Terrestrial N cycling Flashcards
how is N transferred
- Mostly below ground - most usable N found in soil
- Transfers among:
○ Plants
○ Microbes
○ Consumers
○ environment
- Transfers among:
how is N used by plants? what is limiting the rate?
- 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)
why is N important
- 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
why are we looking at nutrients?
○ 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
how is DON (dissolved organic N) used
- 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”
how are microbes limited? how do they use DON to get around it?
- 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)
what do microbes do with DON
mineralize to NH4 - ammonification, not all available to plants bc microbial immobilization
gross vs net NH4 immobilization
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
Critical Net N mineralization threshhold of DON?
at C:N>25:1, NH+ is immobilized (net immoblization)
at C:N <25:1, NH4 is mineralized (net mineralization)
why does the critical net N mineralization exist
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
what factors govern temporal and spatial variation in ammonification
state factors, interactive controls, indirect controls, direct controls
Graph of nitrogen avail and flux ?
- 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)
- Graph of nitrogen pool and nitrogen avail
- More available with more OM
- Green is most usable, yellow is highly usable,
fate of NH4 (6)
- Immobilized by microbes
- Taken up by a plant
- Absorbed on soil - available
- Stabilized on clays or SOM - unavailable
- Volatilized as ammonia (NH3) - happens when there is too much ammonium
Nitrification - oxidation of NH4+ by microbes to nitrite, nitrate (NO2-, NO3-)
what is nitrification? carried out by?
- 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)