Biogeochemical Cycles
Introduction to Biogeochemical Cycles
- Definition: Biogeochemical cycles refer to the pathways in which chemical nutrients move through biological (biotic) and non-biological (abiotic) components of ecosystems.
- Components:
- Bio: Living organisms
- Geo: Inorganic molecules (e.g., rocks, air, water)
- Chemical: Interactions among elements
Types of Nutrients
Macronutrients: Required in large amounts, essential for all biological life.
- Examples:
- Carbon
- Hydrogen
- Oxygen
- Nitrogen
- Phosphorus
- Sulfur
- Additional Macronutrients: Potassium, Calcium, Magnesium
Micronutrients: Required in smaller amounts but still vital.
- Examples:
- Iron
- Manganese
- Copper
- Zinc
- Sodium
Carbon Cycle
- Importance: Carbon forms the basis for life on Earth. It is stored in the atmosphere, land, and water.
- Photosynthesis: Converts inorganic atmospheric carbon into organic carbon used by plants.
- Steps of the Carbon Cycle:
- Atmosphere to Plants: Carbon dioxide from the atmosphere is absorbed by plants during photosynthesis to form organic compounds.
- Plants to Animals: Carbon moves through the food chain as animals consume plants.
- Plants/Animals to Soil: When organisms die, carbon is returned to the soil as they decompose.
- Living Things to Atmosphere: Respiration releases carbon dioxide back into the atmosphere.
- Atmosphere to Oceans: Carbon dioxide is absorbed by oceans, dissolved in water, contributing to the aquatic carbon cycle.
- Increasing CO2 Concentration:
- Caused by organic breakdown during respiration, oil and coal extraction, fuel combustion, and land-use changes.
Nitrogen Cycle
Stages:
- Nitrogen fixation
- Nitrification
- Assimilation
- Ammonification
- Denitrification
Processes:
- Nitrogen Fixation: Conversion of N2 (nitrogen gas) to NH4+ (ammonium) by nitrogen-fixing bacteria, lightning strikes, and industrial processes.
- Nitrification: Conversion of ammonia to nitrite (NO2-) and then to nitrate (NO3-) by nitrifying bacteria.
- Assimilation: Uptake of nitrogen compounds from soil by plants for protein synthesis.
- Ammonification: Decomposition of nitrogen-containing organic matter releases ammonia.
- Denitrification: Conversion of nitrate back to N2 gas by denitrifying bacteria, usually in low-oxygen environments.
Phosphorus Cycle
- Characteristics:
- Phosphorus is primarily found as mineral in phosphate rocks and is a sedimentary cycle (no gas phase).
- Processes:
- Erosion and mining release phosphates into soils/water.
- Plants absorb phosphates, which move to animals through food chains.
- Return to soil occurs via waste and decomposition.
- Eutrophication: Excess phosphates from fertilizers lead to algal blooms.
- Alterations to Cycle: Occur from deforestation and agricultural fertilizer use.
Sulfur Cycle
- Importance: Sulfur is vital for vitamins, proteins, and hormones, impacting climate and ecosystem health.
- Sources: Majority stored in rocks/minerals; weathering releases sulfur.
- Processes:
- Sulfur interacts with air forming sulfate (SO4) and is absorbed by plants.
- Animal consumption moves sulfur through the food chain.
- Decomposition returns some sulfur to soil as sulfate.
- Natural Sources: Volcanic eruptions, organic matter breakdown, water evaporation.
Hydrologic Cycle
Definition: The cycle of water storage, transport, and transformation in the atmosphere-earth system.
Importance: Shapes weather, supports plant growth, and sustains life.
Water Reservoirs:
- Oceans: 97%
- Polar Ice/Glaciers: 2%
- Groundwater: 0.7%
- Lakes: 0.01%
- Atmosphere: 0.001%
- Others: Soils, Rivers/Streams
Transport Methods: Evaporation, Transpiration, Precipitation, Infiltration, Percolation, Runoff, Interflow.
Transformations:
- Liquid to Gas (evaporation)
- Gas to Liquid (rainfall)
- Solid to Liquid (snowmelt)
References
- Nathanson, J.A. 1997. Basic Environmental Technology. Prentice-Hall, Inc.
- Tayo, G. T., et al. 2004. Fundamentals of Environmental Science. Trinitas Publishing, Inc.
- Various web sources concerning biogeochemical cycles.