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Structure and Properties of Water

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Title: Structure and Properties of Water


1
Structure and Properties of Water
  • Molecular Structure
  • Physical Characteristics
  • Implications for Life on Earth
  • www.sbu.ac.uk/water/anmlies.html

2
Why do we care?
  • Molecular structure and physical characteristics
    determine important properties
  • Physical characteristics serve as a foundation
    for measurement systems
  • Physical characteristics support life on the
    planet

3
Bipolar molecule
  • H2O in purest form
  • Two hydrogen atoms and one oxygen atom
  • Bipolar structure due to orientation of hydrogen
    and oxygen atoms held in covalent bond

4
Significance of bipolar structure
  • Covalent bonds result when electrons are shared
    by atoms
  • Oxygen is larger than hydrogen so sharing is
    unequal
  • The result is an asymmetric distribution of
    charge, leading to a positive and negative end of
    the molecule

5
Solubility of Chemical Compounds
  • Efficient solvent
  • Two mechanisms ionic and hydrogen bonding
  • Ionic bonding charged ions of a compound are
    isolated by oppositely charged poles of water
    molecules and separated (the compound
    dissociates)
  • Hydrogen bonding compounds are partially
    dissociated and held in solution

6
Water as solvent
  • Solvent a substance that dissolves other
    substances, thus forming a solution. Substances
    may mix thoroughly so that solute cannot be seen,
    or the solution is visibly changed
  • Almost all chemical substances have been found in
    solution in water
  • Transfers gases to earth surface
  • Dissolved nutrient transfers sustain life

7
Attraction between ions and partial charges of
poles
8
Hydrogen bonding
  • Charge-based bonds
  • Weaker than covalent bonds and temporary
  • Strong enough to develop forces that determine
    many physical properties

9
Hydrogen bonding
  • Results in surface tension
  • Determines density and molecular structure of
    water and ice
  • Determines wetting ability and solubility of
    surfaces and compounds

10
Surface tension
  • The cohesive force of water or the work that
    needs to be done to pull it apart
  • Affects
  • Groundwater flow
  • Infiltration into soils
  • Ability of water surface to support an object
  • Examples
  • water rise in a capillary tube
  • needle floating on water
  • the Jesus lizard

11
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12
Density and molecular structure of water
  • Density Mass per unit volume
  • Typically used density of water 1 g/cm3
  • Actual range of densities of liquid 1 - .987
    g/cm3 (at 4º and 100º C)

13
Density and Molecular Structure
  • As many liquids cool, they decrease in volume
    (alcohol)
  • Hydrogen bonds are temporary, and the overall
    number of bonds formed is dependent upon
    molecular motion
  • Molecular motion decreases as temperature
    decreases

14
Density and Molecular Structure
  • Increased rigidity and alignment lead to slight
    expansion below 4ºC
  • Implications
  • Ice is less dense than liquid water and floats
  • Water bodies freeze from the surface down, rather
    than the bottom up

15
Why is this important?
  • Very few life forms can withstand freezing and
    thawing cycles
  • Many can withstand cold conditions
  • Ice remains on the surface of water bodies
  • Life on the bottom is preserved
  • Lakes turn over
  • Allows for aquatic life in the higher latitude
    regions

16
Trends in boiling points in similar compounds
17
Wetting Hydrophobic and hydrophilic surfaces
  • Hydrogen bonding can occur between molecules of
    chemically diverse substances
  • Tendency for water to coat or bead on a surface
    is related to hydrogen bonding that takes place
    on the surface
  • Hydrophilic surfaces allow coating because they
    have oxygen with unpaired electrons
  • Surface tension forces, caused by hydrogen
    bonding, cause beading on hydrophobic surfaces

18
Water as a reference substance
  • Bounds for liquid state of water define
    temperature measurement scales
  • Example Fahrenheit and Celsius scales
  • Energy specific heat and specific heat capacity

19
Fahrenheit Scale
  • Developed by Gabriel Fahrenheit a thermometer
    maker
  • Scale replaced a previous scale based on body
    temperature
  • Divided temperature difference between water in
    solid state and in gas state into 180º, with 32º
    as the reference for ice
  • Depended upon changes in density of fluids
    (mercury and alcohol)

20
Celsius (Centigrade) Scale
  • Introduced in 1742 by Andreus Celsius
  • A decimal system, with 100º between solid and gas
    phases
  • Reference temperature is 0º at freezing
  • Question at what temperatures are Celsius and
    Fahrenheit readings the same?

21
Modulus of Expansion
  • Liquid
  • Density varies with temperature (mass/volume)
  • Liquid to solid volume expands 9 upon
    freezing
  • If temperature changed from 4ºC ? 4ºC, and we had
    a completely full container, how would the volume
    change?

22
Modulus of Compression
  • Relatively incompressible
  • A 1 psi decreases volume by about 3.410-4
  • ? a pressure of 100 psi would decrease volume by
    about 3.4 10-2
  • Water is efficient in transferring kinetic energy
    when enclosed in a rigid structure

23
Water and Energy Transfer
  • In liquid phase, water absorbs 1 calorie per
    temperature rise of 1º C/cm3
  • An additional 539 calories are needed to go from
    liquid to gas phase
  • Going from liquid to solid phase releases 80
    calories per cm3
  • Change in state releases or absorbs significant
    amounts of energy
  • Liquid water can absorb and store large amounts
    of energy

24
Applications
  • Sweating vaporization for cooling
  • Liquid water on a hot free surface requires 539
    calories per cm3 to become vapor
  • The result is substantial loss of thermal energy
    (cooling)
  • Heat transfer car cooling systems
  • Flowing water efficiently transfers heat away
    from hot spots created by friction

25
Global energy transfer
  • Equatorial zone receives much more solar energy
    than poles
  • Energy transfer from equator is accomplished by
    evaporation, condensation and ocean currents
  • Oceans have tremendous capacity to absorb and
    transfer solar energy

26
Summary
  • Chemical and physical properties of water are
    important and different than many others
  • Hydrogen bonding leads to internal cohesion and
    helps in dissolution of some chemicals
  • Stability in some properties makes it an ideal
    reference substance
  • Also a very good energy transfer medium,
    especially between liquid and vapor states

27
Next time
  • Watershed Delineation
  • Readings p. 175-180
  • Homework due Friday
  • NOAA visit next Wednesday 9/14
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