Changes in the Global Nitrogen Cycle: Causes and Consequences - PowerPoint PPT Presentation

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Changes in the Global Nitrogen Cycle: Causes and Consequences

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The impacts of human domination of the nitrogen cycle that we have identified ... Nitric Oxide (80% from human activities) ... Ammonia (70% from human activity) ... – PowerPoint PPT presentation

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Title: Changes in the Global Nitrogen Cycle: Causes and Consequences


1
Changes in the Global Nitrogen Cycle Causes and
Consequences
  • Taken largely from
  • Human Alteration of the Global Nitrogen
    CycleCauses and Consequences
  • Issues in Ecology Number 1 Spring 1997
  • by
  • Peter M. Vitousek, Chair, John Aber, Robert W.
    Howarth,
  • Gene E. Likens, Pamela A. Matson, David W.
    Schindler,
  • William H. Schlesinger, and G. David Tilman

http//www.esa.org/science_resources/issues/FileEn
glish/issue1.pdf
2
Understanding element cycles as part of the major
functioning of ecosystems, requires following a
specific "approach".
  • 1st - Accounting Accounting tells you "where
    things are", or the distribution of the element
    in different pools within the ecosystem. 
  • 2nd - Cycling Cycling tells you "where things
    are going", and how fast they are moving from
    different pools in the ecosystem. 
  • 3rd - Controls Determining the controls tells
    you "how does the system function, and what
    factors drive the cycling". 

3
The nitrogen (N) cycle is a manifestation of
oxidation and reduction reactions - the loss and
gain of electrons. Oxidation and reduction
reactions are also the hallmark of the
biogeochemical cycling of carbon (C), hydrogen
(H), and oxygen (O) the chemical elements with
which the N cycle is most commonly and intimately
interconnected.
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5
The impacts of human domination of the nitrogen
cycle that we have identified with certainty
include
  • Increased global concentrations of nitrous
    oxide (N2O), a potent greenhouse gas, in the
    atmosphere as well as increased regional
    concentrations of other oxides of nitrogen
    (including nitric oxide, NO) that drive the
    formation of photochemical smog
  • Losses of soil nutrients such as calcium and
    potassium that are essential for long-term soil
    fertility
  • Substantial acidification of soils and of the
    waters of streams and lakes in several regions
  • Greatly increased transport of nitrogen by
    rivers into estuaries and coastal waters where it
    is a major pollutant.

6
Human alterations of the nitrogen cycle have
  • Accelerated losses of biological diversity,
    especially among plants adapted to low-nitrogen
    soils, and subsequently, the animals and microbes
    that depend on these plants
  • Caused changes in the plant and animal life and
    ecological processes of estuarine and nearshore
    ecosystems, and contributed to long-term declines
    in coastal marine fisheries.

7
http//bcs.whfreeman.com/thelifewire/content/chp58
/5802004.html
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9
Nitrogen once upon a time
10
Nitrogen Fixation
  • Global sources of biologically available (Fixed)
    nitrogen)
  • ANTHROPOGENIC SOURCES
  • ANNUAL RELEASE OF FIXED NITROGEN (teragrams)
  • Fertilizer 80
  • Legumes and other plants 40
  • Fossil fuels 20
  • Biomass burning 40
  • Wetland draining 10
  • Land clearing 20
  • Total from human sources 210
  • NATURAL SOURCES
  • Soil bacteria, algae, lightning, 140

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12
  • Nitrous Oxide is
  • a very effective heat-trapping gas in the
    atmosphere
  • unreactive and long lived in the lower atmosphere
  • in the stratosphere it can trigger reactions that
    deplete and thin the stratospheric ozone layer
  • increasing steadily, but source is still not
    completely identified

13
  • Nitric Oxide (80 from human activities)
  • highly reactive in the lower atmosphere and
    therefore much shorter lived.
  • catalyzing force in the formation of
    photochemical (or brown) smog.
  • In the presence of sunlight,nitric oxide and
    oxygen react with hydrocarbons emitted by
    automobile exhausts to form ozone, the most
    dangerous component of smog.
  • Ground-level ozone has serious detrimental
    effects on human health as well as the health and
    productivity of crops and forests.
  • Nitric oxide, along with other oxides of nitrogen
    and sulfur, can be transformed in the atmosphere
    into nitric acid and sulfuric acid, which are the
    major components of acid rain.

14
  • Ammonia (70 from human activity)
  • acts as the primary acid-neutralizing agent in
    the atmosphere, having an opposite influence on
    the acidity of aerosols, cloudwater, and
    rainfall.
  • May have important role in missing carbon or ??
  • Nitrogen saturation and
  • Soil acidification and release of nutrients
  • Marked reduction in overall species diversity as
    the few plant species adapted to take full
    advantage of high nitrogen out compete their
    neighbors.

15
Nitrogen in Aquatic Systems
  • Adding inorganic nitrogen to freshwater
    ecosystems that are also rich in phosphorus can
    eutrophy as well as acidify the waters.
  • Both eutrophication and acidification generally
    lead to decreased diversity of both plant and
    animal species.
  • When high nitrogen loading causes eutrophication
    in stratified waters where a sharp temperature
    gradient prevents mixing of warm surface waters
    with colder bottom waters the result can be
    anoxia (no oxygen) or hypoxia (low oxygen) in
    bottom waters.

16
Effects of Nitrates, Nitrogen and Ammonia
  • Methemoglobinemia
  • Acidification
  • Eutrophication ? anoxia in stratified waters
  • Toxic algal blooms

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20
Some facts
  • The process of manufacturing fertilizer by
    industrial nitrogen fixation was first developed
    in Germany during World War I.
  • Fertilizer production has grown exponentially
    since the 1940s.
  • The amount of industrially fixed nitrogen applied
    to crops during the decade from 1980 to 1990 more
    than equaled all industrial fertilizer applied
    previously in human history.

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22
More facts
  • The momentum of human population growth and
    increasing urbanization ensures that industrial
    fertilizer production will continue at high and
    likely accelerating rates for decades in order to
    meet the escalating demand for food.

23
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24
Crops
  • Soybeans, peas, alfalfa, and other leguminous
    crops and forages.
  • Non-leguminous, non-fixers rice
  • Huge demand for soybeans for animal feed

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28
The Future
  • In fact, global nitrogen deposition may as much
    as double in the next 25 years as agriculture and
    energy use continue to intensify

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30
What needs to be done
  • National and international policies should
    attempt to reduce these impacts through the
    development and widespread dissemination of more
    efficient fossil fuel combustion technologies and
    farm management practices that reduce the
    burgeoning demand for and release of nitrogenous
    fertilizers.

31
What you can focus on
  • Consumers can also contribute substantially to
    closing the open loop which currently allows
    nitrogen to be deposited on the land, washed into
    water courses and flushed out to sea.

32
Accounting for the N stocks, flows, and controls
in the food stream
33
Accounting for N Flows
34
Understanding element cycles as part of the major
functioning of ecosystems, requires following a
specific "approach".
  • 1st - Accounting Accounting tells you "where
    things are", or the distribution of the element
    in different pools within the ecosystem. 
  • 2nd - Cycling Cycling tells you "where things
    are going", and how fast they are moving from
    different pools in the ecosystem. 
  • 3rd - Controls Determining the controls tells
    you "how does the system function, and what
    factors drive the cycling". 
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