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The NonLiving Environment

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Title: The NonLiving Environment


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Chapter 13
  • The Non-Living Environment

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Environmental Factors
  • Biotic Factors
  • Features of the environment that are alive or
    were once alive
  • Biotic means living
  • Abiotic Factors
  • Nonliving physical features of the environment
  • Abiotic factors include air, water, soil,
    sunlight, temperature, and climate
  • These factors determine which kinds of living
    organism can live there

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Abiotic Factors
  • Air
  • Invisible and plentiful
  • Called the atmosphere
  • Contains 78 nitrogen, 21 Oxygen, .94 argon,
    .03 Carbon Dioxide and trace amounts of other
    gases
  • Plants use CO2 along with H2O and Sunlight in
    Photosynthesis to make sugar
  • Give off Oxygen into the atmosphere

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  • All organisms carry out respiration in their
    cells to obtain energy needed for life
  • Respiration is a process to release energy stored
    in the food that we eat
  • In respiration cells take in Oxygen from the
    atmosphere and release Carbon Dioxide

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  • Water
  • Essential for life on earth
  • Major ingredient of the fluid inside the cells of
    all organism
  • Most organisms are composed of 50-95 water
  • Many life function need water to take place, for
    example, Respiration, digestion, and
    photosynthesis

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  • Soil
  • Mixture of minerals and rock particles, the
    remains of dead organisms, water, and air.
  • Topmost portion of the earths crust
  • Supports plant growth
  • Formed from the breaking up of rocks into tiny
    particles
  • Contains many living organisms and the decaying
    remains of dead organisms

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  • Life includes bacteria, fungi, insects and worms
  • Soil contains different combination of sand clay
    and humus (decaying matter)
  • Type of soil presents has an important role of
    what type and how much plant life is found

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  • Sunlight
  • Sunlight is the energy for all life
  • During photosynthesis, producers convert light
    energy into chemical energy
  • Energy from the sun is passed on to consumers
    when they eat producers

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  • Temperature
  • Sunlight supplies heat energy as well as light
    energy
  • Most organisms can only survive if their body
    temperature stays within the range of 0 ans 50
    C
  • Some organism have adapted to live in climates
    below and above these temp.
  • Pengiuns, and Camels

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  • Temperature depends on how much direct sunlight
    an area gets
  • Areas located at latitudes farther from the
    equator tend to have colder temperatures
  • Receive less of the suns energy than equatorial
    areas
  • Equator gets direct sunlight
  • At poles sunlight strikes earth at angles and
    energy is spread out over a larger area

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  • Elevation (distance above sea level) affects
    temperature
  • Higher elevations the atmosphere is thinner,
    meaning fewer air molecules to be heated by the
    sun
  • Therefore, temperature will be cooler
  • At higher elevation, trees are shorter and the
    ground is rocky
  • Above timberline (the elevation beyond which
    trees do not grow) plant life is limited to
    low-growing plants
  • Some mountain tops are covered with snow all year
    around

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  • Climate
  • Refers to an areas average weather conditions
    over time, including temperature, rainfall or
    other precipitation, and wind
  • Temperature and precipitation are the most
    important components for living things
  • Amount of precipitation and average temperature
    influence the type of life in the area

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  • Wind
  • As temperature increase the molecules in the air
    spread farther apart, making warm air lighter
    then cold air
  • Cold air sinks below warm air and pushes it
    upward
  • These motions create air currents that are called
    wind

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  • The rain Shadow Effect
  • Presence of mountains can affect rainfall
    patterns
  • As air masses move over a mountain range it cools
  • As air cools the moisture at carries falls as
    rain or snow
  • By the time the air mass crosses over the
    mountain it has lost all its moisture
  • This results in the other side of the mountain
    getting very little or no precipitation

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Cycles in Nature
  • Water Cycle
  • Evaporation- takes place when liquid water
    changes into water vapor (gas) and enters the
    atmosphere
  • Water evaporates from lakes, streams, puddles and
    oceans
  • Water vapor enters the atmosphere from plants
    through a process of transpiration
  • Animals release water vapor when they exhale

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  • Condensation
  • Water vapor in the atmosphere eventually comes
    into contact with cold air
  • Water vapor cools and changes back into liquid
    form (condensation)
  • Water vapor condenses on particles of dust in
    the air, forming tiny droplets
  • Clump together to form clouds
  • Once they become to heavy they fall as
    precipitation

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Water Uses
  • Homes and Business 39,100 million gallons/day
  • Industry and Mining 27,800 million gallons/day
  • Farms and Ranches- 141,000 million gallons/day
  • Electricity Production- 131,800 Million
    Gallons/day

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Nitrogen Cycle
  • Nitrogen is the main ingredient of proteins
  • Proteins are required for life processes
  • Nitrogen is the most plentiful gas in our
    atmosphere but most organism cannot use
    atmospheric nitrogen
  • Plants need nitrogen that is been combined with
    other elements

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  • Through a process called Nitrogen Fixation, some
    bacteria in the soil can form the nitrogen
    compounds that plants need
  • Plants absorb nitrogen through roots
  • Animals get nitrogen from eating plants and other
    animals
  • When dead organism die they return the nitrogen
    back into the soil or atmosphere

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  • Human activities can affect the nitrogen cycle
  • Growing corn and wheat remove much of the
    nitrogen out of the soil without replacing it
  • Farms add fertilizer to the fields to replace the
    nitrogen taken out
  • Compost and animal manure also contain nitrogen
    compounds

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  • Another method Farmers use is called Crop
    Rotation
  • Farmers grow Nitrogen fixing Crops
  • Nitrogen fixing bacteria live on or in the roots
    of these plants
  • Farmers will grow corn, wheat or potatoes in a
    field for only one-two years and then grow a
    Nitrogen fixing plants for one-two years

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1. Legume symbioses The most familiar examples of
nitrogen-fixing symbioses are the root nodules of
legumes (peas, beans, clover, etc.).
                                                  
                                                  
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rt of a clover root system bearing naturally
occurring nodules of Rhizobium. Each nodule is
about 2-3 mm long.                              
                                                  
                                                  
                
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Carbon Cycle
  • Carbon is important part of soil Humus, and is
    found in the atmosphere as CO2
  • Carbon cycle begins when producers remove CO2 to
    carry out photosynthesis
  • CO2 is released by organism in the process of
    respiration
  • Human activities also release CO2 into the
    environment Burning Fossil Fuels

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  • The Amount of CO2 in the Atmosphere is increasing
    from Tree harvesting, and burning fossil fuels
  • Extra CO2 could trap heat and cause average
    temperatures to increase
  • Global Warming
  • Temperatures are increasing at a rate of about 2
    every 10 years

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Energy Flow
  • Converting Energy
  • Photosynthesis Converting solar energy into
    chemical energy (Glucose)
  • Respiration-Converting stored chemical energy
    into Kinetic energy (energy to do work)
  • Chemosynthesis- Organism that use chemicals to
    produce energy rich molecules
  • Bacteria living near hydrothermal Vents deep in
    the ocean where there is no light

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  • Water near hydrothermal vents are very hot
    because of contact with molten rock
  • Waters are rich in chemicals such as sulfur
  • Consumers living in the vent rely on
    chemosynthetic bacteria for nutrients and energy

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  • Energy Transfer
  • Energy can be transferred from one organism to
    another
  • Throughout nature energy and matter is
    transferred from one organism to another
  • Food Chains
  • Shows how matter an energy passes from one
    organism to another
  • Producers are the first step of the food chain

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  • Herbivores or Omnivores are the second step
  • Carnivores or omnivores are the third and higher
    steps

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  • Food Webs
  • Food webs are made up of many different food
    chains
  • Shows the feeding relationship between all
    organism in the community

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  • Energy Pyramids
  • The amount of energy available is reduced as you
    move from one level to the next
  • For example When a plant absorbs sunlight, it
    uses some of the energy to grow, therefore when
    the plant gets eaten not all the energy is passed
    on
  • Animals use energy they obtained to carry out
    life functions, so when they get eaten less
    energy is passed on

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  • The same thing happens at every feeding level of
    a food chain
  • An energy pyramid shows the amount of energy
    available at each level
  • Bottom level is the largest, contains all the
    producers and contains the most energy
  • Only about 10 of the energy available at each
    level of an energy pyramid is transferred to the
    next highest level

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  • Thus 10 percent of the energy in plants becomes
    stored in the tissues of herbivores, and 10
    percent of the energy in herbivores becomes
    stored in the tissues of carnivores

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