D.2] Important Geographical Cycles
1. Water Cycle (Hydrologic Cycle)
Definition
The continuous movement of water on, above, and below the surface of the Earth.
Key Processes
- Evaporation: Water changes from liquid to vapor due to solar heat.
- Condensation: Water vapor cools and forms clouds.
- Precipitation: Water falls as rain, snow, sleet, or hail.
- Runoff: Water flows over the land surface into rivers, lakes, and oceans.
- Infiltration: Water seeps into the ground and replenishes groundwater.
- Transpiration: Water is released from plants into the atmosphere.
Key Facts (SSC, RRB)
- Important Date: The water cycle has been active since the formation of Earth (around 4.5 billion years ago).
- Important Term: Hydrological cycle.
- Important Example: The monsoon cycle in India is a major example of the water cycle.
Table: Water Cycle Stages
| Stage |
Description |
| Evaporation |
Liquid water turns into vapor |
| Condensation |
Vapor cools and forms clouds |
| Precipitation |
Water falls as rain, snow, etc. |
| Runoff |
Water flows over land into water bodies |
| Infiltration |
Water seeps into the ground to form groundwater |
| Transpiration |
Water released from plants into the atmosphere |
2. Carbon Cycle
Definition
The movement of carbon through the Earth’s atmosphere, oceans, soil, and living organisms.
Key Processes
- Photosynthesis: Plants absorb CO₂ and convert it into organic matter.
- Respiration: Organisms release CO₂ back into the atmosphere.
- Decomposition: Dead organic matter is broken down, releasing CO₂.
- Combustion: Burning of fossil fuels releases CO₂.
- Ocean Absorption: Oceans absorb and store large amounts of CO₂.
- Sedimentation: Carbon is stored in sedimentary rocks over long periods.
Key Facts (SSC, RRB)
- Important Date: The carbon cycle has existed for about 4.5 billion years.
- Important Term: Carbon sequestration.
- Important Example: The Great Barrier Reef is a significant carbon sink.
Table: Carbon Cycle Components
| Component |
Description |
| Atmosphere |
Contains CO₂, methane, and other greenhouse gases |
| Oceans |
Absorb and store large amounts of CO₂ |
| Soil |
Stores carbon in organic matter |
| Living Organisms |
Plants and animals absorb and release CO₂ |
| Fossil Fuels |
Stored carbon from ancient organic matter |
3. Nitrogen Cycle
Definition
The movement of nitrogen through the environment, including the atmosphere, soil, and living organisms.
Key Processes
- Nitrogen Fixation: Conversion of atmospheric nitrogen (N₂) into usable forms (e.g., ammonia) by bacteria.
- Nitrification: Conversion of ammonia to nitrites and nitrates by bacteria.
- Assimilation: Plants absorb nitrates and convert them into proteins.
- Ammonification: Decomposition of organic nitrogen into ammonia.
- Denitrification: Conversion of nitrates back into nitrogen gas by bacteria, returning it to the atmosphere.
Key Facts (SSC, RRB)
- Important Date: The nitrogen cycle has existed for about 4.5 billion years.
- Important Term: Nitrogen fixation, denitrification.
- Important Example: Leguminous plants (e.g., peas, beans) are key in nitrogen fixation.
Table: Nitrogen Cycle Stages
| Stage |
Description |
| Nitrogen Fixation |
Conversion of N₂ to ammonia by bacteria |
| Nitrification |
Conversion of ammonia to nitrites and nitrates |
| Assimilation |
Plants absorb nitrates and convert to proteins |
| Ammonification |
Decomposition of organic nitrogen into ammonia |
| Denitrification |
Conversion of nitrates back to N₂ by bacteria |
Differences Between Cycles
| Cycle |
Primary Source |
Major Storage |
Human Impact |
Key Exam Focus |
| Water Cycle |
Evaporation |
Oceans, lakes |
Climate change |
High |
| Carbon Cycle |
Fossil fuels |
Oceans, soil |
Greenhouse gases |
High |
| Nitrogen Cycle |
Atmosphere |
Soil, plants |
Fertilizers, pollution |
Medium |