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 Nitrogencomprises 78.08 % of the
 atmosphere making it the largest
 constituent of the gaseous envelope that
 surrounds the Earth.

 Nitrogenis important in the make up of
 organic molecules like proteins and DNA.

 Mostorganisms cannot use nitrogen in this
 form, i.e N2
 Plantssecure their nitrogen in “fixed” forms
 i.e incooperated in compounds such as:
  Nitrate ions NO3
  Ammonia NH3
  Urea (NH2)2CO


 Animalssecure their nitrogen (and all other
 compounds from plants (or animals that
 have eaten plants).
 Four processes participate in the cycling
 of nitrogen in the biospere:

  •   Nitrogen fixation
  •   Decay
  •   Nitrification
  •   Denitrification

  *microorganisms play major roles in all
     processes*
 Thenitrogen molecule is quite inert. To
 break it apart so that its atoms can
 combine with other atoms requires the
 input of substantial amounts of energy.


 inert-nonreactive gas during chemical
 synthesis, analysis or preservation of
 reactive materials
 Three processes are responsible for most
 of the nitrogen fixation:

  1. Atmospheric fixation
  2. Biological fixation
  3. Industrial fixation
 Theenormous energy of lightening
 breaks nitrogen molecules and enables
 then to combine with oxygen in the air
 forming nitrogen oxides.

 These dissolve in rain forming nitrates
 that are carried to the earth.

     *contributes   5-8% of total fixed*
 Made   synthetically via Haber Process.

 Nitrogenand hydrogen reacted under
 great pressure and temperature in the
 presence of a catalyst to make ammonia.

 Ammonia    applied directly to farm fields
 as fertilizers or further processed with
 oxygen to make nitric acid.
 Theability to fix nitrogen is found only in
 certain bacteria and archaea.

 Some   live in symbiotic relationship with
  plants of the legume family Rhizobium
 Some establish symbiotic relationships
  with animals
 Some live free in soil
 Biological
          nitrogen fixation requires a
 complex set of enzymes and a huge
 expenditure of ATP
 Protein
        made by plants enter and pass
 through food webs at each level.

 Ateach trophic level metabolism
 produces nitrogen compounds that
 return to the environment in excretions.

 Microorganisms break down the
 molecules in excretion and dead
 organisms into ammonia, NH3.
 Most of the ammonia produced by decay
 is converted into nitrates.

  Bacteria of the genus Nitrosomonas
   oxidize NH3  nitrites NO2

  Bacteria of the genus Nitrobacter
   oxidize nitrites  nitrates NO3
 Thisis the reduction of nitrates to
 nitrogen gas, thus replenishing the
 atmosphere

 Anaerobic bacteria use nitrates as an
 alternative to oxygen in their respiratory
 process.

 Closing   the nitrogen cycle
A side product of this reaction is known
 as nitrous oxide N2O, more commonly
 known as “laughing gas”

A mild anesthetic, also a greenhouse gas
 that contributes to global warming,
 Carbon, C is one of the most common
  elements on Earth.

 Its  found:
4. in the tissues of living organisms
5. in the atmosphere
6. dissolved in ocean water and
7. locked up in limestone deposits that line
   the ocean floor
 Living   organisms provide two important
    steps in the carbon cycle.

r   Plants absorb CO2 from the atmosphere
    to use during photosynthesis
2   Other organisms release CO2 into the air
    during respiration
 In  addition there are several important
    non-organic storage areas of carbon in
    the environment:

a   A large portion is stored in rocks
i   Oceans hold a large amount of CO2
    because it dissolves easily in water
l   Coal, oil and limestone store carbon that
    once form ancient organisms

**burning fossil fuels will release CO2 into
            the atmosphere**
 Photoautotrophsconstantly remove
 carbon dioxide through the process
 photosynthesis.

 Certainbacteria known as
 chemoautotrophs use carbon dioxide to
 synthesize the organic compounds they
 need.
 Thecarbon present in food made by
 plants reaches animals through the food
 chain.

 Carnivorousanimals receive this carbon
 when they eats animals.
 Carbon dioxide is continuously dissolved
 in water bodies by diffusion.

 Once dissolved it either remains in the
 waters or gets converted into carbonates
    -2
 CO3 and bicarbonates HCO3
 Thedissolved carbon dioxide is used by
 plants for photosynthesis.

 Thecarbonates are converted into
 calcium carbonate by certain marine
 organisms.

 Thecalcium carbonate is used by corals
 and oysters to make their shells.

 When  these organisms die their shell
 deposit to the sea floor and eventually
 turn into sedimentary rocks.
 When  plants and animals die and get
 buried under the ground, after millions of
 years they change into fossil fuels due to
 high pressure and other physical and
 chemical changes.
 Carbon  dioxide is regularly returned to
 the atmosphere by the process of
 respiration in plants and animals.

 Burningof wood and fossil fuels in
 industry and automobiles also releases
 carbon dioxide.
 Itabsorbs infrared light. The atmosphere
  absorbs more heat than i

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Nutrient cycles

  • 1.
  • 2.
  • 3.  Nitrogencomprises 78.08 % of the atmosphere making it the largest constituent of the gaseous envelope that surrounds the Earth.  Nitrogenis important in the make up of organic molecules like proteins and DNA.  Mostorganisms cannot use nitrogen in this form, i.e N2
  • 4.  Plantssecure their nitrogen in “fixed” forms i.e incooperated in compounds such as: Nitrate ions NO3 Ammonia NH3 Urea (NH2)2CO  Animalssecure their nitrogen (and all other compounds from plants (or animals that have eaten plants).
  • 5.  Four processes participate in the cycling of nitrogen in the biospere: • Nitrogen fixation • Decay • Nitrification • Denitrification *microorganisms play major roles in all processes*
  • 6.  Thenitrogen molecule is quite inert. To break it apart so that its atoms can combine with other atoms requires the input of substantial amounts of energy.  inert-nonreactive gas during chemical synthesis, analysis or preservation of reactive materials
  • 7.  Three processes are responsible for most of the nitrogen fixation: 1. Atmospheric fixation 2. Biological fixation 3. Industrial fixation
  • 8.  Theenormous energy of lightening breaks nitrogen molecules and enables then to combine with oxygen in the air forming nitrogen oxides.  These dissolve in rain forming nitrates that are carried to the earth.  *contributes 5-8% of total fixed*
  • 9.  Made synthetically via Haber Process.  Nitrogenand hydrogen reacted under great pressure and temperature in the presence of a catalyst to make ammonia.  Ammonia applied directly to farm fields as fertilizers or further processed with oxygen to make nitric acid.
  • 10.  Theability to fix nitrogen is found only in certain bacteria and archaea.  Some live in symbiotic relationship with plants of the legume family Rhizobium  Some establish symbiotic relationships with animals  Some live free in soil
  • 11.  Biological nitrogen fixation requires a complex set of enzymes and a huge expenditure of ATP
  • 12.  Protein made by plants enter and pass through food webs at each level.  Ateach trophic level metabolism produces nitrogen compounds that return to the environment in excretions.  Microorganisms break down the molecules in excretion and dead organisms into ammonia, NH3.
  • 13.  Most of the ammonia produced by decay is converted into nitrates. Bacteria of the genus Nitrosomonas oxidize NH3  nitrites NO2 Bacteria of the genus Nitrobacter oxidize nitrites  nitrates NO3
  • 14.  Thisis the reduction of nitrates to nitrogen gas, thus replenishing the atmosphere  Anaerobic bacteria use nitrates as an alternative to oxygen in their respiratory process.  Closing the nitrogen cycle
  • 15. A side product of this reaction is known as nitrous oxide N2O, more commonly known as “laughing gas” A mild anesthetic, also a greenhouse gas that contributes to global warming,
  • 16.
  • 17.
  • 18.
  • 19.  Carbon, C is one of the most common elements on Earth.  Its found: 4. in the tissues of living organisms 5. in the atmosphere 6. dissolved in ocean water and 7. locked up in limestone deposits that line the ocean floor
  • 20.  Living organisms provide two important steps in the carbon cycle. r Plants absorb CO2 from the atmosphere to use during photosynthesis 2 Other organisms release CO2 into the air during respiration
  • 21.  In addition there are several important non-organic storage areas of carbon in the environment: a A large portion is stored in rocks i Oceans hold a large amount of CO2 because it dissolves easily in water l Coal, oil and limestone store carbon that once form ancient organisms **burning fossil fuels will release CO2 into the atmosphere**
  • 22.  Photoautotrophsconstantly remove carbon dioxide through the process photosynthesis.  Certainbacteria known as chemoautotrophs use carbon dioxide to synthesize the organic compounds they need.
  • 23.  Thecarbon present in food made by plants reaches animals through the food chain.  Carnivorousanimals receive this carbon when they eats animals.
  • 24.  Carbon dioxide is continuously dissolved in water bodies by diffusion.  Once dissolved it either remains in the waters or gets converted into carbonates -2 CO3 and bicarbonates HCO3
  • 25.  Thedissolved carbon dioxide is used by plants for photosynthesis.  Thecarbonates are converted into calcium carbonate by certain marine organisms.  Thecalcium carbonate is used by corals and oysters to make their shells.  When these organisms die their shell deposit to the sea floor and eventually turn into sedimentary rocks.
  • 26.  When plants and animals die and get buried under the ground, after millions of years they change into fossil fuels due to high pressure and other physical and chemical changes.
  • 27.  Carbon dioxide is regularly returned to the atmosphere by the process of respiration in plants and animals.  Burningof wood and fossil fuels in industry and automobiles also releases carbon dioxide.
  • 28.
  • 29.  Itabsorbs infrared light. The atmosphere absorbs more heat than i