Terrestrial Ecology Flashcards

(33 cards)

1
Q

process that makes N2 biologically available

A

Nitrogen fixation

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2
Q

Haber process

A

uses energy from fossil fuels to convert N2 to ammonia for fertilizers
fixes more nitrogen than any other anthropogenic process

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3
Q

Sources of N2O

A

Nitrification and denitrification in oceans and tropical soils

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4
Q

Sources of NH3

A

Domestic animals. ammonia is important for aerosol formation. Most ammonia returns to the earth in precipitation

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5
Q

Largest terrestrial source of NO

A

Nitrification- from soils

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6
Q

most NOx deposition occurs in

A

temperate zones

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7
Q

How does NOx impact concentrations of other gases

A

NO affects the concentration of OH, which is the main oxidizing and cleaning agent in the atmosphere, so it impacts concentrations of other gases

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8
Q

Impacts of nitrogen deposition

A

increased plant growth, decreased plant biodiversity, soil acidification, increased invasive species, increased damages from pests and frost, and increased N leaching to water bodies
may stimulate carbon uptake and storage
alter species dominance and competition, reduce diversity

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9
Q

Nitrogen accumulation

A

plant production is limited by nitrogen (in most environments)-so they retain nitrogen that is deposited in ecosystems

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10
Q

Nitrogen saturation

A

After a lot of nitrogen inputs, nitrogen supply exceeds demands. Associated with declines in forest productivity and increased mortality. Causes nitrogen losses.

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11
Q

Nitrogen losses

A

Caused by nitrogen saturation, losses to stream water, ground water, and atmosphere.
Bad effects on plant and soil processes

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12
Q

Nitrogen availabilty/losses In tropics-

A

nitrogen availability is high relative to demands- deposition can immediately cause nitrogen losses

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13
Q

Four carbon pools that affect carbon cycling

A

land, atmosphere, oceans, sediments

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14
Q

Terrestrial nutrient cycling: nitrogen inputs

A

Nitrogen fixation is main pathway for new nitrogen to enter an ecosystem

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15
Q

Nitrogen fixers

A

bacteria that fix N2 –> NH4+, NH4+ is biologically available and used for growth. Nitrogen that is fixed by nitrogen fixers becomes available to others through litter/decomp

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16
Q

Nitrogenase

A

enzyme that catalyzes the reduction of N2 to NH4. Has high energy requirement- only when bacterium has abundant carbohydrate supply.

17
Q

Symbiotic relationship between nitrogen fixers and plants

A

Plants provide carbohydrates, bacteria reside in root nodules- protected from O2. These have highest rates of nitrogen fixation

18
Q

Limitations on Nitrogen fixation

A

In closed canopy ecosystems- energy availability can constrain nitrogen fixation. Nitrogen fixation can be limited to high light environments, early succession, or limited canopy developments. Can also be limited by carbon, or other nutrients like phosphorus

19
Q

Conifer vs deciduous

A

Deciduous: broad leaves, flowers

Conifer: Needles/pines, cones

20
Q

HNO3 deposition

A

acidifies soil base cations leach from ecosystem.

21
Q

Internal cycling of nitrogen

A

Most nitrogen is available through decomposition. Most soil nitrogen is contained in dead matter. Microbes break down dead organic matter and release nitrogen as dissolved organic nitrogen (DON)

22
Q

Immobilization

A

Removal of inorganic nitrogen from the available pool by microbial uptake and chemical fixation. inorganic –> organic.
Microbes can take up NO3 and NH4+, but take up NH4+ more.

23
Q

Nitrifcation

A

Conversion of ammonium to nitrate-
nitrite acts as intermediate

NH4+ oxidized to NO2- and then NO3-

carried out by hetero and autotrophic nitrifiers

24
Q

nitrogen mineralization or ammonification

A

microbial growth is nitrogen limited, they secrete NH4+ into the soil,

25
Rate limiting step of nitrogen mineralization
conversion of insoluble organic nitrogen to dissolved organic nitrogen- there are pools of insoluble nitrogen in soils
26
Nitrogen limited microbes
Absorb or immobilize ammonium- immobilization
27
Carbon limited microbs
Secrete NH4+ as waste
28
Gross Mineralization
total amount of nitrogen released via mineralization | -regardless of if its absorbed or not
29
Net mineralization
net accumulation of inorganic nitrogen occurs when microbial growth is more carbon limited than nitrogen limited approximately equal to nitrogen uptake by vegetation
30
Most important determinant of the nitrification rate
Availability of NH4+
31
Gaseous nitrogen loss from ecosystems
ammonia volatilization, nitrification, denitirification. Ammonia gas can be emitted from soils and senescing leaves
32
NH3 flux from ecosystems
NH3 flux is low from most ecosystems- NH4+ maintained at low concentrations by plant and microbial uptake and binding to soil complexes. NH3 fluxes are large in ecosystems where NH4+ accumulates due to large nitrogen inputs.
33
NO2-
can be absorbed through leaves and used in metabolism, or deposited in particulate form