environment present
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TOPIC: ENVIRONMENT
PREPARED BY:
THUNISHAA D/O VEERAPPEN
EE LI ZAN
LOH MIN CEK
KHOR JOO HUAT
JASINTHA D/O JAYADURAI
PENDIDIKAN ALAM
SEKITAR
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Vision 2020
ensure that her invaluable resources are
not wasted. The land must remain
productive and fertile, the atmosphere clearand clean, the water unpolluted, the forest
resources capable of regeneration, able to
yield the needs of the national development.
The beauty of the land must not be
desecrated: for its own sake and for its
economic advancement
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WHAT IS ENVIRONMENT?
Environment has two components:
Biotic Abiotic
livings factors (the nonliving chemicalother organisms in and physical factors
an organisms
environment)
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environment
The natural environment, encompasses all living and non-livingthings occurring naturally on Earth or some region thereof.
Complete ecological units that function as natural systems
without massive human intervention, including all vegetation,microorganisms, soil, rocks, atmosphere and naturalphenomena that occur within their boundaries.
Universal natural resources and physical phenomena that lackclear-cut boundaries, such as air, water, and climate, as well asenergy, radiation, electric charge, and magnetism, notoriginating from human activity.
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What is ECOLOGY?
Scientific study of the interactions between
organisms and their environment
enormously complex because interactions
between organisms and their environment are
two-way: organisms affected by environment, but their activities also can
change the environment
e.g. photosynthesis by plants, nutrient cycles by animals
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Four increasingly comprehensive levels of study
ORGANISM
POPULATION
COMMUNITY
ECOSYSTEM
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organisms
Any form of living things
Deals with behavioral, physiological andmorphological ways in which organisms adapt
to their environment.
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population
A group of interacting individuals belonging to
the same species inhabiting a particular
geographical area at the same time.
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community
All organisms inhabiting a particular area
biological community. It is a complex interacting network of plants, animal and
microorganisms
studies involve ways in which predation, competition,
and other interactions among organisms affect
community structure and composition.
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Interactions
between species
Interspecific Intraspecific
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Interspecific interaction
Positive Neutral Negative
Commensalism Competence Predation
Mutualism Parasitism
Ascaris suum
Symbiosis
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ecosystem
includes all abiotic factors in addition to the
community of species that exist in a certain
area
i.e. energy flow, nutrient cycling, etc...
Ecosystem ecology looks at energy
transformations and biogeochemical cycling
within ecosystems.
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ECOSYSYTEM
BIOTIC
BIOGEOCHEMICAL
CYCLES
ABIOTIC
WATERFLORA FAUNA AIR
FOOD WEB
INTERACTION
LAND
TERRESTRIAL
ESOSYSTEMAQUATIC ECOSYSTEM
ECOSYSTEMS HAVE
ENERGY FLOWS
ECOSYSTEMS CYCLE
MATERIALS
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Biotic components
Primary Producers
Herbivores
Omnivores Carnivores
Detritivores
etc
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Abiotic components
Sunlight
Temperature
Precipitation Water or Moisture
Soil or Water Chemistry
etc
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Food chains
SNAKECHICKENGRASS WORM
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Food Webs
SNAKE
BIRD
CHICKENGRASS WORM
HORSE
LION
DOG
CAT
TIGER
GRASSHOPPER
TERRESTRIALECOSYSTEM
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SEA OTTERSEA URCHIN
ALGAE
SMALL FISH
BIG FISH
SHARK
RAY
MOLLUSCA
STAR FISH
HARLEQUIN
SHRIMP
TURTLE
Food WebsAQUATIC
ECOSYSTEM
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Food chain and food web always begin withproducers (plants).
Energy enters the biological system as lightenergy, or photons, is transformed into chemicalenergy in organic molecules by cellular processes
including photosynthesis and respiration, andultimately is converted to heat energy.
This energy is lost to the system as heat at eachtrophic level as heat when consumers burn foodduring cellular respiration.
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Elements such as carbon, nitrogen, or phosphorusenter living organisms in a variety of ways.
Plants obtain elements from the surrounding
atmosphere, water or soils. Animals may also obtain elements directly from the
physical environment, but usually they obtain thesemainly as a consequence of consuming other
organisms.
These materials are transformed biochemically withinthe bodies of organisms, but sooner or later, due toexcretion or decomposition (process by bacteria),
they are returned to an inorganic state.
The elements are cycle endlessly between their bioticand abiotic states within ecosystems (BiogeochemicalCycles).
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photosysnthesis
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Biogeochemical Cycles
Biogeochemical cycles describe the ecosystem
by the transfer of elements through the system.
By examining the cycles we can look at the
fluxes of nutrients (sources and sinks) and
better understand human-caused imbalances.
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The Hydrologic Cycle
Over 71% of the earths surface is covered by
water:
Oceans contain 97%.
Polar ice caps and glaciers contain 2%.
Freshwater in lakes, streams, and ground water
make up less than 1%.
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The Hydrologic Cycle
Distribution of water is not static:
Heat
Evaporation
CloudsPrecipitation
Evaporation
Consumed by organisms
Groundwater
Surface water
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Hydrologic cycle
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The Hydrologic Cycle
Turnover time is the time required for the
entire volume of a reservoir to be renewed.
Atmosphere 9 days
Rivers 12-20 days
Oceans 3,100 years
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Phosphorus Cycle
Global phosphorus cycle does not include
substantial atmospheric pool.
Largest quantities found in mineral deposits and
marine sediments.
Much of this in forms not directly available to plants.
Slowly released in terrestrial and aquatic
ecosystems via weathering of rocks.
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Phosphorus cycle
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Importance of P
transformations
It has been suggested that the level of available phosphorusduring soil development is the primary determinant interrestrial net primary production:
P is present in low concentrations in rocks.
N is abundant in the atmosphere.
Other essential plant nutrients (e.g., S, K, Ca, Mg) are moreabundant than P.
Bacteria that fix N2 gas to biologically available N requireP.
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Nitrogen Cycle
Includes major atmospheric pool - N2.
Only nitrogen fixers can use atmospheric supplydirectly.
Energy-demanding process. N2 reduced to ammonia (NH3).
Once N is fixed it is available to organisms. Upon death of an organism, N can be released by fungi and
bacteria during decomposition.
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Nitrogen cycle
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N2 NH3
Animals
NH4
SOM
N2O
NO2
Plants
NOx HNO3
N2
NO3
N2O
NH3
Atmosphere
Terrestrial
Aquatic(same species &
reaction asterrestrial)
NOx
N stocks can be defined by:
Physical location Atmosphere, Land, Ocean
Chemistry
Reactive vs. Nonreactive
Organic vs. Inorganic
Ecological effects
Fertilizer, greenhouse, acid rain,
smog
Source Biological, Anthropogenic,
Geochemical
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Important N species
Non-reactive (99%) N2, N in recalcitrant minerals
Reactive
Ammonia (NH3)
Ammonium (NH4
+)
Nitrate (NO3-)
Nitrogen oxides (NO, NO2-, NO3
-)
Nitric acid (HNO3)
Nitrous oxide (N2O)
Organic N (urea, proteins, nucleicacid, SOM, PON, DON)
N2 NH3
Animals
NH4
SOM
N2O
NO2
Plants
NOx HNO3
N2
NO3
N2O
NH3
Atmosphere
Terrestrial
Aquatic(same species &
reactionasterrestrial)
NOx
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Important N reactions
Biological
1. Nitrogen fixation
2. Assimilation
3. Mineralization
4. Nitrification
5. Denitrification
Abiotic in atmosphere
Fixation by lightening
N2O reactions
NOx reactions
Anthropogenic
Fixation by Haber-Bosch
Fixation by fossil fuels
Burning organic matter
N2 NH3
Animals
NH4
SOM
N2O
NO2
Plants
NOx HNO3
N2
NO3
N2O
NH3
Atmosphere
Terrestrial
Aquatic(same species &
reactionasterrestrial)
NOx
2
3
5
44
1 1
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Biological reactions: Fixation
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Who:Rhyzobiumbacteria,Azobacterbacteria,
cyanobacteria
What:
2N2 + 3H2 + energy 2NH3, NH3 + H2O NH4
+ + OH-
Where:symbiotically in plants
and free living, low O2
Why:essential bioelement But expensive 8-12 g of
glucose per 1 g N fixed!Animals
NH4
SOM
NO2
Plants
N2
NO3
N2O
NH3
Biological reactions: Fixation
(BNF)
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Animals
NH4
SOM
NO2
Plants
N2
NO3
N2O
NH3
Biological: Assimilation
Who: Plants and certain bacteria
What:
NH3 or NO3 + Organic matter Organic N
Where: aerobic & anaerobic environments
Why: essential bioelement
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Biological: Mineralization
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Who: Aerobic & anaerobic organisms of all kinds What:
Organic-N NH3
Where: aerobic & anaerobic environments Why: byproduct of organic matter degradation
Animals
NH4
SOM
NO2
Plants
N2
NO3
N2O
NH3
Biological: Mineralization(ammonification)
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Who: chemoautotrophic bacteria
What: NH4
+ + 3O2 2NO2- + 2H2O + 4H
+ + energy (Nitrosomonas)
2NO2- + O2 2NO3
-+ energy (Nitrobacter)
Where: aerobic environments (surface layer of sediments)
Why: ammonium is used as a source of energy N is oxidized (N3- N3+ N5+ ) O is reduced
Animals
NH4
SOM
NO2
Plants
N2
NO3
N2O
NH3
Biological: Nitrification
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Who: Pseudomonas denitrificans
What: C6H12O6 + 4NO3 6CO2 + H2O + 2N2 + energy
(N2O = intermediate and byproduct)
Where: anaerobic environments
Why: NO3- = best available e- acceptor Nitrogen is reduced (N5+N0 )
Animals
NH4
SOM
NO2
Plants
N2
NO3
N2O
NH3
Biological: Denitrification
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Atmospheric: Fixation by
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What: N2 + 3O2 + energy 2NO3
Where: atmosphere
Animals
NH4
SOM
NO2
Plants
N2
NO3
N2O
NH3
NOx
Atmospheric: Fixation by
lightning
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A h i N fi i
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Who: Bacteria in crop plants
What:
2N2 + 3H2 + energy 2NH3
Why:green fertilizer
Soybeans
Rhizobiumnodules in pea
roots
Rice
Anthropogenic: N-fixing crops
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Anthropogenic: Haber Bosch
http://www.postech.ac.kr/life/pfg/rice1.jpghttp://www.postech.ac.kr/life/pfg/rice1.jpghttp://www.ecol.kvl.dk/~sto/gf/images/rhizobium%20pea.jpg -
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Who: Human beings
What: N2 + 3H2 2NH3
Where: Industry
Why: Fertilizers and munitions
Animals
NH4
SOM
NO2
Plants
N2
NO3
N2O
NH3
Anthropogenic: Haber-Bosch
fixation
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A th i R l th b ti
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Who: Human beings What: Burning and respiration
Organic-N in fossil fuels, plants, SOM NH4, NOx
Where: Automobiles, industry, forests, agri. lands, drained
wetlands
Why: Byproduct (acid rains)
Anthropogenic: Release thru combustion
and respiration
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Anthropogenic: Fixation thru
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Who: Human beings
What: Abiotic fixation N2 + O2 + energy 2NO
2NO + O2 2NO2 NO2 + H2O HNO3
Where: Automobiles, industry, forests Why: Byproduct (acid rains)
Anthropogenic: Fixation thru
combustion
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At h i Abi ti ti
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NOx Acid formation
SOx + H2O H2SO4
NOx + H2O HNO3 Tropospheric ozone formation
NOx + O2 + hydrocarbons + sunlight O3
NH3
NH3(g) + H2O NH4+ + OH- N2O
Greenhouse gas
Stratosphere destroys ozone
Atmospheric: Abiotic reactions
Emissions of N and S oxides in U.S.
EmissionsinU.S
.(milliontons)
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Carbon Cycle
Moves between organisms and atmosphere as
a consequence of photosynthesis and
respiration.
In aquatic ecosystems, CO2 must first dissolve into
water before being used by primary producers.
Although some C cycles rapidly, some remains
sequestered in unavailable forms for long periodsof time.
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Carbon cycle
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Carbon cycle
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R l f C b C l t
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Relevance of Carbon Cycle toClimate Change
CO2 in atmosphere is increasing 0.4% a year (=40% in 100 yr.)
Increasing CO2 causes increased temperatures.
(Greenhouse effect)
Heat captured by the atmosphere:
1. CO2 = 50%
2. CH4 = 20%
3. CFCs = 15%
4. NO2, H2O, O3 = 15%
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Interaction between biotic
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Interaction between biotic
AND ABIOTIC
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THANK YOU
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