Akhuwat Faisalabad Institute Of Research Science and
Technology.....
This video is a course context of 1st prof Bs (hons) biotechnology.. which is prepared by momin khan niazi...........
1. 4.Properties of Water and Aqueous Solutions
Course: Introduction to Biotechnology
Instructor: Moman Niazi
2.
3. Properties of Water
• Polar molecule
• Cohesion and
adhesion
• High specific heat
• Density – greatest
at 4oC
• Universal solvent of
life
4. Polarity of Water
• In a water molecule two hydrogen atoms
form single polar covalent bonds with an
oxygen atom. Gives water more structure
than other liquids
– Because oxygen is more electronegative, the
region around oxygen has a partial negative
charge.
– The region near the two hydrogen atoms has a
partial positive charge.
• A water molecule is a polar molecule with
opposite ends of the molecule with opposite
charges.
6. HYDROGEN BONDS
• Hold water molecules
together
• Each water molecule can
form a maximum of 4
hydrogen bonds
• The hydrogen bonds
joining water molecules
are weak, about 1/20th as
strong as covalent bonds.
• They form, break, and
reform with great
frequency
• Extraordinary Properties that
are a result of hydrogen
bonds.
– Cohesive behavior
– Resists changes in temperature
– High heat of vaporization
– Expands when it freezes
– Versatile solvent
7. Organisms Depend on Cohesion
• Cohesion is responsible for the
transport of the water column in
plants
• Cohesion among water molecules
plays a key role in the transport of
water against gravity in plants
• Adhesion, clinging
of one substance to
another, contributes
too, as water adheres
to the wall of the
vessels.
Hydrogen bonds hold the substance
together, a phenomenon called cohesion
9. Moderates Temperatures on Earth
• What is kinetic energy?
• Heat?
• Temperature?
• Calorie?
• What is the difference in
cal and Cal?
• What is specific heat?
Celsius Scale at Sea Level
100oC Water boils
37oC Human body temperature
23oC Room temperature
0oC Water freezes
Water stabilizes air temperatures by absorbing heat from warmer air and releasing
heat to cooler air.
Water can absorb or release relatively large amounts of heat with only a slight change
in its own temperature.
10. Three-fourths of the earth is covered
by water. The water serves as a
large heat sink responsible for:
1. Prevention of temperature
fluctuations that are outside the
range suitable for life.
2. Coastal areas having a mild
climate
3. A stable marine environment
Specific Heat is the amount of heat that must be
absorbed or lost for one gram of a substance to change
its temperature by 1oC.
11. Evaporative Cooling
• The cooling of a
surface occurs when
the liquid evaporates
• This is responsible for:
– Moderating earth’s
climate
– Stabilizes
temperature in
aquatic ecosystems
– Preventing organisms
from overheating
12. Density of Water
• Most dense at 4oC
• Contracts until 4oC
• Expands from 4oC to
0oC
The density of water:
1. Prevents water from freezing from the bottom up.
2. Ice forms on the surface first—the freezing of the
water releases heat to the water below creating
insulation.
3. Makes transition between season less abrupt.
14. Solvent for Life
• Solution
– Solute
– solvent
• Aqueous solution
• Hydrophilic
– Ionic compounds
dissolve in water
– Polar molecules
(generally) are water
soluble
• Hydrophobic
– Nonpolar compounds
15. Most biochemical reactions involve
solutes dissolved in water.
• There are two important quantitative
proprieties of aqueous solutions.
–1. Concentration
–2. pH
16. Concentration of a Solution
• Molecular weight – sum of the weights of all atoms in
a molecule (daltons)
• Mole – amount of a substance that has a mass in
grams numerically equivalent to its molecular weight
in daltons.
• Avogadro’s number – 6.02 X 1023
– A mole of one substance has the same number of molecules
as a mole of any other substance.
17. Molarity
The concentration of a material in solution is called its molarity.
A one molar solution has one mole of a substance dissolved in one liter of solvent,
typically water.
Calculate a one molar solution of sucrose, C12H22O16.
C = 12 daltons
H = 1 dalton
O = 16 daltons
12 x12 = 144
1 x 22 = 22
16 x 11 = 176
342
For a 2M solution?
For a .05 M solution?
For a .2 M solution?
19. • A simpler way to view this process is that a
water molecule dissociates into a hydrogen ion
and a hydroxide ion:
– H2O <=> H+ + OH-
• This reaction is reversible.
• At equilibrium the concentration of water
molecules greatly exceeds that of H+ and OH-.
• In pure water only one water molecule in every
554 million is dissociated.
– At equilibrium, the concentration of H+ or OH-
is 10-7M (25°C) .
20. Acids and Bases
• An acid is a substance that
increases the hydrogen ion
concentration in a solution.
• Any substance that reduces the
hydrogen ion concentration in a
solution is a base.
– Some bases reduce H+ directly by
accepting hydrogen ions.
• Strong acids and bases complete
dissociate in water.
• Weak acids and bases dissociate
only partially and reversibly.
21. pH Scale
• The pH scale in any aqueous solution :
– [ H+ ] [OH-] = 10-14
• Measures the degree of acidity (0 – 14)
• Most biologic fluids are in the pH range
from 6 – 8
• Each pH unit represents a tenfold
difference (scale is logarithmic)
– A small change in pH actually indicates a
substantial change in H+ and OH-
concentrations.
22. Buffers
• A substance that eliminates large sudden
changes in pH.
• Buffers help organisms maintain the pH of
body fluids within the narrow range
necessary for life.
–Are combinations of H+ acceptors and
donors forms in a solution of weak acids
or bases
–Work by accepting H+ from solutions
when they are in excess and by donating
H+ when they have been depleted.
23. Acid Precipitation
• Rain, snow or fog with more strongly acidic than pH
of 5.6
• West Virginia has recorded 1.5
• East Tennessee reported 4.2 in 2000
• Occurs when sulfur oxides and nitrogen oxides react
with water in the atmosphere
– Lowers pH of soil which affects mineral solubility
– decline of forests
– Lower pH of lakes and ponds – In the Western
Adirondack Mountains, there are lakes with a pH
<5 that have no fish.
24. Copyright McGraw-Hill 2009 24
4.1 General Properties of
Aqueous Solutions
• Solution - a homogeneous mixture
– Solute: the component that is dissolved
– Solvent: the component that does the
dissolving
Generally, the component present in the greatest
quantity is considered to be the solvent.
Aqueous solutions are those in which water is
the solvent.
25. Copyright McGraw-Hill 2009 25
• Electrolytes and Nonelectrolytes
– Electrolyte: substance that dissolved in water
produces a solution that conducts electricity
• Contains ions
– Nonelectrolyte: substance that dissolved in water
produces a solution that does not conduct
electricity
• Does not contain ions
26. Copyright McGraw-Hill 2009 26
• Dissociation - ionic compounds separate
into constituent ions when dissolved in
solution
• Ionization - formation of ions by molecular
compounds when dissolved
27. Copyright McGraw-Hill 2009 27
• Strong and weak electrolytes
– Strong Electrolyte: 100% dissociation
• All water soluble ionic compounds, strong
acids and strong bases
– Weak electrolytes
• Partially ionized in solution
• Exist mostly as the molecular form in
solution
• Weak acids and weak bases
29. Copyright McGraw-Hill 2009 29
• Examples of weak electrolytes
– Weak acids
HC2H3O2(aq) C2H3O2
(aq) + H+
(aq)
– Weak bases
NH3 (aq) + H2O(l) NH4
+
(aq) + OH
(aq)
(Note: double arrows indicate a reaction that
occurs in both directions - a state of dynamic
equilibrium exists)
30. Copyright McGraw-Hill 2009 30
Method to Distinguish Types of Electrolytes
nonelectrolyte weak electrolyte strong electrolyte
31. Copyright McGraw-Hill 2009 31
Classify the following as nonelectrolyte,
weak electrolyte or strong electrolyte
– NaOH
strong electrolyte
– CH3OH
nonelectrolyte
– H2CO3
weak electrolyte
32. Copyright McGraw-Hill 2009 32
4.2 Precipitation Reactions
• Precipitation (formation of a solid from two
aqueous solutions) occurs when product is
insoluble
• Produce insoluble ionic compounds
• Double replacement (or metathesis reaction)
• Solubility is the maximum amount of a solid that
can dissolve in a given amount of solvent at a
specified temperature
• Prediction based on solubility rules