Nitrogen and Ecosystem Nutrient Cycling
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Nitrogen and Ecosystem Nutrient Cycling. Nicole and Sarah Biogeochemistry of Northern Ecosystems March 2005. Cycling Essential Life Elements. Interactions between plants, animals, and soil microbes link the internal biogeochemistry of terrestrial ecosystems. Essential life elements:

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Nitrogen and Ecosystem Nutrient Cycling

Nicole and Sarah

Biogeochemistry of Northern Ecosystems

March 2005


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Cycling Essential Life Elements

  • Interactions between plants, animals, and soil microbes link the internal biogeochemistry of terrestrial ecosystems.

  • Essential life elements:

    C, N, P, S, P, Ca, Mg, F

    -often limiting and their supply may control NPP

  • Biosphere exerts strong control on major life elements-

    intrasystem cycle is the annual cycle of nutrients in vegetation and is responsible for long-term retention of elements


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Annual Nutrient Requirements for Growth

(Schlesinger, 1997 p.168)


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General Nitrogen Information

  • Out of those elements required to sustain life, Nitrogen has the greatest total

    abundance in the atmosphere, biosphere, and hydrosphere but it is the least

    readily available to sustain life.

  • In the form of molecular nitrogen, two nitrogen atoms are held together by a

    triple bond. Only a small number of N-fixing species have the energy required to

    break apart this bond.

  • There are two categories of Nitrogen in nature, N which is the non-reactive

    molecular form of nitrogen and Nr which is all the reactive nitrogen in the earths

    atmosphere and biosphere.

  • Reactive nitrogen was originally formed by one of two ways: lightning or

    biological fixation.


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The Nitrogen Cycle

Note: Nitrous oxide is N20.



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Denitrification

  • Denitrification is the loss of Nr from

    the biosphere because of its

    conversion back to its molecular

    form, with a triple bond.

  • Three conditions required: 1)

    presence of NO3- or nitrate, 2)

    availability of labile organic matter,

    and 3) absence or low

    concentration oxygen.

  • The residence time of water is an

    important factor in controlling how

    much denitrification goes on.

  • Denitrification is an effective sink

    for N

  • Denitrification can control

    phytoplankton blooms and degree

    of eutrophication


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Denitrification Reduces the Downstream N Transport (Galloway et al, 2003)

Land

30-70% entering rivers denitrified

Rivers

10-80% entering estuaries denitrified

Estuaries

Cont.

Shelves

>80% entering shelves denitrified

?


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How Humans Have Impacted the Nitrogen Cycle

  • Three main causes of the global increase in Nr:

  • Cultivation of plants associated with n-fixers (e.g. legumes) increasing BNF

  • Industrial N Fixation by the Haber-Bosch process- (fertilizer and bombs)

1. Generate Hydrogen

CH4+H2ONi catalystCO+3H2

React H2 + N2 to produce NH3

N2 + 3H22NH3

3. Fossil Fuel burning- converts non reactive N into NOx


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billion

x1012 g yr-1

Haber-Bosch

World population

Crop Fixation

Fossil Fuel


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Discussion Questions

Hypothetical Situation

  • A farmer lives in close proximity to the watershed of a major river which feeds into the ocean. He uses nitrogen fertilizer to increase his crop yield. In an effort to become more eco-friendly he wants to know what effect his farm will have on the surrounding ecosystem and its nitrogen cycle? Suggest possible ways he can improve his farming practices and maintain economic stability.

  • Since the industrial revolution there has been a dependency on the burning of fossil fuels for energy. One of the effects of this process is the release of NOx to the atmosphere. How is NOx created and what are the implications of its presense in the atmosphere?


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Discussion Questions- Potential Ecosystem Effects

Agriculture

Fossil Fuel

  • Initially release of NOx in troposphere

  • produces ozone (health implications)

  • Increases accumulation of small

  • particles in air- decreases atmospheric

  • visibility

  • Acid precipitation and N deposition

  • N2O emitted back to atmosphere can

  • first contribute to greenhouse warming

  • N2O in the stratosphere can deplete

  • ozone layer

  • Over saturation of N leads to high

  • N loss from system to soil,

  • atmosphere and water

  • Inputs of Nr exceeds the systems

  • ability to remove N through

  • denitrification

  • transported N can alter species

  • composition and trophic structure

  • in surrounding ecosystems

  • High levels of N can degrade

  • habitats (e.g. eutrophication,

  • areas of anoxia and hypoxia)



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Nitrogen Saturation and Ecosystem Degradation

  • Inputs of N from the atmosphere in the northeastern U.S. are 5 to 20 times

    higher than those under pristine conditions (10-50kg N ha-1yr-1)

  • Added N may be accumulated in organic matter however, forest decline is

  • observed as the ecosystem becomes saturated with N


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Discussion Questions- Potential Solutions

Agriculture

Fossil Fuel

?ideas

?ideas


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