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The Nitrogen Cycle

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Deficiencies are world wide, in cultivated. and natural environments ... a bacteria called cyanobacteria) is an important free-living nitrogen fixer ... – PowerPoint PPT presentation

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Title: The Nitrogen Cycle


1
The Nitrogen Cycle
  • Aquatic Ecology

2
Forms of Nitrogen
  • Urea ? CO(NH2)2
  • Ammonia ? NH3 (gaseous)
  • Ammonium ? NH4
  • Nitrate ? NO3
  • Nitrite ? NO2
  • Atmospheric Dinitrogen ?N2
  • Organic N

3
Nitrogen History
  • More money and effort are spent on the
  • management of N and S than any other
  • mineral nutrient
  • Deficiencies are world wide, in cultivated
  • and natural environments
  • Excesses cause a degradation of the
  • quality of live, N pollution

4
Nitrogen History
  • Adding N to soils is one of the most
  • costly parts or agriculture

5
Significance of N
  • Nitrogen (N) is an essential component of
  • DNA, RNA and proteins, the building blocks
  • of life
  • All organisms require nitrogen to live and
  • grow
  • Although the majority of the air we breathe is
  • N2, most of the nitrogen in the atmosphere is
  • unavailable for use by organisms
  • This is because the strong triple bond
  • between the N atoms in N2 molecules makes
  • it relatively inert

6
Significance of N
  • Nitrogen is an incredibly versatile
  • element, existing in both inorganic and
  • organic forms as well as many different
  • oxidation states
  • The movement of nitrogen between the
  • atmosphere, biosphere and geosphere
  • in different forms is described by the
  • nitrogen cycle

7
Significance of N
  • N2 gas must first be converted to more a
  • chemically available form such as ammonium
  • (NH4), nitrate (NO3-), or organic nitrogen
  • (e.g. urea - (NH3)2CO)
  • The inert nature of N2 means that biologically
  • available nitrogen is often in short supply in
  • natural ecosystems, limiting plant growth and
  • biomass accumulation

8
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9
Chemistry of N
10
Chemistry of N
  • The valence range which N undergoes
  • in its biogeochemical cycling is full
  • Going from loss of all five of its outer shell
  • electrons (5) to other elements
  • To the gain of three electrons from other
  • elements (-3) to complete all of the orbitals
  • of its outer electron shell

11
Chemistry of N
  • On the right-hand side of the depicted N
  • cycle, the N atom can eventually lose all
  • five of its outer shell electrons to O
  • With this, N can eventually become fully
  • oxidized as nitrate (NO3-)

12
Chemistry of N
  • On the left-hand of the depicted N cycle, N
  • can eventually add three electrons to fill all of
  • its outer shell electron orbitals from elements
  • such as hydrogen (H) and carbon (C)
  • With such gain of electrons, N can be fully
  • reduced to ammonia (NH3) - which most
  • commonly exists in its ionic form, ammonium
  • (NH4)
  • Or N can be fully-to-partially reduced in
  • organic compounds

13
Nitrogen Cycle - Animation
14
6 Important Processes
  • Nitrogen fixation
  • Nitrogen uptake/Assimilation
  • Nitrogen mineralization
  • Nitrification
  • Denitrification
  • Volatilization

15
Nitrogen Fixation
N2
N2O
NH4
NO2
R-NH2
NO
NO2
NO3
16
Nitrogen fixation
  • N2 ? NH4
  • N2 is converted to ammonium
  • Essential because it is the only way that
  • organisms can attain nitrogen directly from the
    atmosphere
  • Energy intensive process
  • N2 8H 8e- 16 ATP 2NH3 H2 16ADP 16
    Pi

17
Nitrogen fixation
  • Certain bacteria, Rhizobium, are the only
  • organisms that fix nitrogen through metabolic
  • processes
  • N fixing bacteria often form symbiotic
  • relationships with host plants (e.g. beans,
  • peas, and clover)
  • N fixing bacteria inhabit legume root nodules
  • and receive carbohydrates and a favorable
  • environment from their host plant in exchange
  • for some of the nitrogen they fix

18
N fixation w/ Blue-Green Algae
  • In aquatic environments, blue-green algae (really
    a bacteria called cyanobacteria) is an important
    free-living nitrogen fixer

Anacystis bloom Ford Lake August 2002.
19
Measuring water transparency with a Secchi disk
on Ford Lake during a bloom of Aphanizomenon.
August 2004.
20
Nitrogen fixation in Cyanobacteria
  • Nitrogen fixation occurs in special cells called
    heterocysts, but
  • Not all cyanobacteria have heterocysts or can fix
    nitrogen
  • Some cyanobacteria can fix nitrogen without
    heterocysts

www.bio.purdue.edu/people/faculty/sherman/ShermanL
ab
www.micrographia.com/specbiol/bacteri/bacter/bact0
200/anabae03.jpg
21
N Fixation Contd
  • ½ can be contributed by N-fixing org.
  • The rest comes from atmospheric deposition
    (lightning) or runoff.
  • Salmon
  • Alders

22
Nitrification
N2
N2O
NH4
NO2
R-NH2
NO
NO3
NO2
23
Nitrification
  • NH4 ? NO3- or NO2
  • Some of the ammonium produced by
  • decomposition is converted to nitrate via a
  • process called nitrification Nitrosomonas and
    Nitrobacter
  • The bacteria that carry out this reaction gain
  • energy
  • Requires the presence of oxygen
  • circulating or flowing waters and the very
    surface
  • layers of soils and sediments

24
Methemoglobinemia
  • Nitrate is one of the most common groundwater
    contaminants in rural areas.
  • It is regulated in drinking water primarily
    because excess levels can cause
    methemoglobinemia, or "blue baby" disease.
  • Affects nursing infants b/c gut is too acidic (pH
    2) for denitrifying bacteria to reduce nitrate to
    nitrite.
  • Nitrite combines w/ hemoglobin to produce
    methemoglobin, does not break down easily or
    carry Oxygen.

25
Methemoglobinemia
  • Nitrate in groundwater originates primarily from
    fertilizers, septic systems, manure storage or
    spreading operations.
  • Fertilizer nitrogen that is not taken up by
    plants, volatilized, or carried away by surface
    runoff leaches to the groundwater in the form of
    nitrate (nitrification NH4 ? NO3).
  • This not only makes the nitrogen unavailable to
    crops, but also can elevate the concentration in
    groundwater above the levels acceptable for
    drinking water quality.
  • Nitrogen from manure similarly can be lost from
    fields, barnyards, or storage locations.
  • Septic systems also can elevate groundwater
    nitrate concentrations because they remove only
    half of the nitrogen in wastewater, leaving the
    remaining half to percolate to groundwater.

26
Denitrification
N2
N2O
NH4
NO2
R-NH2
NO
NO2
NO3
27
Denitrification
  • NO3- ? N2 ? N2O
  • Oxidized forms of nitrogen such as nitrate and
    nitrite (NO2-) are converted to dinitrogen (N2)
    and, to a lesser extent, nitrous oxide gas
  • An anaerobic process that is carried out by
    denitrifying bacteria, which convert nitrate to
    dinitrogen in the following sequence
  • NO3- ? NO2- ? NO ? N2O ? N2.

28
Denitrification
  • Effluent of sewage treatment plants.
  • Denitrification by bacteria converts
    nitrogen-oxygen compounds into nitrogen gas.
  • N leaves treatment plant as a gas to reduce the
    amount of DIN in effluent.
  • USBF (Upflow Sludge Blanket Filtration)

29
N Uptake/Assimilation
  • NH4 ? Organic N
  • The ammonia produced by nitrogen fixing
  • bacteria is usually quickly incorporated into
  • protein and other organic nitrogen
  • compounds, either by a host plant, the
  • bacteria itself, or another soil organism
  • When organisms nearer the top of the food
  • chain eat, they are using nitrogen that has
  • been fixed initially by nitrogen fixing bacteria

30
Ammonification or Mineralization
N2
N2O
NH4
NO2
R-NH2
NO
NO2
NO3
31
Ammonification/Mineralization
  • Organic N ? NH4
  • After nitrogen is incorporated into organic
  • matter, it is often converted back into
  • inorganic nitrogen,
  • During this process, usually called decay, a
  • significant amount of the nitrogen contained
  • within the dead organisms is converted to
  • ammonium
  • Once in the form of ammonium, nitrogen is
  • available for use by plants

32
Ammonia Volatilization
  • The process of nitrogen loss as ammonia gas
    from urea forms under alkaline conditions
  • During this process, ammonium is converted into
    NH3 gas which is then lost to the air
  • In cooler conditions the enzyme breaks down
    urea much slower
  • Thus, little ammonia gas is lost when urea is
    applied to cool soils
  • Urea may originate from animal manure, urea
    fertilizers and, to a lesser degree, the decay of
    plant materials.

33
Nitrogen Excretion
  • N compounds are metabolized by animals for energy
    NH3 is a waster product.
  • If O2 is present oxidized to NO3 or NO4
  • If O2 is absent NH3 will accumulate.
  • Aquatic Snails N is excreted by diffusion of
    (highly toxic) ammonia NH3 into the water.
  • Terrestrial Snails excrete N as cyclic C-N
    compounds (uric acid) b/c NH3 cannot be easily
    washed away. NH3 would poison their lungs.

34
Nitrogen Excretion
  • Urea HN(CH3)2 - Excreted if animal is too large
    to excrete NH4 water is available.
  • Less toxic than NH4
  • Fishes excrete waste as urea

35
Nitrogen Cycle in Lakes
36
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37
Aquarium N Cycle
38
Tank Cycling
  • New System Cycle tank using live rock
  • If the ph is under 7, you will have ammonium. If
    the ph is 7 or higher you will have ammonia.
  • Nitrates are not as harmful to tropical fish as
    ammonia or nitrites, but nitrate is still harmful
    in large amounts.
  • Tropical Tank Setup Website
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