Cycling of Matter & The Climate System
Cycling of Matter & The Climate System
Biogeochemical Cycles
Define biogeochemical cycles:
Natural cycling of matter and energy between abiotic (non-living) and biotic (living) environments.
Importance of biogeochemical cycles:
Matter is held for longer periods in stores or reservoirs, facilitating essential ecological processes.
Human activities can disrupt the natural balance of these cycles, leading to environmental issues.
The Carbon Cycle
Carbon Stores
Define carbon stores: Locations where carbon is stored in various forms.
Major carbon stores and their respective amounts of carbon (in gigatonnes):
Marine sediments and sedimentary rock: Between 68 to 100,000,000 gigatonnes
Oceans: 39,000 gigatonnes
Fossil fuels: 3,300 gigatonnes
Vegetation, soil, and organic matter: 2,115 gigatonnes
Atmosphere: 750 gigatonnes
Global Carbon Budget
Definition: The global carbon budget describes the exchanges of carbon across different parts of the carbon cycle.
Impact of Human Activities:
Human activities affect the carbon cycle by altering the relative amounts of carbon stored in various reservoirs, which can lead to climate change and ecological disruption.
Nitrogen Cycle
Nitrogen
Composition of atmosphere: About 80% nitrogen gas (N2).
Process to enter the nitrogen cycle: N2 must be converted to other forms, such as ammonium (NH4) and nitrate (NO3-), to participate in biological processes.
Nitrogen Fixation:
Occurs naturally through:
Nitrogen-fixing bacteria in soil
Lightning strikes
Industrial process:
Using high temperatures and pressures to convert nitrogen into ammonia (NH3) for use in fertilizers.
Human Activity & Nitrogen
Impact on the Nitrogen Cycle:
Agricultural practices:
Use of fertilizers adds nitrogen to soils and enhances nitrogen fixation.
Environmental consequences:
Runoff from agricultural fields can add excessive nitrogen to waterways.
Resulting in ecological issues such as algal blooms and “dead zones” in aquatic ecosystems.
Other sources:
Farming and the combustion of fossil fuels also contribute to nitrogen accumulation in the atmosphere.