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Title: CH. 3


1
CH. 3
  • Water and the Fitness of the Environment

2
The Effects of Waters Polarity
  • The polarity of water molecules results in
    hydrogen bonding
  • Organisms depend on the cohesion of water
    molecules
  • Water moderates temperatures on Earth
  • Oceans and lakes dont freeze solid because ice
    floats
  • Water is the solvent of life

3
The polarity of water molecules results in
hydrogen bonding
  • The bonds that hold together the atoms in a water
    molecule are polar covalent bonds, with the
    oxygen region of the molecule having a partial
    negative charge and the hydrogens having a
    partial positive charge.
  • Polar molecule-opposite ends of the molecule have
    opposite charges.
  • The extraordinary qualities of water are emergent
    properties resulting from the hydrogen bonding
    that orders molecules into a higher level of
    structural organization.

4
Organisms depend on the cohesion of water
molecules
  • Water molecules stick to each other as a result
    of hydrogen bonding. In liquid form, water is
    constantly forming, breaking, and reforming, so
    that at any instant a substantial percentage of
    molecules are bonded to their neighbor, making
    water more structured that most liquids.
  • Cohesion-the binding together of like molecules,
    often by hydrogen bonds
  • Cohesion due to hydrogen bonding contributes to
    the transport of water against gravity in plants.
  • Adhesion- the clinging of one substance to
    another
  • Adhesion of water to the walls of the vessels
    helps counter the downward pull of gravity.
  • Surface Tension- a measure of how difficult it is
    to stretch or break the surface of a liquid
  • Water has a greater surface tension than most
    other liquids.

5
Water moderates temperatures on EarthHeat and
Temperature
  • Kinetic energy- the energy of motion
  • Heat- the measure of total quantity of kinetic
    energy due to molecular motion in a body of
    matter
  • Temperature- measures the intensity of heat due
    to the average kinetic energy of the molecules
  • Calorie (cal)- the amount of heat energy it takes
    to raise the temperature of 1 g of water by 1
    degree celsius

6
Water moderates temperatures on EarthWaters
High Specific Heat
  • The ability of water to stabilize temperature
    stems from its relatively high specific heat.
  • Specific heat- the amount of heat that must be
    absorbed or lost for 1 g of that substance to
    change its temperature by 1 degree celsius
  • Because of its high specific heat relative to
    other substances, water will change its
    temperature less when it absorbs or loses a given
    amount of heat.
  • A calorie of heat causes a relatively small
    change in the temperature of water because much
    of the heat energy is used to disrupt hydrogen
    bonds before the water molecules begin moving
    faster.
  • Because of its high specific heat, the water that
    covers most of the Earth keeps temperature
    fluctuations on land and in water within limits
    that permit life. Because organisms are made
    primarily of water, they are more able to resist
    changes in their own temperatures than if they
    were made of a liquid with a lower specific heat.

7
Water moderates temperatures on EarthEvaporative
Cooling
  • Heat of vaporization- the quantity of heat a
    liquid must absorb for 1 g of it to be converted
    from the liquid to the gaseous state
  • Waters high heat of vaporization helps moderate
    Earths climate.
  • Evaporative cooling- as a liquid evaporates, the
    surface of the liquid left behind cools down
  • Provides a mechanism that prevents terrestrial
    organisms from overheating.

8
Oceans and lakes dont freeze solid because ice
floats
  • Water is one of the few substances that are less
    dense as a solid than a liquid. While other
    materials contract when solidified, water
    expands.
  • If ice sank, then eventually all ponds, lakes,
    and even oceans would freeze solid, making life
    as we know it impossible on Earth.

9
Water is the solvent of life
  • Solution- a liquid that is a completely
    homogeneous mixture of two or more substances
  • Solvent- the dissolving agent
  • Solute- the substance being dissolved
  • Aqueous solution- solution where water is the
    solvent
  • Hydration cell- the sphere of water around each
    dissolved ion

10
Water is the solvent of lifeHydrophilic and
Hydrophobic Substances
  • Hydrophilic- substance that has an affinity for
    water
  • Hydrophilic is used even if the substance cant
    be dissolved because the molecules are too
    large, for instance.
  • Cellulose is hydrophilic but has molecules that
    are too large to be dissolved. Cellulose is also
    present in the walls of water-conducting vessels
    in a plant.
  • Hydrophobic- substances that repel water
  • Usually because they are nonpolar or non-ionic
  • Hydrophobic molecules are major ingredients of
    cell membranes

11
Water is the solvent of lifeSolute Concentration
in Aqueous Solutions
  • Most of the chemical reactions that occur in
    organisms involve solutes dissolved in water.
  • Mole (mol)- a practical way to measure molecules
    equal in number to the molecular weight of a
    substance
  • Molecular weight- the sum of the weights of all
    the atoms in a molecule
  • A mole of one substance has the exact same number
    of molecules as a mole of any other substance
  • Avogadros number- 6.02x1023
  • Measuring in moles makes it convenient for
    scientists working in the laboratory to combine
    substances in fixed ratios of molecules.
  • Molarity- the number of moles of solute per liter
    of solution the unit of concentration most often
    used by biologists for aqueous solutions.

12
The Dissociation of Water Molecules
  • Organisms are sensitive to changes in pH
  • Hydroxide ion (OH-) the water molecule that has
    lost a proton charge of -1
  • Hydrogen ion (H) a single proton with a charge
    of 1
  • Acid precipitation threatens the fitness of the
    environment

13
Organisms are sensitive to changes in pHAcids
and Bases
  • Acid- a substance that increases the hydrogen ion
    concentration of a solution
  • Base- substance that reduces the hydrogen ion
    concentration of a solution
  • Some bases reduce H concentration directly by
    accepting hydrogen ions. Other bases reduce the
    H concentration indirectly by dissociating to
    form hydroxide ions, which then combine with
    hydrogen ions in the solution to form water.
  • A solution in which the H and OH- are equal is
    said to be neutral.

14
Organisms are sensitive to changes in pHThe pH
Scale
  • In any aqueous solution the product of H and OH-
    concentrations is constant at 10(-14)
  • An acid not only adds hydrogen ions to a
    solution, but also removes hydroxide ions because
    of the tendency of for H to combine with OH- and
    form water. A base has the opposite effect.
  • The pH of a solution is defined as the negative
    logarithm (base 10) of the hydrogen ion
    concentration
  • The pH of a neutral solution is 7, the midpoint
    of the scale. A pH calue less that 7 denotes an
    acidic solution (the lower the more acidic).The
    pH for basic solutions is above 7.
  • Buffers- substances that minimize changes in the
    concentrations of H and OH- in a solution

15
Acid precipitation threatens the fitness of the
environment
  • One of the most serious assaults on water quality
    is acid precipitation.
  • Acid precipitation- rain, snow, or fog that is
    more acidic than pH 5.6
  • It is caused primarily by the presence in the
    atmosphere of sulfur oxides and nitrogen oxides,
    gaseous compounds that react with water to form
    strong acids, which fall to Earth with rain or
    snow.
  • A major source of the oxides come from the
    burning of fossil fuels.
  • Strong acidity can alter the structure of
    biological molecules and prevent them from
    carrying out the essential chemical processes of
    life.
  • Acid rain and snow can bring about profound
    changes in soils by affecting the solubility of
    soil minerals.
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