back into atmosphere (ADDS CO₂)
- Decomposition: Dead organisms decay → decomposers (bacteria, fungi) release CO₂
- Combustion: Burning of wood, fossil fuels → releases CO₂
- Ocean absorption: Oceans absorb CO₂ from the atmosphere (marine organisms use it for shells)
Human Impact on Carbon Cycle
'Burning FOSSIL FUELS (coal, oil, natural gas) and DEFORESTATION have dramatically INCREASED atmospheric CO₂ levels — from 280 ppm (pre-industrial) to over 420 ppm today. This is the PRIMARY driver of CLIMATE CHANGE.'
5.2 The Nitrogen Cycle
Nitrogen is ESSENTIAL for making PROTEINS and NUCLEIC ACIDS (DNA, RNA). While 78% of air is nitrogen, most organisms CANNOT use atmospheric N₂ directly.
Key Steps:
- Nitrogen Fixation: Atmospheric N₂ is converted to AMMONIA (NH₃). Done by:
- Rhizobium bacteria (in ROOT NODULES of leguminous plants like peas, beans, groundnuts)
- Free-living bacteria (Azotobacter, Clostridium)
- Lightning (atmospheric fixation — about 10%)
- Industrial fixation (Haber process — for fertilisers)
- Nitrification: Ammonia → Nitrites (Nitrosomonas bacteria) → Nitrates (Nitrobacter bacteria). Plants absorb NITRATES from soil.
- Assimilation: Plants use nitrates to make proteins. Animals eat plants → get nitrogen.
- Ammonification: Decomposers convert dead organic nitrogen → AMMONIA back to soil.
- Denitrification: Denitrifying bacteria (Pseudomonas) convert nitrates → N₂ gas back to atmosphere.
'Without the nitrogen cycle, there would be NO PROTEINS — and therefore NO LIFE as we know it. Farmers in AP grow groundnuts (a legume) in ROTATION with rice because Rhizobium in groundnut roots ENRICHES the soil with nitrogen — this is NATURAL fertilisation.'
5.3 The Oxygen Cycle
Oxygen cycles between the atmosphere and living organisms.
Sources of Oxygen:
- PHOTOSYNTHESIS (the MAJOR source — all atmospheric O₂ comes from this)
- Photolysis: UV splits water vapour in the upper atmosphere → O₂ (minor source)
Consumption of Oxygen:
- RESPIRATION (all living organisms)
- COMBUSTION (burning)
- DECAY of organic matter
'Rainforests are called the 'LUNGS of the Earth' because they produce about 20% of the world's oxygen through photosynthesis. Marine phytoplankton produce about 50-80% of Earth's oxygen — the OCEANS are the TRUE lungs of our planet.'
6. Greenhouse Effect and Global Warming
The Natural Greenhouse Effect
Certain gases (CO₂, CH₄, H₂O vapour, N₂O) in the atmosphere TRAP heat from the Sun, keeping the Earth WARM. Without this natural greenhouse effect, Earth's average temperature would be about −18°C instead of +15°C — life as we know it would be IMPOSSIBLE.
Enhanced Greenhouse Effect (Global Warming)
Human activities are INCREASING the concentration of greenhouse gases:
- CO₂: Burning fossil fuels, deforestation
- Methane (CH₄): Rice paddies, cattle farming, landfills
- Nitrous oxide (N₂O): Fertilisers, industrial processes
- CFCs: Refrigerants (also destroy ozone)
Consequences of Global Warming
- Rising sea levels: Melting glaciers and ice caps + thermal expansion of seawater
- Extreme weather: More intense cyclones, floods, droughts, heatwaves
- Impact on agriculture: Changing rainfall patterns, reduced crop yields
- Biodiversity loss: Species unable to adapt face extinction
- Ocean acidification: CO₂ absorbed by oceans forms carbonic acid → harms coral reefs and shellfish
AP Context — Climate Vulnerability
'Andhra Pradesh is in the TOP 5 most climate-vulnerable states in India. The 974 km coastline faces sea-level rise and CYCLONES (like Cyclone Hudhud, 2014, which devastated Visakhapatnam). Rayalaseema region faces DROUGHTS and water scarcity. Understanding climate change is CRITICAL for AP's future planning.'
7. AP's Major Natural Resources
Forests
AP has about 22% forest cover. Major forests are in the EASTERN GHATS (Visakhapatnam, East Godavari, Kadapa, Chittoor). Red Sanders (Red Sandalwood) — an ENDEMIC and highly valuable tree — grows in the Seshachalam Hills of AP.
Minerals
AP is a mineral-rich state: Bauxite (Vishakhapatnam), Mica (Nellore), Limestone (Guntur, Kurnool), and Natural Gas (Krishna-Godavari basin).
Water Resources
Major rivers: Godavari, Krishna, Penna, and Vamsadhara. The KRISHNA-GODAVARI delta region is known as the 'RICE BOWL of India' — some of the most fertile agricultural land in the country.
Coastal and Marine Resources
AP's 974 km coastline supports: Fishing industry (Machilipatnam, Visakhapatnam, Kakinada). Ports (Visakhapatnam is one of India's busiest). Mangrove forests (Coringa Wildlife Sanctuary near Kakinada — second largest mangrove forest in India).
8. Common Mistakes to Avoid
- 'Ozone is always harmful' — Ozone in the STRATOSPHERE is PROTECTIVE (absorbs UV). But ozone at GROUND LEVEL (tropospheric ozone) is a harmful pollutant that causes respiratory problems.
- 'The water cycle and the nitrogen cycle operate independently' — They are INTERCONNECTED. For example, Rhizobium bacteria need WATER for nitrogen fixation. Deforestation affects BOTH the water and carbon cycles.
- 'Plants only respire at night' — Plants respire CONTINUOUSLY (24 hours). Photosynthesis occurs only during the DAY. At night, plants release CO₂ (respiration) — but the CO₂ released is MUCH less than the CO₂ absorbed during photosynthesis.
- 'CFCs were banned only because of the ozone hole' — CFCs are ALSO powerful greenhouse gases (one CFC molecule traps about 10,000 times more heat than one CO₂ molecule).
- 'Nitrogen fixation only occurs through bacteria' — Lightning ALSO fixes nitrogen (about 10% of total). The Haber process (industrial) also produces nitrogenous fertilisers.
9. AP SSC Exam Focus
| Topic | Marks | Question Type |
|---|---|---|
| Atmosphere — layers and their features | 3-4 | Short Answer + Diagram |
| Water cycle — processes | 3-4 | Short Answer with flow diagram |
| Ozone layer — formation, depletion, CFCs | 4-5 | Long Answer + Application |
| Biogeochemical cycles (C, N, O) | 4-5 | Long Answer (any one cycle) |
| Greenhouse effect and global warming | 3-4 | Short Answer + Application |
| AP natural resources (contextual) | 2-3 | Application-based VSA |
Key Tip
'For cycle questions: Always draw a WELL-LABELLED DIAGRAM showing the flow of elements. Include ALL key processes and organisms involved (bacteria names for nitrogen cycle). Diagrams fetch FULL marks for labelling.'
10. Quick Self-Test
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'What is the role of Rhizobium in the nitrogen cycle?' Answer: Rhizobium bacteria live in ROOT NODULES of leguminous plants (peas, beans, groundnuts). They convert atmospheric NITROGEN (N₂) into AMMONIA (NH₃) through BIOLOGICAL NITROGEN FIXATION. This is a SYMBIOTIC relationship — the bacteria get shelter and food, the plant gets usable nitrogen.
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'Why is the ozone layer important? What is causing its depletion?' Answer: The ozone layer absorbs 97-99% of harmful UV-B radiation from the Sun. Without it, UV radiation causes skin cancer, cataracts, and crop damage. Ozone depletion is primarily caused by CFCs (chlorofluorocarbons) used in refrigerators, ACs, and aerosol sprays. CFCs release chlorine atoms that CATALYTICALLY destroy ozone molecules.
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'Explain how carbon moves from the atmosphere into living organisms and back.' Answer: CO₂ from atmosphere → PHOTOSYNTHESIS converts it into glucose in plants → animals eat plants → RESPIRATION releases CO₂ back → DECOMPOSITION by microbes also releases CO₂ → COMBUSTION of wood/fossil fuels releases CO₂ → Oceans ABSORB CO₂ (used by marine organisms for shells).
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'What percentage of Earth's water is freshwater available for human use?' Answer: About 0.3% of total water is accessible freshwater (rivers, lakes, shallow groundwater). 97.3% is in oceans (salt water) and 2.1% is locked in ice caps and glaciers.
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'How does deforestation affect the carbon cycle and the water cycle?' Answer: Deforestation REDUCES the number of trees that absorb CO₂ (photosynthesis) → more CO₂ remains in atmosphere → enhanced greenhouse effect → global warming. Deforestation also REDUCES transpiration → less water vapour in atmosphere → reduced rainfall → disruption of water cycle → desertification.
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'What are CFCs and why are they considered dangerous?' Answer: CFCs (Chlorofluorocarbons) are synthetic compounds used in refrigerators, ACs, and foam packaging. They are dangerous because: (1) They deplete the OZONE LAYER (one chlorine atom destroys up to 100,000 ozone molecules). (2) They are POWERFUL greenhouse gases. The Montreal Protocol (1987) has successfully phased out CFC production globally.
