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Carbon Cycle

Carbon Cycle. Carbonic acid ( HCO 3 − ) Carbonate rocks (limestone and coral = CaCO 3 ) Deposits of Fossil fuels. Carbon. Carbon exists in the nonliving environment as: . Hydrocarbons: CH 4 Carbohydrate: CH 2 O. Organic Carbon. Carbon Dioxide: CO 2 Calcium Carbonate: CaCO 3.

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Carbon Cycle

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  1. Carbon Cycle

  2. Carbonic acid ( HCO3−) Carbonate rocks (limestone and coral = CaCO3) Deposits of Fossil fuels Carbon Carbon exists in the nonliving environment as:

  3. Hydrocarbons: CH4 Carbohydrate: CH2O Organic Carbon

  4. Carbon Dioxide: CO2 Calcium Carbonate: CaCO3 Inorganic carbon Mandale Limestone Quarry

  5. Carbon Reservoirs

  6. Carbon reservoirs • The atmosphere -as carbon dioxide • The biosphere - as organic carbon (include fresh water systems and non-living organic material, such as soil carbon). • The oceans - as dissolved carbon dioxide and molecules like calcium carbonate ( including dissolved inorganic carbon and living and non-living marine biota). • The lithosphere as sedimentary rock like limestone and metamorphic rock like marble (sediments, Earth core including fossil fuels).

  7. Carbon Cycle

  8. Respiration by plants and animals. Decay of animal and plant matter. Combustion of organic material Production of cement made from limestone The ocean releases CO2 by diffusion into the atmosphere. Volcanic eruptions and metamorphism Carbon is released into the atmosphere in several ways

  9. 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 organic molecules, or carbonates. Carbon is taken from the atmosphere in several ways

  10. sunlight 6CO2 + 12H2O + ---------->C6H12O6 + 6 O2 Chlorophyll Photosynthesis

  11. C6H12O6 + 6O2 --> 6CO2 + 6H2O + usable energy(ATP) Respiration

  12. Combustion or Oxidization of hydrocarbon CH4 + 2 O2 --> CO2 + 2 H2O + energy

  13. Human Impacts on the Carbon Cycle The burning of fossil fuels has a serious impact on the carbon cycle.

  14. 86% of global primary energy consumption is fossil fuels. Fossil Fuel

  15. Petroleum Natural Gas Coal Fossil Fuels

  16. Pre-Industrial value: 280 ppm (600 billion tons) Current value: 400 ppm (840 billion tons) Critical value: 560 ppm (1200 billion tons) CO2 Concentration

  17. Keeling Curve Question: Why does line of the curve go up and down by about 5 ppmv instead of in a straight line?

  18. What process is occurring at each number? Plant Respiration Animal Respiration Decay of animal wastes Photosynthesis Decay of plant litter

  19. Carbon Cycle Summary Green Plants, Algae, some bacteria CO2 C6H12O6 All organisms C6H12O6 CO2 Organic Carbon Decay bacteria, Fungi CO2 Organic Carbon N/A Burning CO2 N/A In water CO2 Carbonic acid Plant and animal remains Fossil fuels N/A Forming rocks Limestone, Marble CaCO3 Calcium carbonate N/A Gas from volcanos Limestone, Marble CO2

  20. Part II: The Carbon Reservoirs On a global scale , carbon moves between four major reservoirs (also called carbon sinks). These reservoirs include ______________________, ______________________,______________________, and __________________________. Which reservoir contains the most carbon? _______________. Atmosphere Ocean Biosphere Lithosphere Lithosphere

  21. Part III: The Biological (Biotic) Processes • 1. Photosynthesis is a process that takes place in organisms containing pigments • capable of capturing the energy of light. The main photosynthetic pigment is the green • pigment called chlorophyll found in green plants, algae, and Cyanobacteria. Organisms • with this pigment are able to remove ___________________________ from the • atmosphere and combine it with ________________ in the presence of chlorophyll and • sunlight making ____________________ (energy storage molecules) and releasing the • gas _________________ to the atmosphere. • Complete the generalized equation: • Sunlight • ________ + ________ --------------------> ________ + ________ • Chlorophyll Carbon dioxide Water Glucose Oxygen 6O2 C6H12O6 12 H2O 6 CO2

  22. 2. Cellular respiration is a process that takes place in cells that releases the chemical energy stored in larger molecules to be restored in small molecules that cells can use. The process takes the larger energy storage molecule called __________________ and combines it with __________________ from the atmosphere. This releases the chemical energy that is captured by the small energy molecules called ____________ that can be used by cells. End products of cellular respiration are _______________ and _________________ which is released into the atmosphere. Complete the generalized equation: __________ + __________ --------------------> _________ + __________ + __________ Glucose Oxygen ATP carbon dioxide water 6O2 6 CO2 ATP C6H12O6 6 H2O

  23. Part IV: The Inorganic (abiotic) Processes • The burning of any organic matter form fossil fuels to forests rapidly releases the • carbon stored in its molecules as the gas _______________________ to the • atmosphere. • 2. Carbon as the gas _____________________ readily dissolves into bodies of water • from ponds to oceans. This gas readily combines with water molecules to form an acid • called _______________________ often lowering the pH of the water. Carbon dioxide Carbon dioxide Carbonic Acid

  24. 3. Aquatic organisms that protect themselves with shells combine the gas _____________________ with the mineral calcium making _____________________, the material that forms its shell. When these shelled organisms died, their shells rain down to the bottom of the lake or ocean collecting in deep layers as sediment. Slowly, the shells are compressed into sedimentary rock in a process called _________________________ 4. Over geologic time, sedimentary and metamorphic rock containing carbon are subducted, melted and rise toward the surface of the earth as magma and gases like _________________________ which are released into the atmosphere when volcanos ______________________. Carbon dioxide Calcium carbonate Limestone Carbon dioxide Erupt

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