Terrestrial N cycling Flashcards

1
Q

how is N transferred

A
  • Mostly below ground - most usable N found in soil
    • Transfers among:
      ○ Plants
      ○ Microbes
      ○ Consumers
      ○ environment
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2
Q

how is N used by plants? what is limiting the rate?

A
  • Diversity of the cycle composition matters
    • most N used by plsnts is from OM decomp (vs other inputs)
    • Conversion of dead OM -> DON by microbes
    • Rate limiting step (dead OM pool> DON pool)
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3
Q

why is N important

A
  • Nitrogen is important in the context of a terrestrial system bc the flow of nitrogen does at some point filter through plant systems etc
    ○ Whereas micronutrients are used in a smaller quantity of the plants and not necessarily filtered thru plants - not driven by terrestrial plants
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4
Q

why are we looking at nutrients?

A

○ When we try to understand global patterns, we have to think about a component that can be extrapolated in order to capture the complexity in models or data sampling
Like following energy or water - give us a generalization for ecological systems - overall picture

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5
Q

how is DON (dissolved organic N) used

A
  • Ultimately the DON is what funnels the nitrogen in the system
    ○ Used by planys, mycorrhizae, microbes
    ○ DON is a bunch of types of nitrogen in a solution - a “soup”
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6
Q

how are microbes limited? how do they use DON to get around it?

A
  • Growth often C limited
    • Break down DON and use C to support energy requirements
    • Secrete ammonium into soil when its in excess
    • Not all NH4+ (ammonium) available to plants (microbe immobilization)
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7
Q

what do microbes do with DON

A

mineralize to NH4 - ammonification, not all available to plants bc microbial immobilization

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8
Q

gross vs net NH4 immobilization

A

Gross NH4+ mineralization (total amount mineralized by microbes regardless of fate) - gross NH4 immobilization (total amount taken up by microbes) = Net NH4+ mineralization (net accumulation of N in soil solution available for plant uptake; N in excess of microbial demand

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9
Q

Critical Net N mineralization threshhold of DON?

A

at C:N>25:1, NH+ is immobilized (net immoblization)
at C:N <25:1, NH4 is mineralized (net mineralization)

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10
Q

why does the critical net N mineralization exist

A

microbial C:N approx 10:1 but inefficient at using C (use 40%; respire 60%)
so substrate (DON) needs C:N of 100:4 (25:1) for net N mineralization
this is a generalization; varies with microbial community

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11
Q

what factors govern temporal and spatial variation in ammonification

A

state factors, interactive controls, indirect controls, direct controls

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12
Q

Graph of nitrogen avail and flux ?

A
  • The more nitrogen in organic matter the more DON there is
    ○ Gross Nmin and NetNmin follow this pattern
    ○ Hence there’s greater nitrification and less immobilization (bc theres more available to them so they don’t require it from the soil)
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13
Q
  • Graph of nitrogen pool and nitrogen avail
A
  • More available with more OM
    • Green is most usable, yellow is highly usable,
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14
Q

fate of NH4 (6)

A
  1. Immobilized by microbes
    1. Taken up by a plant
    2. Absorbed on soil - available
    3. Stabilized on clays or SOM - unavailable
    4. Volatilized as ammonia (NH3) - happens when there is too much ammonium
      Nitrification - oxidation of NH4+ by microbes to nitrite, nitrate (NO2-, NO3-)
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15
Q

what is nitrification? carried out by?

A
  • Oxidation of: NH4+ -> NO2- - e.g. nitrosolobus bacteria
    • Then, NO2- -> NO3- - e.g. nitrobacter bacteria
    • Nitrification- carried out by specific group of autotrophic and heterotrophic microbes (nitrifiers)
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16
Q

controls of nitrification?

A

○ Amount of NH4 - substrate
O2 - most nitrifiers require it

17
Q

trophic ecosystems graph

A

○ Amount of nitrogen available for use by organisms has a 1:1 relationship
§ Any amount is quickly taken up by microbes and used immediately
○ In temperate its 4:1, not immediately utilized by bacteria bc their community is less active due to adaptations, limitations, and temperate conditions

18
Q

fate of nitrates

A
  1. Immobilized by microbes (used up by them)
    1. Taken up by a plant
    2. Leached -> groundwater (more readily leached than NH4)
    3. May absorb in soils
    4. Reduced by denitrifying microbes to Nox, N2O, or N2 (output)
      * Often lost to runoff and ground water bc its soluable
      Gases are particularily important in greenhouse effects