Important geographical cycles

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