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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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