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Biogeochemical Cycles
Lecture slides by
PROFESSOR AJAL A J
9188 142 143
Biogeochemical Cycles
Water
Nitrogen
Carbon Dioxide
Phosphorus
Sulfur
Biogeochemical Cycle :
 chemical elements are required by life from
the living and nonliving parts of the
environment.
 These elements cycle in either a gas cycle or
a sedimentary cycle
 In a gas cycle elements move through the
atmosphere
Carbon
Cycle
 Photosynthesi
s
 Respiration
 Decomposition
Carbon Cycle
 Carbon (C) enters the biosphere during
photosynthesis:
 CO2 + H2O (carbon dioxide+ water)--->
C6H12O6 + O2 + H2O(sugar+oxygen+water)
 Carbon is returned to the biosphere in cellular
respiration:
 O2 +H2O + C6H12O6 ---> CO2 +H2O + energy
Carbon Facts
 Every year there is a measurable difference
in the concentration of atmospheric CO2 with
changes in the seasons.
 For example, in winter there is almost
no photosynthesis ( higher CO2 )
 During the growing season there is a
measurable difference in the
concentration of atmospheric CO2
over parts of each day.
Phosphorus
(P) Cycle
Water cycle
 Evaporation, condensation and precipitation are the main processes
involved inwater cycle these processes alternate with each otherWater
from oceans, lakes, ponds, rivers, streams and soil surface evaporates
by sun’sheat energy. Plants also transpire huge amounts of water
through their leaves. Water remains in the vapour state in air and forms
clouds, which drift with the wind. Clouds meet with the cold air in the
mountainous regions above the forests and condense to form rain,
which falls due to gravity.
Phosphorus (P) Cycle
Component of DNA, RNA, ATP, proteins and enzymes
- Cycles in a sedimentary cycle
- A good example of how a mineral element becomes part of
an organism.
- The source of Phosphorus (P) is rock.
- Phosphorus is released into the cycle through erosion or
mining.
- Phosphorus is soluble in H2O as phosphate (PO4)
-Phosphorus is taken up by plant roots, then travels through
food chains.
- It is returned to sediment

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Biogeochemical cycles

  • 1. Biogeochemical Cycles Lecture slides by PROFESSOR AJAL A J 9188 142 143
  • 3. Biogeochemical Cycle :  chemical elements are required by life from the living and nonliving parts of the environment.  These elements cycle in either a gas cycle or a sedimentary cycle  In a gas cycle elements move through the atmosphere
  • 5. Carbon Cycle  Carbon (C) enters the biosphere during photosynthesis:  CO2 + H2O (carbon dioxide+ water)---> C6H12O6 + O2 + H2O(sugar+oxygen+water)  Carbon is returned to the biosphere in cellular respiration:  O2 +H2O + C6H12O6 ---> CO2 +H2O + energy
  • 6. Carbon Facts  Every year there is a measurable difference in the concentration of atmospheric CO2 with changes in the seasons.  For example, in winter there is almost no photosynthesis ( higher CO2 )  During the growing season there is a measurable difference in the concentration of atmospheric CO2 over parts of each day.
  • 9.  Evaporation, condensation and precipitation are the main processes involved inwater cycle these processes alternate with each otherWater from oceans, lakes, ponds, rivers, streams and soil surface evaporates by sun’sheat energy. Plants also transpire huge amounts of water through their leaves. Water remains in the vapour state in air and forms clouds, which drift with the wind. Clouds meet with the cold air in the mountainous regions above the forests and condense to form rain, which falls due to gravity.
  • 10. Phosphorus (P) Cycle Component of DNA, RNA, ATP, proteins and enzymes - Cycles in a sedimentary cycle - A good example of how a mineral element becomes part of an organism. - The source of Phosphorus (P) is rock. - Phosphorus is released into the cycle through erosion or mining. - Phosphorus is soluble in H2O as phosphate (PO4) -Phosphorus is taken up by plant roots, then travels through food chains. - It is returned to sediment