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Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
PowerPoint®
Lecture Presentations for
Biology
Eighth Edition
Neil Campbell and Jane Reece
Lectures by Chris Romero, updated by Erin Barley with contributions from Joan Sharp
Chapter 3
Water and the Fitness of
the Environment
Overview: The Molecule That Supports All of Life
• Water is the biological medium on Earth
• All living organisms require water more than
any other substance
• Most cells are surrounded by water, and cells
themselves are about 70–95% water
• The abundance of water is the main reason the
Earth is habitable
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-1
Concept 3.1: The polarity of water molecules
results in hydrogen bonding
• The water molecule is a polar molecule: The
opposite ends have opposite charges
• Polarity allows water molecules to form
hydrogen bonds with each other
Animation: Water StructureAnimation: Water Structure
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-2
Hydrogen
bond
δ –
H
δ +
H
O
——
——
δ +
δ +
δ +
δ –
δ –
δ –
Fig. 3-UN1
Concept 3.2: Four emergent properties of water
contribute to Earth’s fitness for life
• Four of water’s properties that facilitate an
environment for life are:
– Cohesive behavior
– Ability to moderate temperature
– Expansion upon freezing
– Versatility as a solvent
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Cohesion
• Collectively, hydrogen bonds hold water
molecules together, a phenomenon called
cohesion
• Cohesion helps the transport of water against
gravity in plants
• Adhesion is an attraction between different
substances, for example, between water and
plant cell walls
Animation: Water TransportAnimation: Water Transport
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-3
Water-conducting
cells
Adhesion
Cohesion
150 µm
Direction
of water
movement
• Surface tension is a measure of how hard it is
to break the surface of a liquid
• Surface tension is related to cohesion
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-4
Moderation of Temperature
• Water absorbs heat from warmer air and
releases stored heat to cooler air
• Water can absorb or release a large amount of
heat with only a slight change in its own
temperature
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Heat and Temperature
• Kinetic energy is the energy of motion
• Heat is a measure of the total amount of kinetic
energy due to molecular motion
• Temperature measures the intensity of heat
due to the average kinetic energy of molecules
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• The Celsius scale is a measure of
temperature using Celsius degrees (°C)
• A calorie (cal) is the amount of heat required
to raise the temperature of 1 g of water by 1°C
• The “calories” on food packages are actually
kilocalories (kcal), where 1 kcal = 1,000 cal
• The joule (J) is another unit of energy where
1 J = 0.239 cal, or 1 cal = 4.184 J
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Water’s High Specific Heat
• The specific heat of a substance is the
amount of heat that must be absorbed or lost
for 1 g of that substance to change its
temperature by 1ÂşC
• The specific heat of water is 1 cal/g/ºC
• Water resists changing its temperature
because of its high specific heat
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Water’s high specific heat can be traced to
hydrogen bonding
– Heat is absorbed when hydrogen bonds break
– Heat is released when hydrogen bonds form
• The high specific heat of water minimizes
temperature fluctuations to within limits that
permit life
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-5
San Diego 72°
40 miles
Pacific Ocean
70s (°F)
80s
90s
100s
Santa Barbara 73°
Los Angeles
(Airport) 75°
Burbank
90°
San Bernardino
100°
Riverside 96°
Santa Ana
84°
Palm Springs
106°
Evaporative Cooling
• Evaporation is transformation of a substance
from liquid to gas
• Heat of vaporization is the heat a liquid must
absorb for 1 g to be converted to gas
• As a liquid evaporates, its remaining surface
cools, a process called evaporative cooling
• Evaporative cooling of water helps stabilize
temperatures in organisms and bodies of water
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Insulation of Bodies of Water by Floating Ice
• Ice floats in liquid water because hydrogen
bonds in ice are more “ordered,” making ice
less dense
• Water reaches its greatest density at 4°C
• If ice sank, all bodies of water would eventually
freeze solid, making life impossible on Earth
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-6
Hydrogen
bond
Liquid water
Hydrogen bonds break and re-form
Ice
Hydrogen bonds are stable
Fig. 3-6a
Hydrogen
bond
Liquid water
Hydrogen bonds break and re-form
Ice
Hydrogen bonds are stable
The Solvent of Life
• A solution is a liquid that is a homogeneous
mixture of substances
• A solvent is the dissolving agent of a solution
• The solute is the substance that is dissolved
• An aqueous solution is one in which water is
the solvent
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Water is a versatile solvent due to its polarity,
which allows it to form hydrogen bonds easily
• When an ionic compound is dissolved in water,
each ion is surrounded by a sphere of water
molecules called a hydration shell
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-7
Cl–
Na
Cl–
+
+
+
+
+
+
+
+
–
–
–
–
–
–
–
–
Na+
–
–
–
+
• Water can also dissolve compounds made of
nonionic polar molecules
• Even large polar molecules such as proteins
can dissolve in water if they have ionic and
polar regions
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-8
(a) Lysozyme molecule in a
nonaqueous environment
(b) Lysozyme molecule (purple) in an aqueous
environment
(c) Ionic and polar regions
on the protein’s surface
attract water molecules.
Fig. 3-8ab
(b) Lysozyme molecule (purple) in an aqueous
environment
(a) Lysozyme molecule in a
nonaqueous environment
Fig. 3-8bc
(c) Ionic and polar regions
on the protein’s surface
attract water molecules.
(b) Lysozyme molecule (purple) in an aqueous
environment
Hydrophilic and Hydrophobic Substances
• A hydrophilic substance is one that has an
affinity for water
• A hydrophobic substance is one that does not
have an affinity for water
• Oil molecules are hydrophobic because they
have relatively nonpolar bonds
• A colloid is a stable suspension of fine
particles in a liquid
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Solute Concentration in Aqueous Solutions
• Most biochemical reactions occur in water
• Chemical reactions depend on collisions of
molecules and therefore on the concentration
of solutes in an aqueous solution
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Molecular mass is the sum of all masses of all
atoms in a molecule
• Numbers of molecules are usually measured in
moles, where 1 mole (mol) = 6.02 x 1023
molecules
• Avogadro’s number and the unit dalton were
defined such that 6.02 x 1023
daltons = 1 g
• Molarity (M) is the number of moles of solute
per liter of solution
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Concept 3.3: Acidic and basic conditions affect
living organisms
• A hydrogen atom in a hydrogen bond between
two water molecules can shift from one to the
other:
– The hydrogen atom leaves its electron behind
and is transferred as a proton, or hydrogen
ion (H+
)
– The molecule with the extra proton is now a
hydronium ion (H3O+
), though it is often
represented as H+
– The molecule that lost the proton is now a
hydroxide ion (OH–
)
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Water is in a state of dynamic equilibrium in
which water molecules dissociate at the same
rate at which they are being reformed
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-UN2
Hydronium
ion (H3O+
)
Hydroxide
ion (OH–
)
2H2O
H
H
H
H
H
H
H
H
OOOO
• Though statistically rare, the dissociation of
water molecules has a great effect on
organisms
• Changes in concentrations of H+
and OH–
can
drastically affect the chemistry of a cell
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Effects of Changes in pH
• Concentrations of H+
and OH–
are equal in pure
water
• Adding certain solutes, called acids and bases,
modifies the concentrations of H+
and OH–
• Biologists use something called the pH scale to
describe whether a solution is acidic or basic
(the opposite of acidic)
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Acids and Bases
• An acid is any substance that increases the H+
concentration of a solution
• A base is any substance that reduces the H+
concentration of a solution
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
The pH Scale
• In any aqueous solution at 25°C the product of
H+
and OH–
is constant and can be written as
[H+
]
[OH–
] = 10–14
• The pH of a solution is defined by the negative
logarithm of H+
concentration, written as
pH = –log [H+
]
• For a neutral aqueous solution
[H+
] is 10–7
= –(–7) = 7
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Acidic solutions have pH values less than 7
• Basic solutions have pH values greater than 7
• Most biological fluids have pH values in the
range of 6 to 8
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-9
Neutral
solution
Acidic
solution
Basic
solution
OH–
OH–
OH–
OH–
OH–
OH–
OH–
H+
H+
H+
OH–
H+
H+
H+ H+
OH–
OH–
OH–
OH–
H+
OH–
H+
H+
H+
H+
H+
H+
H+
OH–
Neutral
[H+
] = [OH–
]
IncreasinglyAcidic
[H+
]>[OH–
]
IncreasinglyBasic
[H+
]<[OH–
]
pH Scale
0
1
2
3
4
5
6
7
8
Battery acid
Gastric juice,
lemon juice
Vinegar, beer,
wine, cola
Tomato juice
Black coffee
Rainwater
Urine
Saliva
Pure water
Human blood, tears
Seawater
9
10
Milk of magnesia
Household ammonia
Household
bleach
Oven cleaner
11
12
13
14
Buffers
• The internal pH of most living cells must
remain close to pH 7
• Buffers are substances that minimize changes
in concentrations of H+
and OH–
in a solution
• Most buffers consist of an acid-base pair that
reversibly combines with H+
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Threats to Water Quality on Earth
• Acid precipitation refers to rain, snow, or fog
with a pH lower than 5.6
• Acid precipitation is caused mainly by the
mixing of different pollutants with water in the
air and can fall at some distance from the
source of pollutants
• Acid precipitation can damage life in lakes and
streams
• Effects of acid precipitation on soil chemistry
are contributing to the decline of some forests
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-10
More
acidic
0
Acid
rain
Acid
rain
Normal
rain
More
basic
1
2
3
4
5
6
7
8
9
10
11
12
13
14
• Human activities such as burning fossil fuels
threaten water quality
• CO2 is released by fossil fuel combustion and
contributes to:
– A warming of earth called the “greenhouse”
effect
– Acidification of the oceans; this leads to a
decrease in the ability of corals to form calcified
reefs
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fig. 3-11
EXPERIMENT
RESULTS
Calcificationrate
(mmolCaCO3
perm2
perday)
[CO3
2–
] (µmol/kg)
150 200 250 300
0
20
40
Fig. 3-11a
EXPERIMENT
Fig. 3-11b
Calcificationrate
(mmolCaCO3
perm2
perday)
40
20
0
300150 200 250
[CO3
2–
] (µmol/kg)
RESULTS
Fig. 3-UN3
Hydrogen
bond
δ –
δ +
δ +
δ +
δ +
δ –
δ –
δ –
H
H
O
Fig. 3-UN4
Liquid water:
transient hydrogen
bonds
Ice: stable hydro-
gen bonds
Fig. 3-UN5
Bases donate OH–
or accept H+
in
aqueous solutions
Acids donate H+
in
aqueous solutions
Acidic
[H+
] > [OH–
]
Neutral
[H+
] = [OH–
]
Basic
[H+
] < [OH–
]
14
7
0
Fig. 3-UN6
Surface of EarthSurface of Mars
Fig. 3-UN7
You should now be able to:
1. List and explain the four properties of water
that emerge as a result of its ability to form
hydrogen bonds
2. Distinguish between the following sets of
terms: hydrophobic and hydrophilic
substances; a solute, a solvent, and a
solution
3. Define acid, base, and pH
4. Explain how buffers work
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings

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Water Properties Support Life

  • 1. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings PowerPoint® Lecture Presentations for Biology Eighth Edition Neil Campbell and Jane Reece Lectures by Chris Romero, updated by Erin Barley with contributions from Joan Sharp Chapter 3 Water and the Fitness of the Environment
  • 2. Overview: The Molecule That Supports All of Life • Water is the biological medium on Earth • All living organisms require water more than any other substance • Most cells are surrounded by water, and cells themselves are about 70–95% water • The abundance of water is the main reason the Earth is habitable Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 4. Concept 3.1: The polarity of water molecules results in hydrogen bonding • The water molecule is a polar molecule: The opposite ends have opposite charges • Polarity allows water molecules to form hydrogen bonds with each other Animation: Water StructureAnimation: Water Structure Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 5. Fig. 3-2 Hydrogen bond δ – H δ + H O —— —— δ + δ + δ + δ – δ – δ –
  • 7. Concept 3.2: Four emergent properties of water contribute to Earth’s fitness for life • Four of water’s properties that facilitate an environment for life are: – Cohesive behavior – Ability to moderate temperature – Expansion upon freezing – Versatility as a solvent Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 8. Cohesion • Collectively, hydrogen bonds hold water molecules together, a phenomenon called cohesion • Cohesion helps the transport of water against gravity in plants • Adhesion is an attraction between different substances, for example, between water and plant cell walls Animation: Water TransportAnimation: Water Transport Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 10. • Surface tension is a measure of how hard it is to break the surface of a liquid • Surface tension is related to cohesion Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 12. Moderation of Temperature • Water absorbs heat from warmer air and releases stored heat to cooler air • Water can absorb or release a large amount of heat with only a slight change in its own temperature Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 13. Heat and Temperature • Kinetic energy is the energy of motion • Heat is a measure of the total amount of kinetic energy due to molecular motion • Temperature measures the intensity of heat due to the average kinetic energy of molecules Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 14. • The Celsius scale is a measure of temperature using Celsius degrees (°C) • A calorie (cal) is the amount of heat required to raise the temperature of 1 g of water by 1°C • The “calories” on food packages are actually kilocalories (kcal), where 1 kcal = 1,000 cal • The joule (J) is another unit of energy where 1 J = 0.239 cal, or 1 cal = 4.184 J Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 15. Water’s High Specific Heat • The specific heat of a substance is the amount of heat that must be absorbed or lost for 1 g of that substance to change its temperature by 1ÂşC • The specific heat of water is 1 cal/g/ÂşC • Water resists changing its temperature because of its high specific heat Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 16. • Water’s high specific heat can be traced to hydrogen bonding – Heat is absorbed when hydrogen bonds break – Heat is released when hydrogen bonds form • The high specific heat of water minimizes temperature fluctuations to within limits that permit life Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 17. Fig. 3-5 San Diego 72° 40 miles Pacific Ocean 70s (°F) 80s 90s 100s Santa Barbara 73° Los Angeles (Airport) 75° Burbank 90° San Bernardino 100° Riverside 96° Santa Ana 84° Palm Springs 106°
  • 18. Evaporative Cooling • Evaporation is transformation of a substance from liquid to gas • Heat of vaporization is the heat a liquid must absorb for 1 g to be converted to gas • As a liquid evaporates, its remaining surface cools, a process called evaporative cooling • Evaporative cooling of water helps stabilize temperatures in organisms and bodies of water Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 19. Insulation of Bodies of Water by Floating Ice • Ice floats in liquid water because hydrogen bonds in ice are more “ordered,” making ice less dense • Water reaches its greatest density at 4°C • If ice sank, all bodies of water would eventually freeze solid, making life impossible on Earth Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 20. Fig. 3-6 Hydrogen bond Liquid water Hydrogen bonds break and re-form Ice Hydrogen bonds are stable
  • 21. Fig. 3-6a Hydrogen bond Liquid water Hydrogen bonds break and re-form Ice Hydrogen bonds are stable
  • 22. The Solvent of Life • A solution is a liquid that is a homogeneous mixture of substances • A solvent is the dissolving agent of a solution • The solute is the substance that is dissolved • An aqueous solution is one in which water is the solvent Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 23. • Water is a versatile solvent due to its polarity, which allows it to form hydrogen bonds easily • When an ionic compound is dissolved in water, each ion is surrounded by a sphere of water molecules called a hydration shell Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 25. • Water can also dissolve compounds made of nonionic polar molecules • Even large polar molecules such as proteins can dissolve in water if they have ionic and polar regions Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 26. Fig. 3-8 (a) Lysozyme molecule in a nonaqueous environment (b) Lysozyme molecule (purple) in an aqueous environment (c) Ionic and polar regions on the protein’s surface attract water molecules.
  • 27. Fig. 3-8ab (b) Lysozyme molecule (purple) in an aqueous environment (a) Lysozyme molecule in a nonaqueous environment
  • 28. Fig. 3-8bc (c) Ionic and polar regions on the protein’s surface attract water molecules. (b) Lysozyme molecule (purple) in an aqueous environment
  • 29. Hydrophilic and Hydrophobic Substances • A hydrophilic substance is one that has an affinity for water • A hydrophobic substance is one that does not have an affinity for water • Oil molecules are hydrophobic because they have relatively nonpolar bonds • A colloid is a stable suspension of fine particles in a liquid Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 30. Solute Concentration in Aqueous Solutions • Most biochemical reactions occur in water • Chemical reactions depend on collisions of molecules and therefore on the concentration of solutes in an aqueous solution Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 31. • Molecular mass is the sum of all masses of all atoms in a molecule • Numbers of molecules are usually measured in moles, where 1 mole (mol) = 6.02 x 1023 molecules • Avogadro’s number and the unit dalton were defined such that 6.02 x 1023 daltons = 1 g • Molarity (M) is the number of moles of solute per liter of solution Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 32. Concept 3.3: Acidic and basic conditions affect living organisms • A hydrogen atom in a hydrogen bond between two water molecules can shift from one to the other: – The hydrogen atom leaves its electron behind and is transferred as a proton, or hydrogen ion (H+ ) – The molecule with the extra proton is now a hydronium ion (H3O+ ), though it is often represented as H+ – The molecule that lost the proton is now a hydroxide ion (OH– ) Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 33. • Water is in a state of dynamic equilibrium in which water molecules dissociate at the same rate at which they are being reformed Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 34. Fig. 3-UN2 Hydronium ion (H3O+ ) Hydroxide ion (OH– ) 2H2O H H H H H H H H OOOO
  • 35. • Though statistically rare, the dissociation of water molecules has a great effect on organisms • Changes in concentrations of H+ and OH– can drastically affect the chemistry of a cell Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 36. Effects of Changes in pH • Concentrations of H+ and OH– are equal in pure water • Adding certain solutes, called acids and bases, modifies the concentrations of H+ and OH– • Biologists use something called the pH scale to describe whether a solution is acidic or basic (the opposite of acidic) Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 37. Acids and Bases • An acid is any substance that increases the H+ concentration of a solution • A base is any substance that reduces the H+ concentration of a solution Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 38. The pH Scale • In any aqueous solution at 25°C the product of H+ and OH– is constant and can be written as [H+ ] [OH– ] = 10–14 • The pH of a solution is defined by the negative logarithm of H+ concentration, written as pH = –log [H+ ] • For a neutral aqueous solution [H+ ] is 10–7 = –(–7) = 7 Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 39. • Acidic solutions have pH values less than 7 • Basic solutions have pH values greater than 7 • Most biological fluids have pH values in the range of 6 to 8 Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 40. Fig. 3-9 Neutral solution Acidic solution Basic solution OH– OH– OH– OH– OH– OH– OH– H+ H+ H+ OH– H+ H+ H+ H+ OH– OH– OH– OH– H+ OH– H+ H+ H+ H+ H+ H+ H+ OH– Neutral [H+ ] = [OH– ] IncreasinglyAcidic [H+ ]>[OH– ] IncreasinglyBasic [H+ ]<[OH– ] pH Scale 0 1 2 3 4 5 6 7 8 Battery acid Gastric juice, lemon juice Vinegar, beer, wine, cola Tomato juice Black coffee Rainwater Urine Saliva Pure water Human blood, tears Seawater 9 10 Milk of magnesia Household ammonia Household bleach Oven cleaner 11 12 13 14
  • 41. Buffers • The internal pH of most living cells must remain close to pH 7 • Buffers are substances that minimize changes in concentrations of H+ and OH– in a solution • Most buffers consist of an acid-base pair that reversibly combines with H+ Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 42. Threats to Water Quality on Earth • Acid precipitation refers to rain, snow, or fog with a pH lower than 5.6 • Acid precipitation is caused mainly by the mixing of different pollutants with water in the air and can fall at some distance from the source of pollutants • Acid precipitation can damage life in lakes and streams • Effects of acid precipitation on soil chemistry are contributing to the decline of some forests Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 44. • Human activities such as burning fossil fuels threaten water quality • CO2 is released by fossil fuel combustion and contributes to: – A warming of earth called the “greenhouse” effect – Acidification of the oceans; this leads to a decrease in the ability of corals to form calcified reefs Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
  • 48. Fig. 3-UN3 Hydrogen bond δ – δ + δ + δ + δ + δ – δ – δ – H H O
  • 49. Fig. 3-UN4 Liquid water: transient hydrogen bonds Ice: stable hydro- gen bonds
  • 50. Fig. 3-UN5 Bases donate OH– or accept H+ in aqueous solutions Acids donate H+ in aqueous solutions Acidic [H+ ] > [OH– ] Neutral [H+ ] = [OH– ] Basic [H+ ] < [OH– ] 14 7 0
  • 51. Fig. 3-UN6 Surface of EarthSurface of Mars
  • 53. You should now be able to: 1. List and explain the four properties of water that emerge as a result of its ability to form hydrogen bonds 2. Distinguish between the following sets of terms: hydrophobic and hydrophilic substances; a solute, a solvent, and a solution 3. Define acid, base, and pH 4. Explain how buffers work Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings

Editor's Notes

  1. Figure 3.1 Why does the abundance of water allow life to exist on the planet Earth?
  2. Figure 3.2 Hydrogen bonds between water molecules
  3. Figure 3.3 Water transport in plants
  4. Figure 3.4 Walking on water
  5. Figure 3.5 The effect of a large body of water on climate
  6. Figure 3.6 Ice: crystalline structure and floating barrier
  7. Figure 3.6 Ice: crystalline structure and floating barrier
  8. Figure 3.7 Table salt dissolving in water
  9. Figure 3.8 A water-soluble protein
  10. Figure 3.8 A water-soluble protein
  11. Figure 3.8 A water-soluble protein
  12. Figure 3.9 The pH scale and pH values of some aqueous solutions
  13. Figure 3.10 Acid precipitation and its effects on a forest
  14. Figure 3.11 What is the effect of carbonate ion concentration on coral reef calcification?
  15. Figure 3.11 What is the effect of carbonate ion concentration on coral reef calcification?
  16. Figure 3.11 What is the effect of carbonate ion concentration on coral reef calcification?