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7/29/2019 Chemistry presentation1
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Carbon and Nitrogen
CyclePROUDLY PRESENT BY ,
MD ADIB FIKRIKAVISYA
LOGADHARSHINISUGANEYAALKHALWARIZMI
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Aim: To explore the carbon and nitrogencycles
Objectives
Describe how energy flows in an ecosystem
Illustrate the carbon and nitrogen cycles
Explain how human activity is affecting carbon
emissions
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INTRODUCTION
Additions of reactive nitrogen to terrestrialecosystems primarily through fertilizer application
and atmospheric deposition have more than doubled
since 1860 owing to human activities.
Nitrogen additions tend to increase the net uptake of
carbon by the terrestrial biosphere, but they also
stimulate nitrous oxide release from soils.
However, given that the magnitude of these effectsis uncertain, and that the carbon and nitrogen cycles
are tightly coupled, the net climatic impact of
anthropogenic nitrogen inputs is unknown
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Trophic Levels
Energy moves from one organisms to another
when it is eaten
Each step in this transfer of energy is known as
a trophic level
The main trophic levels are producers and consumers
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Food Chains
The energy flow from one trophic level to theother is know as a food chain
A simple food chain shows how energy istransferred from the sun through livingorganisms.
It involves one organism at each trophic level Producers (e.g. plants) Primary Consumers
Secondary Consumers
Tertiary Consumers
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Food Chain
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Food Web
Most animals eat more than JUST one organism
So in any ecosystem food chains connect toform a food web
Food webs are more complex and involve lots oforganisms
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Food web
TREES produce ACORNS which
act as food for many MICE andINSECTS.
Because there are many MICE,WEASELS and SNAKES havefood.
The insects and the acorns also
attract BIRDS, SKUNKS, andOPOSSUMS.
With the SKUNKS, OPPOSUMS,WEASELS and MICE around,HAWKS, FOXES, and OWLS canfind food.
They are all connected! Like aspiders web, if one part isremoved, it can affect the wholeweb.
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Ecological Pyramid
At each trophic level energy is used and
waste material produced
So there is less energy available for transfer
at each stage and a food pyramid is formed
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Carbon cycle
The circulation of carbon atoms in the
biosphere as a result of photosynthetic
conversion of carbon dioxide into complex
organic compounds by plants, which areconsumed by other organisms
The carbon returns to the atmosphere in
the form of carbon dioxide as a result ofrespiration, decay by fungi, bacteria, and
combustion of fossil fuels.
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AtmosphericCarbon Dioxide
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AtmosphericCarbon Dioxide
Plants use carbondioxide to make theirfood (photosynthesis)
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AtmosphericCarbon Dioxide
Plants use carbondioxide to make theirfood (photosynthesis)
Green plants areeaten byanimals
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AtmosphericCarbon Dioxide
Plants use carbondioxide to make theirfood (photosynthesis)
Green plants areeaten byanimals
respiration
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AtmosphericCarbon Dioxide
Plants use carbondioxide to make theirfood (photosynthesis)
green plants areeaten byanimals
respiration
dead remains of plants andanimals
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AtmosphericCarbon Dioxide
Plants use carbondioxide to make theirfood (photosynthesis
green plants areeaten byanimals
respiration
dead remains of plantsand animals
decayby fungiand bacteria
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Carbon in Oceans
Additional carbon is stored in the ocean.
Many animals pull carbon from water to use in
shells, etc.
Animals die and carbon substances are
deposited at the bottom of the ocean.
Oceans contain earths largest store of carbon.
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Human Impact
Fossil fuels release carbon stores very slowly
Burning anything releases more carbon intoatmosphere especially fossil fuels
Increased carbon dioxide in atmosphereincreases global warming
Fewer plants mean less CO2 removed fromatmosphere
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21
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Greenhouse Gases
The greenhouse effect is causing the
Earth to warm up.
This is causing climate change
and melting of the polar icecaps, this could lead toflooding.
It is due to increasing amounts ofgreenhouse gases, such as carbondioxide, water vapour andmethane.
Burning fuels is a majorcause of this increase.
Video
http://www.youtube.com/watch?v=dP-tg4atr5M&feature=relatedhttp://www.youtube.com/watch?v=dP-tg4atr5M&feature=related7/29/2019 Chemistry presentation1
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Nitrogen cycle
The nitrogen cycle is the process by which nitrogen is
converted between its various chemical forms. This
transformation can be carried out through both biological
and physical processes.
Important processes in the nitrogen cycle
include fixation, ammonification, nitrification,
and denitrification.
The majority of Earth's atmosphere (78%) is nitrogen,
making it the largest pool of nitrogen. However,atmospheric nitrogen has limited availability for biological
use, leading to a scarcity of usable nitrogen in many types
of ecosystems.
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( )
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Denitrifyingbacteria
Nitrates(NO3
)Detritivores
Ammonium (NH4+)
Amino acidsand proteins in
plants and animals
Detritus
Assimilationby plants
Nitrogen-fixingbacteria in soil
Nitrogenfixation
Decomposition
Nitrogen-fixingbacteria in root
nodules of legumes
Nitrogenfixation
Nitrogen (N2) in atmosphere
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There are 4 phases in the cycle:
Nitrogen fixation = NH3/NH4+
Decay = decomposing organic nitrogen into NH4+
Nitrification = converting NH4+ to NO2 to NO3
Denitrification = converting NO3 into N2
Micro-organisms play an important part in this cycle!
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Nitrogen Fixation
The enormous energy oflightning breaks nitrogen moleculesapart and enables the nitrogen atoms to combine withoxygen forming nitrogen oxides (N2O)
Nitrogen oxides dissolve in rain, forming nitrates (NO3)
Nitrates(NO3) are carried to the ground with the rain.
NN O
(NO3)
(N2O)
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Lightning fixes Nitrogen!
Nitrogen combineswith Oxygen
Nitrogen oxides forms
Nitrogen oxidesdissolve in rain andchange to nitrates
Plants use nitrates
to grow!
(NO3)
NN O
(N2O)
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Decay
Animals acquire their amino acids when they eat
plants.
When animals and plants die their remains areused as food by micro-organisms such as bacteria
and fungi.
Decomposers convert the nitrogen back intoammonia (NH3)
Ammonia (NH3) is
stored in soil.
Decomposers convert organic nitrogen toammonia (NH3) Ammonia (NH3) is used by some
plants
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Nitrifying bacteria in soil combineammonia with oxygen
Ammonia changes to nitrites
Nitrifying bacteria in soil convertnitrites to nitrates
Plants absorb nitrates and
grow!
Ammonia Nitrites Nitrates
(NH3) (NO3)(NO2)
Nitrification Living in the soil are nitrifying bacteria.
First, Nitrosomonas bacteria combine ammonia with oxygen toform nitrites.
Then another group of nitrifying bacteria, Nitrobacter, convertnitrites to nitrates which green plants can absorb and use!
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Figure 32.13
ATMOSPHERE
N2
N2 Nitrogen-fixingbacteria
Ammonifyingbacteria
Organicmaterial
NH4+
(ammonium) Nitrifyingbacteria
NO3
(nitrate)
Root
NH4+
Aminoacids
Soil
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Denitrification
Denitrification converts nitrates (NO3) in the soil to
atmospheric nitrogen (N2) which is returned to the air.
Denitrifying bacteria live deep in soil and in aquatic
sediments where conditions make it difficult for them to get
oxygen
Denitrifying bacteria live deepin soil and use nitrates as analternative to oxygen making abyproduct of nitrogen gas.
Nitrogen in atmospherecloses the nitrogen cycle!
(NO3) (N2)
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Acid Rain
Human activity havedoubled the amount offixed nitrogen entering thenitrogen cycle in just 100
years
Manufacture and use of
nitrogen fertilisers,combustion of fossilfuels and forest burning
Kills fish, damages trees andbuildings.
Video
Climate change, acidrain, the acidification of
soils and loss of soilnutrients, and theacidification of streamsand lakes.
http://www.youtube.com/watch?v=HE6Y0iEuXMQhttp://www.youtube.com/watch?v=HE6Y0iEuXMQ7/29/2019 Chemistry presentation1
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Effects of Nitrogen Overload
Effects on soil makes soil acidicdissolving toxic metals such as aluminium.
Effects on the atmosphere acid
precipitation killing many organisms
Effects on fresh-water ecosystems
eutrophication and algal bloom.
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Thank You !!!!