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Title: OGT Review


1
OGT Review
2
Elements
  • Elements are the basic building blocks of matter.
  • There are 115 known elements.
  • This number changes as new elements are created
    in research labs.
  • 90 elements occur in nature and fewer than half
    of them are common.

3
Elements Continued
  • Elements are listed on the Periodic Table of
    Elements by atomic number (number of protons).
  • Elements are composed of atoms.

4
Atoms
  • Atoms are the smallest particle of an element
    that has the properties of that element.
  • John Dalton (1803)- Modern atomic theory.
  • All atoms of a particular element are alike, but
    they are different from the atoms of any other
    element.

5
Atoms Continued
  • Atoms are made up of protons, neutrons and
    electrons (subatomic particles).
  • Protons have a positive charge ()
  • Electrons have a negative charge (-)
  • Neutrons have no charge

6
Atoms Continued
  • Protons and neutrons make up the nucleus of an
    atom.
  • Electrons orbit (circle) the nucleus.
  • Move around the nucleus in shells or energy
    levels.
  • The further away from the nucleus a shell is, the
    more electrons it can hold and therefore it has a
    higher energy level.
  • The inner most level can hold 2 electrons, the
    second can hold 8, the third up to 18 and so on.
  • The outer most shell (valence) can hold no more
    than 8 electrons.

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The Periodic Table
  • Elements are arranged by atomic number (number of
    protons in the nucleus).
  • Vertical columns are called groups or families.
  • Horizontal rows are called periods.
  • Elements located in the same group have similar
    electron configurations (same number of valence
    electrons). Therefore they will react in similar
    ways.

9
Changes in Matter
  • Scientists know of millions of different
    substances in the world.
  • How is this possible if there are only 115 known
    elements?
  • Elements combine to form different substances.

10
Chemical Bonds
  • Atoms are held together in molecules by chemical
    bonds.
  • Chemical bonds store energy.

11
Ionic Bonds
  • Ions are formed when an atom gains or loses an
    electron to become or -.
  • Sodium (Na) can lose its valence electron to form
    a sodium ion (Na).
  • Chlorine (Cl) can gain an electron to form a
    chlorine ion (Cl-).
  • An ionic bond is formed when two ions of opposite
    charges (metal and nonmetal) are attracted to
    each other and form a new substance.
  • NaCl Sodium Chloride (table salt).

12
Covalent Bonds
  • Covalent bonds are formed between atoms of two
    nonmetals.
  • Electrons are shared.
  • Example Carbon can share electrons with 2
    oxygen atoms (1 with each) to form carbon dioxide
    (CO2).
  • Covalent bonds are stronger than ionic bonds
    because of this sharing of electrons.

13
pH
  • The pH scale refers to strength of an acid or a
    base.
  • The scale ranges from 0-14.
  • 0 is the most acidic. (hydrochloric acid)
  • 14 is the most basic. (sodium hydroxide)
  • 7 is neutral. (water)

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15
Chemical Equations Continued
  • Chemical equations must be balanced. This means
    that each element appears the same number of
    times in both the reactants and products.
  • Example
  • C O2 ? CO2

16
  • If there are different amounts of each element on
    either side of an equation we must balance it
    using coefficients.
  • Example
  • H2 O2 ? H2O
  • This is not balanced. To balance we add
    coefficients.
  • 2 H2 O2 ? 2 H2O

17
States of Energy
  • Potential Energy (PE) Stored energy
  • Gasoline (chemical)
  • Rock on a cliff (position)
  • Food (chemical)
  • Coal (chemical)

18
  • Kinetic Energy (KE) energy an object has when
    it is moving.
  • Falling rock
  • Thrown ball
  • Runner
  • Waterfall

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20
End of Physical Science Review
21
Conduction
  • Conduction is the transfer of heat by direct
    molecular contact.
  • Metals are good conductors of heat.
  • Example If you hold a metal rod in fire the
    heat will quickly distribute between the
    molecules in the rod and it will become hot.

22
Convection
  • Convection is the transfer of heat by the flow of
    a liquid or a gas.
  • Warm air in a room rises and cool air sinks.
    This causes a circular motion called a convection
    current.

23
Radiation
  • Radiation is the transfer of heat through space
    in the form of waves.
  • Heat from the sun travels through the vacuum of
    space to reach Earth.

24
Wave Diagram
25
What is Force?
  • A force is a push or pull that is exerted on an
    object.
  • Force stops motion gloved hand catching a ball
  • Force slows motion friction slowing a
    skateboard
  • Force changes direction tennis racket striking
    a tennis ball

26
Gravity
  • Law of Universal Gravitation states that in the
    universe every mass attracts every other mass.
  • Greater mass greater gravitational force
  • An apple falls to Earth because the Earth is much
    more massive.

27
Friction
  • Friction is a force that resists motion.
  • It must be overcome to start an object moving
    and/or to keep it moving.
  • Rougher surfaceHeavy object More friction
  • Smooth surfaceLight object Less friction

28
Speed and Velocity
  • Speed and velocity are terms used to describe the
    motion of an object.
  • Speed is the distance traveled over a certain
    period of time.
  • Velocity is the same but includes a specific
    direction (north, east, southwest, etc.)

29
  • The equation used to determine both speed and
    velocity is distance divided by time.
  • S d/t V d/t
  • Units for measuring speed/velocity
  • Kilometers/hour (km/hr)
  • Miles/hour (mi/hr)
  • Feet/second (ft/s)
  • Meters/minute (m/min)
  • Centimeters/second (cm/s)

30
Acceleration
  • Acceleration is the rate in change in velocity.
  • Can be used to describe increased or decreased
    (deceleration) change.
  • Acceleration is calculated by subtracting an
    objects starting velocity from its final
    velocity and dividing by time.
  • A vf vs / t

31
Motion of falling objects
  • Gravity causes objects released above Earths
    surface to fall to the ground.
  • Mass, size and shape of the object determines how
    fast it will fall.
  • Air resistance (air drag) also affects falling
    objects.
  • In a vacuum (no air) all objects will fall at the
    same rate because gravity is the only force
    acting on them.

32
Spheres
  • The Earth consists of 3 spheres
  • The lithosphere (rock sphere)
  • The hydrosphere (water sphere)
  • The atmosphere (gas sphere)
  • These are smaller parts of the Biosphere The
    place where all life exists on Earth.

33
Interaction of Air, Land, and Water
  • Weathering is the breaking down of rocks into
    smaller pieces.
  • Physical weathering water seeps into cracks in
    rock and freezes, the water expands, breaking the
    rock apart.
  • Chemical weathering oxygen and water chemically
    react with iron mineral in rocks, turning to
    rust, which crumbles away easily.

34
Erosion
  • Erosion is the process by which rock material at
    Earths surface is removed and carried away.
  • Erosion requires a moving force (like water).
  • Example Streams and rivers turn a muddy brown
    after a heavy rain due to the rock material in
    the water.
  • Glaciers and wind can also contribute to erosion.

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36
Structure of the Earth
  • The Earth is composed of 3 layers.
  • The crust outermost layer (5-50 km)
  • The mantle middle layer (2900 km)
  • The core innermost layer
  • Outer core (2300 km)
  • Inner core (1200 km) Thought to be solid

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38
Theory of Continental Drift
  • 1912 Alfred Wegener proposed the continents
    were drifting across Earths surface.
  • Based on how the shapes of the continents fit
    together like a puzzle.
  • The original super continent was called Pangea.

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40
Plate Tectonics
  • Earths crust is broken into pieces, or plates,
    that slowly move and interact at their boundaries
    in various ways.
  • Caused by heat circulating in the mantle.
  • There are 10 major plates The Pacific, North
    American, Nazca, Cocos, South American, African,
    Arabian, Eurasian, Indian, and Antarctic.

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Plate Interactions
  • As the plates move, some are colliding, some are
    spreading apart, and some are sliding past one
    another.
  • Subduction zone When an oceanic plate collides
    with a continental plate it tends to slide down
    under it. This forms mountains and volcanoes.
  • Fault zones When one plate slides sideways past
    another. This sometimes causes severe
    earthquakes.

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44
Now Do the OGT Review Questions 2
45
Earths Geologic History
  • Scientists have pieced together much of Earths
    history by studying rocks.
  • There are 3 main rock types
  • Sedimentary
  • Igneous
  • Metamorphic

46
Sedimentary Rock
  • Most commonly formed by the deposition of
    particles underwater. (dirt being submerged)
  • About 75 of land surface is covered with
    sedimentary rocks.

47
Igneous Rock
  • Form from hot molten rock material, either
    underground (magma) or on Earths surface (lava)
  • Volcanoes

48
Metamorphic Rock
  • Form from pre-existing rocks that undergo changes
    caused by extreme heat and/or pressure.
  • Plate motions

49
Distances in Space
  • Distances in space are so great they are
    difficult to comprehend.
  • The distance between Earth and the nearest star
    (besides the sun) is 41,000,000,000,000 km. (41
    trillion)
  • We use light-years to express distances in space.
  • A light-year is the distance light travels in a
    year.

50
The Big Bang Theory
  • According to this theory, all the matter and
    energy that exists in the universe today was once
    concentrated in a very small, dense object about
    the size of an atom.
  • For some unknown reason this object suddenly
    expanded creating the beginning of space and
    time.
  • Matter continued to move away and over time small
    amounts combined to form stars and planets.

51
Evidence
  • The universe is expanding outward (Red Shift).
  • Galaxies are slowly moving apart.
  • Galaxies are determined to be about 15 billion
    years old.
  • Large quantities of a hydrogen isotope are
    scattered throughout the universe (remnants of
    big bang).

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53
The Solar System
  • Scientists believe that our solar system formed
    about 5 billion years ago.
  • After the Big Bang some gases and dust became
    our star (sun).
  • The leftover material condensed into planets,
    satellites, comets, meteoroids and asteroids.
  • The sun contains 99 of all matter in our solar
    system.

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55
Types of Symbiosis
  • Mutualism When both organisms benefit.
    (butterfly/flower)
  • Commensalism When one organism benefits and the
    other is not affected. (remora/shark)
  • Parasitism When one organism benefits and the
    other is harmed. (tapeworm/animal)

56
Mutualism
57
Commensalism
58
Parasitism
59
Overpopulation
  • Overpopulation, competition, and changes in the
    environment challenge the survival of all
    individuals within a population (same species).
  • More individuals than the environment can
    support.
  • Competition for resources food, territory,
    shelter and mates.
  • Most do not survive to reproduce.

60
Variations
  • Due to variations (differences) among members of
    a species, some individuals are better adapted.
  • These organisms survive to reproduce while others
    die out.
  • Natural Selection Survival of the Fittest,
    Only the Strong Survive etc. Darwins Theory

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62
NATURAL SELECTION
63
A major misconception about natural selection!
http//evolution.berkeley.edu/evosite/misconceps/I
Eneeds.shtml
64
Evolution the basics
  • 1. over population
  • 2. constant struggle for resources
  • 3. variation in the species
  • 4. the best adapted to the environment survive
  • 5. surviving organisms transmit variation to
    offspring

65
Random facts
  • ATP cellular energy
  • CO2 taken in and O2 given off photosynthesis
  • Flagella moves a cell
  • Mitochondria makes cellular energy
  • Placebo fake drug
  • Ethics
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