Overview of main atmospheric gas cycles:
Carbon cycle
Oxygen cycle
Carbon dioxide cycle
Other cycles: Phosphorous cycle, Water cycle
Carbon Presence
Carbon exists in the atmosphere primarily as carbon dioxide (CO2).
Atmosphere serves as the source of carbon for living beings.
Photosynthesis
Green plants absorb CO2 and utilize sunlight to produce carbohydrates, a form of food.
Carbohydrates serve as a vital energy source for all living organisms.
Carbon Dissolution
CO2 dissolves in water bodies, leading to lime accumulation on Earth.
The dissolution process known as carbonization causes CO2 to re-enter the atmosphere.
Carbon Release
CO2 is produced through respiration by plants and animals, decomposition of organic matter, and combustion of fossil fuels (coal, petroleum, natural gas).
This continuous cycle maintains the balance of carbon and the biosphere.
Oxygen Proportion
Oxygen makes up approximately 21% of the atmosphere; essential for respiration in all living beings.
Role in Combustion
Oxygen is crucial for the combustion of fuels (wood, coal, gas), producing CO2 in the process.
Sources of Oxygen
Oxygen is predominantly produced by plants and trees; more vegetation leads to higher oxygen availability.
Cycle Continuity
Oxygen produced via photosynthesis is cycled back into the atmosphere through respiration by animals and plants.
Atmospheric Nitrogen
Comprises 78% of the atmosphere, crucial for life.
Sources of Nitrogen
Primary sources are nitrates in the soil.
Biological Transformation
Nitrogen enters biological components through biological (nitrogen fixation) and industrial processes.
Food Chain Transfer
Nitrogen compounds are transferred from plants to animals through the food chain.
Decomposition
Decomposition of organic matter by bacteria returns nitrogen gas to the atmosphere, completing the nitrogen cycle.
Unique Characteristics
Unlike other cycles, the phosphorus cycle is sedimentary, without a gaseous phase.
Sources
The largest reservoir is in sedimentary rocks; phosphorous enters the cycle through weathering and erosion.
Transportation
Phosphates are transported to water bodies where they are utilized by aquatic plants and algae.
Excess phosphates can lead to environmental issues like eutrophication.
Human Impact
Commercial fertilizers, mining, deforestation, and agricultural runoff contribute to nutrient overload in aquatic ecosystems.
Definition
Nutrient enrichment (eutrophication) leads to serious environmental issues in aquatic ecosystems.
Consequences
Algae blooms consume dissolved oxygen, resulting in anoxic conditions.
Decomposition of algae further depletes oxygen, affecting fish survival.
Process Overview
Also known as the hydrologic cycle; encompasses evaporation, condensation, precipitation, and runoff.
Evaporation
Water transforms from liquid to gas due to solar energy, including transpiration from plants.
Condensation
Vapors cool and consolidate into clouds, essential for precipitation.
Precipitation
Returns water to Earth in forms such as rain, snow, sleet, or hail.
Infiltration and Run-off
Water seeps into the ground forming aquifers or flows into bodies of water; crucial for recharging groundwater supplies.
Main Learning Objectives
The cycle facilitates the natural circulation of water, influences climate, and impacts weather patterns.
Highlights the importance of water availability and ecosystem health.