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Anton Cwik, Ethan Sox

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Title: Anton Cwik, Ethan Sox


1
Anton Cwik, Ethan Sox
  • Per. 4

2
BIOGEOCHEMICAL CYCLES
3
Fundamentals of biogeochemical cycles
  • All matter cycles...it is neither created nor
    destroyed...
  • As the Earth is essentially a closed system with
    respect to matter, we can say that all matter on
    Earth cycles .
  • Biogeochemical cycles the movement (or cycling)
    of matter through a system

4
  • by matter we mean elements (carbon, nitrogen,
    oxygen) or molecules (water) so the movement of
    matter (for example carbon) between these parts
    of the system is, practically speaking, a
    biogeochemical cycle
  • The Cycling Elements macronutrients required
    in relatively large amounts "big six"
  • carbon , hydrogen , oxygen , nitrogen ,
    phosphorous sulfur

5
  • other macronutrients
  • potassium , calcium , iron , magnesium
    micronutrients required in very small
    amounts, (but still necessary) boron (green
    plants) copper (some enzymes) molybdenum
    (nitrogen-fixing bacteria)

6
ATMOSPHERE
7
LITHOSPHERE
8
HYDROSPHERE
9
ECOSPHERE
10
6 of the most important cycles are the water,
carbon, nitrogen, sulfur, phosphorus and oxygen.
11
1. Which part of the atmosphere has the highest
altitude?A. Troposphere B. Stratosphere C.
Thermosphere D. Mesosphere2. Which part
includes all three of the other
parts?Lithosphere B. Ecosphere C. Hydrosphere D.
Atmosphere3. Which one is not a major cycle?A.
Hydrogen B. Nitrogen C. Oxygen D. Sulfur E. Water
12
HYDROLOGIC CYCLE
13
HYDROLOGIC CYCLE
CONNECTS ALL OF THE CYCLES AND SPHERES TOGETHER
14
HUMAN IMPACTS TO WATER CYCLE
  • Water withdrawal from streams, lakes and
    groundwater. (salt water intrusion and
    groundwater depletion)
  • Clear vegetation from land for agriculture,
    mining, road and building construction. (nonpoint
    source runoff carrying pollutants and reduced
    recharge of groundwater)
  • Degrade water quality by adding nutrients(NO2,
    NO3, PO4) and destroying wetlands (natural
    filters).
  • Degrade water clarity by clearing vegetation and
    increasing soil erosion.

15
Water Quality Degradation
16
MARINE CARBON CYCLE
17
TERRESTRIAL CARBON CYCLE
18
Explain
19
Carbon in Oceans
  • Additional carbon is stored in the ocean.
  • Many animals pull carbon from water to use in
    shells, etc.
  • Animals die and carbon substances are deposited
    at the bottom of the ocean.
  • Oceans contain earths largest store of carbon.

20
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21
IMPORTANCE OF CARBON CYCLE
CARBON IS THE BACKBONE OF LIFE!
22
1. What is no part of the water cycle?A.
Precipitation B. Percolation C. Transpiration D.
Surface Runoff E. Boiling2. Which is
not a man made way of adding carbon to the carbon
cycle?A. Airplanes B. Natural Fires C. Cars D.
Burning fossil fuels3. What are the predictions
for how much carbon will be added from fossil
fuels?A. Low B. Medium-Low C. Medium D. High
23
The Nitrogen Cycle
24
Sources
  • Lightning
  • Inorganic fertilizers
  • Nitrogen Fixation
  • Animal Residues
  • Crop residues
  • Organic fertilizers


25
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26
Forms of Nitrogen
  • Urea ? CO(NH2)2
  • Ammonia ? NH3 (gaseous)
  • Ammonium ? NH4
  • Nitrate ? NO3
  • Nitrite ? NO2
  • Atmospheric Dinitrogen ?N2
  • Organic N

27
Global Nitrogen Reservoirs
28
Roles of Nitrogen
  • Plants and bacteria use nitrogen in the form of
    NH4 or NO3-
  • It serves as an electron acceptor in anaerobic
    environment
  • Nitrogen is often the most limiting nutrient in
    soil and water.

29
Nitrogen is a key element for
  • amino acids
  • nucleic acids (purine, pyrimidine)
  • cell wall components of bacteria (NAM).

30
Nitrogen Cycles
  • Ammonification/mineralization
  • Immobilization
  • Nitrogen Fixation
  • Nitrification
  • Denitrification

31
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32
Which of the following is not part of the
Nitrogen Cycle? A) Ammonification B)
Nitrification C) Denitrosation D) Nitrogen
Fixation E) Denitrification
In what form(s) do plants and bacteria use
nitrogen? A) NH4 B) NH3 C) NO3- D) A and
C E) All of the above
What is the molecular formula for ammonium? A)
NH4 B) NH3 C) NO3 D) NO2 E) none of the above
33
Ammonification or Mineralization
N2
N2O
NH4
NO2
R-NH2
NO
NO2
NO3
34
Mineralization or Ammonification
  • Decomposers earthworms, termites, slugs, snails,
    bacteria, and fungi
  • Uses extracellular enzymes ? initiate degradation
    of plant polymers
  • Microorganisms uses
  • Proteases, lysozymes, nucleases to degrade
    nitrogen containing molecules

35
  • Plants die or bacterial cells lyse ? release of
    organic nitrogen
  • Organic nitrogen is converted to inorganic
    nitrogen (NH3)
  • When pHlt7.5, converted rapidly to NH4
  • Example
  • Urea NH3 2 CO2

36
Immobilization
  • The opposite of mineralization
  • Happens when nitrogen is limiting in the
    environment
  • Nitrogen limitation is governed by C/N ratio
  • C/N typical for soil microbial biomass is 20
  • C/N lt 20 ?Mineralization
  • C/N gt 20 ?Immobilization

37
Nitrogen Fixation
N2
N2O
NH4
NO2
R-NH2
NO
NO2
NO3
38
Nitrogen Fixation
  • Energy intensive process
  • N2 8H 8e- 16 ATP 2NH3 H2 16ADP 16
    Pi
  • Performed only by selected bacteria and
    actinomycetes
  • Performed in nitrogen fixing crops
  • (ex soybeans)

39
Microorganisms fixing
  • Azobacter
  • Beijerinckia
  • Azospirillum
  • Clostridium
  • Cyanobacteria
  • Require the enzyme nitrogenase
  • Inhibited by oxygen
  • Inhibited by ammonia (end product)

40
Rates of Nitrogen Fixation
41

42
Immobilization is the opposite of which process
in the cycle? A) Mineralization B)
Nitrification C) Immobilization D) Nitrogen
Fixation E) Denitrification
What process takes place when nitrogen is
limiting in the environment? A)
Mineralization B) Nitrification C)
Immobilization D) Nitrogen Fixation E)
Denitrification
Which has the highest rate of nitrogen
fixation? A) Rhizobium-legume B)
Cynaobacteria-moss C) Rhizosphere
associations D) Free-living E) Azobacter
43
Applications to wetlands
  • Occur in overlying waters
  • Aerobic soil
  • Anaerobic soil
  • Oxidized rhizosphere
  • Leaf or stem surfaces of plants

44
Bacterial Fixation
  • Occurs mostly in salt marshes
  • Is absent from low pH peat of northern bogs
  • Cyanobacteria found in waterlogged soils

45
Nitrification
N2
N2O
NH4
NO2
R-NH2
NO
NO3
NO2
46
Nitrification
  • Two step reactions that occur together
  • 1rst step catalyzed by Nitrosomonas
  • 2 NH4 3 O2 ? 2 NO2- 2 H2O 4 H
  • 2nd step catalyzed by Nitrobacter
  • 2 NO2- O2 ? 2 NO3-

47
  • Optimal pH is between 6.6-8.0
  • If pH lt 6.0 ? rate is slowed
  • If pH lt 4.5 ? reaction is inhibited

In which type of wetlands do you thing
Nitrification occurs?
48
Denitrification
N2
N2O
NH4
NO2
R-NH2
NO
NO2
NO3
49
Denitrification
  • Removes a limiting nutrient from the environment
  • 4NO3- C6H12O6? 2N2 6 H20
  • Inhibited by O2
  • Not inhibited by ammonia
  • Microbial reaction
  • Nitrate is the terminal electron acceptor

50
Looking at the Nitrogen cycle through the eye of
NH4
51
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52
Denitrication is inhibited by A) NH3 B)
NH4 C) NO2- D) O2
The second step of Nitrification is catalyzed
by A) Nitrosomonas B) Clostridium C)
Azobacter D) Nitrobacter E) Beijerinckia
Which pH is within the optimal range for
nitrication? A) 1.5 B) 4.6 C) 7.1 D) 8.7 E)
10.9
53
Surface water
Low NH4
Oxidized layer
Biodegradation
Reduced soil layer
Slow Diffusion
C/N lt20
C/N gt20
NH4 HIGH
54
Surface water
nitrification
Low NH4
Oxidized layer
NO3 high
Reduced soil layer
Slow Diffusion
NH4 HIGH
55
N2
Surface water
Oxidized layer
NO3 high
Leaching
Reduced soil layer
NO3 Low
Denitrification
56
PHOSPHOROUS CYCLE
57
HUMAN IMPACTS TO PHOSPHOROUS CYCLE
  • Humans mine LARGE quantities of phosphate rock to
    use in commercial fertilizers and detergents.
    Phosphorous is NOT found as a gas, only as a
    solid in the earths crust. It takes millions to
    hundreds of millions of years to replenish.
  • Phosphorous is held in the tissue of the trees
    and vegetation, not in the soil and as we
    deforest the land, we remove the ability for
    phosphorous to replenish globally in ecosystems.
  • Cultural eutrophication ad excess phosphate to
    aquatic ecosystems in runoff of animal wastes
    from livestock feedlots, runoff of commercial
    phosphate fertilizers fro cropland, and discharge
    of municipal sewage.

58
IMPORTANCE OF PHOSPHOROUS CYCLE
  • 1.Phosphorous is an essential nutrient of both
    plants and animals.
  • 2. It is part of DNA molecules which carry
    genetic information.
  • 3. It is part of ATP and ADP) that store
    chemical energy for use by organisms in cellular
    respiration.
  • 4. Forms phospholipids in cell membranes of
    plants and animal cells.
  • 5. Forms bones, teeth, and shells of animals as
    calcium phosphate compounds.

59
SULFUR CYCLE
60
HUMAN IMPACTS TO SULFUR CYCLE
  • Approximately 1/3 of all sulfur emitted into
    atmosphere comes from human activities.
  • 1. Burning sulfur containing coal and oil to
    produce electric power (SOx acid deposition).
  • 2. Refining petroleum (SOx emissions)
  • 3. Smelting to convert sulfur compounds of
    metallic minerals into free metals (Cu, Pb, Zn)
  • 4. Industrial processing.

61
IMPORTANCE OF SULFUR CYCLE
  • Sulfur is a component of most proteins and some
    vitamins.
  • Sulfate ions (SO4 2- ) dissolved in water are
    common in plant tissue. They are part of
    sulfur-containing amino acids that are the
    building blocks for proteins.
  • Sulfur bonds give the three dimensional structure
    of amino acids.
  • Many animals, including humans, depend on plants
    for sulfur-containing amino acids.

62
The Oxygen cycle
63
1. The Phosphorus Cycle takesA. Short time B. 20
years to fully cycle through C. 100 years to
cycle through D. Geological Timescal2. What
percentage of sulfur is emmited buy human
activity?A. .01 B. 20 C. 33.3 D. 66.7 E.
Over 903. The vast majority of oxygen in the
ecosphere is inA. Outer space B. Lithosphere C.
Atmosphere D. Hydrosphere
64
PHOTOSYNTHESIS
Photosynthesis occurs within the chloroplasts
of green plants. The photosynthetic membranes
are arranged in flattened sacs called the
thylakoids. 6CO2 12H2O C6H12O6 6O2
6H2O light
(reactants) (products) Function Chemical
energy Storage for cell use
65
CELLULAR RESPIRATION
Cellular Respiration occurs in light
simultaneously with photosynthesis. It occurs in
the cytoplasm and mitochondria. It is the reverse
reaction of photosynthesis. Function chemical
energy release
C6H12O6 6O2 6H2O 6CO2 12H2O
chemical energy (reactants) (products)
66
Primary Productivity Connection
  • Gross Primary Productivity (GPP) the rate at
    which an ecosystems producers capture and store
    a given amount of chemical energy as biomass in a
    given period of time.
  • Net Primary Productivity (NPP) the rate at
    which all the plants in an ecosystem produce net
    useful energy equal to the difference between
    energy produced through photosynthesis and energy
    used for cellular respiration.

67
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68
GOOD OZONE UP HIGH
69
PHOTOCHEMICAL SMOGBAD OZONE DOWN LOW
70
OZONE DEPLETION
71
ACID DEPOSITION
72
CULTURAL EUTROPHICATION
73
Cultural Eutrophication Anoxia
  • Eutrophication natural process over 1000s of
    years, lakes fill in with sediment, become
    marshes then dry land
  • Cultural Eutrophication same process, but
    speeded enormously by loading with limiting
    nutrients (typically P, sometimes N)
  • Problems associated with cultural eutrophication
  • Algal blooms
  • Water anoxia

74
ROCK CYCLE
75
HUMAN IMPACTS ON THE ROCK CYCLE
  • 1. Humans are excavating minerals and removing
    rock material. It takes millions of years for
    rock to form.
  • 2. Humans remove sediments for building
    materials. This removes sediments that may form
    sedimentary rocks in the future.
  • 3. Humans are filling in wetlands (peatlands),
    area that will form future coal beds.

76
1. Which part of the atmosphere is the ozone
layer right above?A. Stratosphere B. Troposphere
C. Mesosphere D. Thermosphere2. How long does
it take rock formations to form?A. 1,000 years
B. 10,000 years C. 100,000 years D. 1,000,000
years E. 10,000,000 years3. What is cultural
eutrophication good for?A. Fish B. Dissolved
Oxygen in the lake C. algae D. clear lake
77
Works Cited
  • http//science.pppst.com/carboncycle.html
  • westernreservepublicmedia.org/earthmotion3/images/
    Carbon_Cycle.ppt
  • clima-dods.ictp.it/d3/annalisa/ocean_sv/lecture1.p
    pt
  • www.geology.wmich.edu/Koretsky/envs2150/Pcycle_1.p
    pt
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