Chapter 3, Water
Figure 3.x1 Water
Figure 3.0
Earth
The Chemistry of Water
Earth
is the water planet.
Water
exists as a liquid at relatively low temperatures.
75%
Earths surface is covered by liquid water moderates climate.
Life originated in a medium of water, and
evolved for 3 billion years before moving to land.
2/3
of an organisms body is composed of water.
Life
on earth is possible because of the unique properties of water.
Water molecules act like tiny magnets.
Water
molecules form weak chemical associations with each other called hydrogen
bonds. Hydrogen bond
are the underpinning for all the unique properties of water.
How hydrogen bonds are formed:
The
water molecule has distinct + and charged ends, like two poles of a magnet. A polar molecule.
polar molecules interact to form hydrogen bonds
weak electrostatic attractions between opposite partial charges create a
force that is 5-10% as strong a covalent bond.
Figure 3.1
Hydrogen bonds between water molecules
The Properties of Water
Water
clings to polar molecules
Water
stores heat
Water
is an Excellent Solvent
Water
influences the arrangement of nonpolar molecules
Water
ionizes
Water clings to polar molecules
cohesion: water to water
responsible for surface tension
adhesion: water to other polar molecules
capillary action
Figure 3.3
Walking on water
Figure 3.2
Water transport in plants
Figure 3.2x Trees
Water stores heat
Water
moderates temperature because of two properties: high specific heat and high heat
of vaporization.
Large
input of thermal energy is required to break hydrogen bonds.
Figure 3.x1 Water
Specific heat
Specific
heat is defined as the amount of heat that must be absorbed or lost by 1 gram
of substance to change its temperature by 1 degree Celsius.
Water
has a specific heat of 1 calorie/gram/◦C
This
is 2X that of most carbon compounds
9X
higher than iron
NH3,
which is more polar than water, has a higher specific
heat (1.23 calories/ gram/◦C).
Effects of having a high specific heat
heats up more slowly and holds temperature longer
allows organisms to regulate body temperature
large bodies of water on Earth moderate climate
Heat of Vaporization
Transition
of from liquid to a gas require input of energy to break H-bonds, therefore
evaporation of water from a surface causes cooling.
Temperature
regulation by evaporative cooling sweating
Figure 3.4
Evaporative cooling
Ice is less dense than water
Water
freezes at lower temperature than predicted because of cohesion from H
bonds. Ice is less dense than water
because H-bonds now are rigid, and making spaces in
the crystal.
Figure 3.6x2 Ice floats and frozen benzene sinks
Figure 3.5
The structure of ice (Layer 1)
Figure 3.5
The structure of ice (Layer 2)
Figure 3.5x1 Ice, water, and steam
Water is an Excellent Solvent (for polar molecules!)
interacts with polar groups on molecules, pulls them away from the
solid, then covers them with a hydrogen shell so they dont re-associate
blood, cytoplasm are complex solutions using water as the solvent
Figure 3.7
A crystal of table salt dissolving in water
Figure 3.8
A water-soluble protein
Water influences the arrangement of nonpolar molecules
polar molecules are hydrophilic, whereas non-polar molecules are hydrophobic
Carbon compounds largely hydrophobic because covalent bonds
in carbon share electron equally, nonpolar.
Water influences the arrangement of nonpolar molecules, cont
when polar molecules aggregate in water, they push away hydrophobic
molecules: hydrophobic exclusion
This
cause particular shapes and arrangements to form.
Ex.
cellular membranes, protein structure
Water ionizes
H2O
→ H+
+ OH-
At
25 degrees Celsius
1
out of every 550 million water molecules dissociates
one liter of water contains 10-7 moles of H+ ions, or 10-7
moles/liter.
one mole is 6.02 x 1023 molecules, (Avagadros
number)
[ ] means concentration
Unnumbered Figure (page 47) Chemical reaction: hydrogen bond shift
The pH Scale
pH = -log [H+]
So,
pure water, with a [H+] of 10-7 moles/liter, has a pH of
7.
The
pH scale is logarithmic
the lower the pH value, the greater the [H+].
Each
difference of 1 indicates a 10X change in pH.
Figure 3.9
The pH of some aqueous solutions
Acids and Bases
Acid:
a substance that increases the [H+] when in dissociates in water.
Base:
a substance that increases the [OH-] when in dissociates in water.
Figure 3.10 The effects of acid precipitation on a
forest
Figure 3.10x1 Pulp mill
Figure 3.10x2 Acid rain damage to statuary, 1908
& 1968
Buffers
Essential
that pH inside living cells and surrounding fluids is kept to a narrow range,
usually ph 7.
However,
chemical reactions of life constantly produce acids and bases!
Buffer:
a substance that acts as a reservoir for hydrogen ions. Donates to solution when
they fall, or takes them up from the solution when they are in excess.
Examples of Buffers
Example:
carbonic acid and bicarbonate in human blood, Fig. 2.2
H2O
+ CO2 ↔ H2CO3 ↔ HCO3-
+ H+
The End.