Terrestrial Ecology Flashcards
(33 cards)
process that makes N2 biologically available
Nitrogen fixation
Haber process
uses energy from fossil fuels to convert N2 to ammonia for fertilizers
fixes more nitrogen than any other anthropogenic process
Sources of N2O
Nitrification and denitrification in oceans and tropical soils
Sources of NH3
Domestic animals. ammonia is important for aerosol formation. Most ammonia returns to the earth in precipitation
Largest terrestrial source of NO
Nitrification- from soils
most NOx deposition occurs in
temperate zones
How does NOx impact concentrations of other gases
NO affects the concentration of OH, which is the main oxidizing and cleaning agent in the atmosphere, so it impacts concentrations of other gases
Impacts of nitrogen deposition
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
Nitrogen accumulation
plant production is limited by nitrogen (in most environments)-so they retain nitrogen that is deposited in ecosystems
Nitrogen saturation
After a lot of nitrogen inputs, nitrogen supply exceeds demands. Associated with declines in forest productivity and increased mortality. Causes nitrogen losses.
Nitrogen losses
Caused by nitrogen saturation, losses to stream water, ground water, and atmosphere.
Bad effects on plant and soil processes
Nitrogen availabilty/losses In tropics-
nitrogen availability is high relative to demands- deposition can immediately cause nitrogen losses
Four carbon pools that affect carbon cycling
land, atmosphere, oceans, sediments
Terrestrial nutrient cycling: nitrogen inputs
Nitrogen fixation is main pathway for new nitrogen to enter an ecosystem
Nitrogen fixers
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
Nitrogenase
enzyme that catalyzes the reduction of N2 to NH4. Has high energy requirement- only when bacterium has abundant carbohydrate supply.
Symbiotic relationship between nitrogen fixers and plants
Plants provide carbohydrates, bacteria reside in root nodules- protected from O2. These have highest rates of nitrogen fixation
Limitations on Nitrogen fixation
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
Conifer vs deciduous
Deciduous: broad leaves, flowers
Conifer: Needles/pines, cones
HNO3 deposition
acidifies soil base cations leach from ecosystem.
Internal cycling of nitrogen
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)
Immobilization
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.
Nitrifcation
Conversion of ammonium to nitrate-
nitrite acts as intermediate
NH4+ oxidized to NO2- and then NO3-
carried out by hetero and autotrophic nitrifiers
nitrogen mineralization or ammonification
microbial growth is nitrogen limited, they secrete NH4+ into the soil,