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Four Phases or states of Matter

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Four Phases or states of Matter Solid Liquid Gas Plasma Solids Constant volume Constant shape Atoms or molecules are well ordered into a crystal lattice for most ... – PowerPoint PPT presentation

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Title: Four Phases or states of Matter


1
Four Phases or states of Matter
  • Solid
  • Liquid
  • Gas
  • Plasma

2
Solids
  • Constant volume
  • Constant shape
  • Atoms or molecules are well ordered into a
    crystal lattice for most materials
  • Particles have VIBRATIONAL motion ONLY
  • Exceptions
  • Glass which is a very slow flowing liquid
  • Amorphous solids have no crystal structure

3
Liquids
  • Constant volume
  • Variable shape
  • Incompressible
  • Atoms or molecules loosely attracted to its
    neighbors, but in close proximity which allows
    fluid particles Translational (place to place)
    motion

4
Gases
  • Variable volume
  • Variable shape
  • VERY Compressible
  • Atoms or molecules are widely separated and have
    little interaction with each other aside from
    collisions resulting from their Translational
    motion

5
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6
Water is strange! Water expands as it forms a
solid. This causes the density of ice to be less
than liquid water and, therefore, ice floats in
liquid water. Note the structure of liquid
water (left) and ice (right). Notice the
greater space in the organized crystalline ice
structure which is the cause of the expansion.
Germanium also does this.
7
Plasma
  • Temperature is so high that negative electrons
    are separated from their positively charged
    atomic nuclei
  • No molecules exist
  • Particles are electrically charged
  • Found in Sun, stars, neon bulbs, lightning bolts
    and Fusion reactors.

8
Direction of Heat Transfer
  • Heat ALWAYS travels from a higher concentration
    of energy (high temperature) to a lower
    concentration of energy (low temperature).

9
Changing Phases or States
  • For elements, all four states are possible.
    Compounds can be only solids, liquids or gases
  • PHASE CHANGES occur when energy content changes
  • ENERGY PlasmagtGasgtLiquidgtSolid
  • Energy content is the cause of the differences
    between states or phases at the particle level

10
Molecular velocity determines TEMPERATURE and
STATE
  • Slow moving molecules
  • Fast moving molecules
  • Means cooler material
  • If cool enough, particle attractions overcome
    motion and they begin to stick together(freezing)
  • Means warmer material
  • If warm enough, particles have enough energy to
    leave the solid surface to liquid
    (melting) or the liquid surface to become
    gaseous (vaporizing)

11
6 Phase Changes
  • Freezing (liquid to solid)
  • Melting(solid to liquid)
  • Vaporization (evaporation or boiling)(liquid to
    gas)
  • Condensation(gas to liquid)
  • Sublimation(solid to gas- skip liquid)
  • Deposition(gas to solid- skip liquid)

12
Melting and Freezing
  • Changes between liquid and solid
  • Freezing is the opposite of melting
  • Melting - Attractions between solid particles
    break when energy is added and vibrations
    increase until they escape into liquid state
  • Freezing - Particles move slowly enough that
    attractions can pull particles together to form
    solid

13
Vaporizing
  • Liquid particles break the attractions of
    neighboring particles and travel up into the
    gaseous layer
  • Evaporation- only particles near the surface have
    enough energy (traveling fast enough) to break
    the attractions
  • Boiling particles throughout the liquid are
    traveling fast enough to form bubbles with higher
    pressure than outside conditions. Boiling Point

14
Evaporation occurs only from
the surface
15
Evaporation-surface particles only
  • Only particles near the surface have enough
    energy to become a gas
  • Liquid particles take energy from the liquid
    to enter gaseous state which cools the liquid
  • The gas layer can also cool because of the influx
    of slower moving gas particles

16
Boiling any particle in the sample has enough
energy to travel fast enough to exit the liquid
phase
17
Evaporation (are you sure?)
18
Condensation
19
Condensation
  • The opposite of evaporation
  • Interaction of high energy particles with a
    cooler surface to form liquid
  • Evaporation and Condensation occur usually on the
    SURFACE
  • Gas particles release heat to rejoin the liquid
    (Exothermic)

20
Sublimation
  • Particles going directly from solid state to
    gaseous state.
  • Dry Ice is a good example Dont touch, use
    gloves -78C - Sublimation point which is
    115colder than you
  • Extended contact Frost bite
  • Dry Ice NEVER melts
  • Solids that smell usually do so because of
    Sublimation Chocolate particles enter your
    nose

21
Deposition
  • Hot gaseous atoms forming a layer of solid on a
    cooler surface manmade Diamonds are gaseous
    Carbon on a seed crystal
  • Can be used to form a layer of thin expensive
    metal on cheap metal base

22
Energy and Phase Change
Adding heat at a constant rate
T
Boiling
Melting
Time
23
Viscosity is related to flow rate
  • Low Viscosity material can flow rapidly
  • Water and Alcohol have low viscosity
  • High Viscosity material flows slowly
  • Motor oil, lava, molasses, honey
  • all have high viscosity

24
Pressure
  •  

25
Boyles Law Pressure vs Volume Relationship
  • P1 x V1 P2 x V2
  • Original New
  • Decrease the volume of a gas causes a higher
    pressure.
  • Increase the Volume of a gas causes a lower
    pressure. Indirect Relationship

26
Boyles Law Sample Problem
  •  

27
Charles Law Volume vs Temperature
  •  

28
Charles Law Sample problem
  •  

29
Graphing Reasons and Rules
  • Purpose To find how variables relate
  • X-axis Independent variable (manipulated)
  • Y-axis Dependent variable (responding)
  • Slope rise/run rate of change
  • Use Predicting values that were previously
    unknown
  • Graphs MUST have TITLES
  • Graphs MUST have Labels
  • X-axis Independent
  • Y-axis Dependent

30
Graphing Outcomes
  • Directly proportional A is up B is up
  • Indirectly proportional A is up but B is
    down
  • Straight line graph varying at a constant rate
  • Curved line graph varying at a changing rate
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