5

CO 2 + H 2 O H 2 CO 3 (carbonic acid) H 2 CO 3 H + + HCO 3 - (bicarbonate) HCO 3 - H + + CO 3 2- (carbonate) Ca 2+ + CO 3 2- CaCO 3 (calcium carbonate

Embed Size (px)

Citation preview

Page 1: CO 2 + H 2 O  H 2 CO 3 (carbonic acid) H 2 CO 3  H + + HCO 3 - (bicarbonate) HCO 3 -  H + + CO 3 2- (carbonate) Ca 2+ + CO 3 2-  CaCO 3 (calcium carbonate
Page 2: CO 2 + H 2 O  H 2 CO 3 (carbonic acid) H 2 CO 3  H + + HCO 3 - (bicarbonate) HCO 3 -  H + + CO 3 2- (carbonate) Ca 2+ + CO 3 2-  CaCO 3 (calcium carbonate

• CO2 + H2O H2CO3 (carbonic acid)

• H2CO3 H+ + HCO3- (bicarbonate)

• HCO3- H+ + CO3

2- (carbonate)

• Ca2+ + CO32- CaCO3 (calcium carbonate

– used by all shelled marine animals and diatoms)

Page 3: CO 2 + H 2 O  H 2 CO 3 (carbonic acid) H 2 CO 3  H + + HCO 3 - (bicarbonate) HCO 3 -  H + + CO 3 2- (carbonate) Ca 2+ + CO 3 2-  CaCO 3 (calcium carbonate
Page 4: CO 2 + H 2 O  H 2 CO 3 (carbonic acid) H 2 CO 3  H + + HCO 3 - (bicarbonate) HCO 3 -  H + + CO 3 2- (carbonate) Ca 2+ + CO 3 2-  CaCO 3 (calcium carbonate

• Movement in atmosphere: atmospheric C as CO2 (0.04% of troposphere)

• Primary production: photosynthesis (“carbon fixation”) moves C from atmosphere to organic molecules in organisms

• Movement through food web: C moves in organic form from organism to organism

• Aerobic respiration: organic molecules broken down to release CO2 back to atmosphere

• Combustion: organic molecules broken by burning release CO2 back to atmosphere

• Dissolving in oceans: C forms carbonate (CO32–) &

bicarbonate (HCO3–)

• Movement to sediments: C enters sediments, primarily as calcium carbonate (CaCO3)

Page 5: CO 2 + H 2 O  H 2 CO 3 (carbonic acid) H 2 CO 3  H + + HCO 3 - (bicarbonate) HCO 3 -  H + + CO 3 2- (carbonate) Ca 2+ + CO 3 2-  CaCO 3 (calcium carbonate

• How are humans affecting the carbon cycle?

• Which parts of the carbon cycle are considered short-term and which are considered long-term?