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Explore the dynamics of the carbon cycle, from reservoirs in the atmosphere, biosphere, oceans, and lithosphere to processes like photosynthesis, respiration, and combustion. Learn about human impacts, fossil fuels, and CO2 concentrations.
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Carbon Carbon exists in the nonliving environment as: • Carbon dioxide (CO2) • Carbonic acid ( HCO3−) • Carbonate rocks (limestone and coral = CaCO3) • Deposits of Fossil fuels • Dead organic matter
Organic Carbon • Hydrocarbons: CH4 • Carbohydrate: CH2O
Inorganic carbon • Carbon Dioxide: CO2 • Calcium Carbonate: CaCO3 Mandale Limestone Quarry
Carbon reservoirs • The atmosphere. • The biosphere (include fresh water systems and non-living organic material, such as soil carbon). • The oceans ( including dissolved inorganic carbon and living and non-living marine biota). • The lithosphere (sediments, Earth core including fossil fuels).
Carbon is released into the atmosphere in several ways • Respiration by plants and animals. • Decay of animal and plant matter. • Combustion of organic material • Production of cement. • The ocean releases CO2 into the atmosphere. • Volcanic eruptions and metamorphism
Carbon is taken from the atmosphere in several ways • Photosynthesis. • The oceans when the seawater becomes cooler, more CO2 dissolve and become carbonic acid. • In the upper ocean areas organisms convert reduced carbon to tissues, or carbonates.
Photosynthesis • CO2 + H2O + sunlight CH2O + O2
Respiration • CH2O + O2 CO2 + H2O + energy
Combustion or Oxidization of hydrocarbon CH4 + 2 O2 CO2 + 2 H2O + energy
Human Impacts on the Carbon Cycle Burning fossil fuels have serious impact on the carbon cycle.
Fossil Fuel 86% of global primary energy consumption is fossil fuels.
Fossil Fuels • Petroleum • Natural Gas • Coal
CO2 Concentration Pre-Industrial value: 280 ppm (600 billion tons) Current value: 380 ppm (800 billion tons) Critical value: 560 ppm (1200 billion tons)