Self Ionisation of Water
Water undergoes Self Ionisation
⇄
H2O(l)
H+(aq)
OH-(aq)
+
or
H2O(l)
+
H2O(l) ⇄
H3O+(aq)
-
+ OH (aq)
The concentration of H+ ions and OH- ions
is extremely small.
Because the equilibrium lies very much on the left hand
side.
Ionic Product of Water
H2O(l)
⇄
H+(aq) + OH-(aq)
Kc
=
In the above expression, the value of [H2O] may be taken as having a
constant value because the degree of ionisation is so small.
Kc
=
Kc [H2O] = [H+] [OH-]
Both Kc and [H2O] are constant values so
Kw = Kc [H2O] = [H+] [OH-]
Kw = [H+] [OH-] is the ionic product of water
Acid–Base Concentrations in Solutions
concentration (moles/L)
10-1
OH-
H+
10-7
H+
OH-
OH-
H+
10-14
[H+] > [OH-]
[H+] = [OH-]
acidic
solution
neutral
solution
[H+] < [OH-]
basic
solution
pH Scale
Soren Sorensen
(1868 - 1939)
The pH scale was invented by the Danish chemist
Soren Sorensen to measure the acidity of beer in a
brewery. The pH scale measured the concentration of
hydrogen ions in solution. The more hydrogen ions,
the stronger the acid.
The pH Scale
1
2
Strong
Acid
3
4
Weak
Acid
5
6
7
Neutral
8
9
10
11
Weak
Alkali
12
13
14
Strong
Alkali
pH Scale
The quantity of hydrogen ions in
solution can affect the color of
certain dyes found in nature. These
dyes can be used as indicators to
test for acids and alkalis.
An
indicator such as litmus (obtained
from lichen) is red in acid. If base is
slowly added, the litmus will turn
blue when the acid has been
neutralized, at about 6-7 on the pH
scale. Other indicators will change
color at different pH’s.
A
combination of indicators is used to
make a universal indicator.
Measuring pH
• Universal Indicator Paper
• Universal Indicator Solution
• pH meter
Measuring pH
pH can be measured in several ways
– Usually it is measured with a coloured acidbase indicator or a pH meter
– Coloured indicators are a crude measure of
pH, but are useful in certain applications
– pH meters are more accurate, but they must
be calibrated prior to use with a solution of
known pH
Limitations of pH Scale
The pH scale ranges from 0 to 14
Values outside this range are possible
but do not tend to be accurate because
even strong acids and bases do not
dissociate
completely
in
highly
concentrated solutions.
pH is confined to dilute aqueous solutions
pH
At 250C
Kw = 1 x 10-14 mol2/litre2
[H+ ] x [OH- ] = 1 x 10-14 mol2/litre2
This equilibrium constant is very important because it
applies to all aqueous solutions - acids, bases, salts,
and non-electrolytes - not just to pure water.
For H2O(l) ⇄
→
pH
H+(aq) + OH-(aq)
[H+ ] =
[H+ ] x [OH- ] = 1 x 10-14
[OH- ]
= [1 x 10-7 ] x [1 x 10-7 ]
[H+ ] of water is at 250C is 1 x 10-7 mol/litre
Replacing [H+ ] with pH to indicate acidity of solutions
pH 7 replaces [H+ ] of 1 x 10-7 mol/litre
where
pH =
- Log10 [H+ ]
pH is temperature dependent
T (°C)
pH
0
7.12
10
7.06
20
7.02
25
7
30
6.99
40 as the temperature
6.97
pH of pure water decreases
increases
A word of warning!
If the pH falls as temperature increases, does this mean that water
becomes more acidic at higher temperatures?
NO!
Remember a solution is acidic if there is an excess of hydrogen ions over hydroxide ions.
In the case of pure water, there are always the same number of hydrogen ions and
hydroxide ions. This means that the water is always neutral - even if its pH change
Acid – Base Concentrations and pH
concentration (moles/L)
10-1
pH = 11
pH = 3
OH-
H+
pH = 7
10-7
H+
OH-
OH-
H+
10-14
[H3O+] > [OH-] [H3O+] = [OH-]
acidic
solution
neutral
solution
[H3O+] < [OH-]
basic
solution
• pH describes both [H+ ] and [OH- ]
0
Acidic
pH
7
Neutral
pH
14
Basic
pH
[H+ ] = 100
= 0
[OH- ] =10-14
pOH
[H+ ] = 10-7
= 7
[H+ ] = 10-14
= 14
= 14
[OH- ] =10-7
pOH
= 7
[OH- ] = 100
pOH
= 0
•
pH of Common Substances
Acidic
Neutral
Basic
More acidic
More basic
pH
NaOH, 0.1 M
Household bleach
Household ammonia
Lime water
Milk of magnesia
Borax
Baking soda
Egg white, seawater
Human blood, tears
Milk
Saliva
Rain
Black coffee
Banana
Tomatoes
Wine
Cola, vinegar
Lemon juice
Gastric juice
14
13
12
11
10
9
8
7
6
5
4
3
2
1
0
[H+]
1 x 10-14
1 x 10-13
1 x 10-12
1 x 10-11
1 x 10-10
1 x 10-9
1 x 10-8
1 x 10-7
1 x 10-6
1 x 10-5
1 x 10-4
1 x 10-3
1 x 10-2
1 x 10-1
1 x 100
[OH-]
1 x 10-0
1 x 10-1
1 x 10-2
1 x 10-3
1 x 10-4
1 x 10-5
1 x 10-6
1 x 10-7
1 x 10-8
1 x 10-9
1 x 10-10
1 x 10-11
1 x 10-12
1 x 10-13
1 x 10-14
pOH
0
1
2
3
4
5
6
7
8
9
10
11
12
13
14
Calculations and practice
• You will need to use the following:
pH = – log10[H+]
pOH = – log10[OH–]
pH + pOH = 14
pH Calculations
pH
pH = -log10[H+]
[H+]
[H+] = 10-pH
[H+] [OH-] = 1 x10-14
pH + pOH = 14
pOH
pOH = -log10[OH-]
[OH-]
[OH-] = 10-pOH
pH for Strong Acids
• Strong acids dissociate completely in
solution
• Strong bases also dissociate completely in
solution
pH Exercises
c) pH of solution where [H +]
a)pH of 0.02M HCl
is 7.2x10-8M
+
pH = – log10 [H ]
pH
= – log10 [H+]
= – log10 [0.020]
= – log10 [7.2x10-8]
= 1.6989
= 7.14
= 1.70
(slightly basic)
b)pH of 0.0050M NaOH
pOH = – log10 [OH–]
= – log10 [0.0050]
= 2.3
pH = 14 – pOH
= 14 – 2.3
=11.7
pH = - log [H+]
Given: pH = 4.6
pH = - log10 [H+]
choose proper equation
4.6 = - log10 [H+]
substitute pH value in equation
- 4.6 =
2nd
log
determine the [hydrogen ion]
- 4.6 =
log10[H+]
antilog [H+]
multiply both sides by -1
take antilog of both sides
[H+] = 2.51x10-5 M
10x
antilog
You can check your answer by working backwards.
pH = - log10[H+]
pH = - log10[2.51x10-5 M]
pH = 4.6
Most substances that are acidic in water are actually weak acids.
Because weak acids dissociate only partially in aqueous solution,
an equilibrium is formed between the acid and its ions.
The ionization equilibrium is given by:
HX(aq)
where X- is the conjugate base.
H+(aq) + X-(aq)
pH calculations for Weak Acids and Weak
Bases
For Weak Acids
pH = -Log10
For Weak Bases
pOH = Log10
pH =
14 - pOH
pH of solutions of weak concentrations
Weak Acid
pH of a 1M solution of ethanoic acid with a Ka
value of 1.8 x 10-5
pH = -Log10
pH = -Log10
pH = 2.3723
pH of solutions of weak concentrations
Weak Base
pH of a 0.2M solution of ammonia with a Kb value of
1.8 x 10-5
pOH = -log10
pOH = -log10
pOH = 2.7319
pH = 14 – 2.7319
Theory of Acid Base Indicators
Acid-base titration indicators are quite often weak
acids.
For the indicator HIn
The equilibrium can be simply expressed as
HIn(aq, colour 1)
H+(aq) + In-(aq, colour 2)
Theory of Acid Base Indicators
Applying Le Chatelier's equilibrium principle:
Addition of acid
•
favours the formation of more HIn (colour 1)
HIn(aq)
H+(aq) + In-(aq)
because an increase on the right of [H+]
causes a shift to left
increasing [HIn] (colour 1)
to minimise 'enforced' rise in [H+].
Theory of Acid Base Indicators
Applying Le Chatelier's equilibrium principle:
Addition of base
•
favours the formation of more In- (colour 2)
HIn(aq)
H+(aq) + In-(aq)
The increase in [OH-] causes a shift to right
because the reaction
H+(aq) + OH-(aq) ==> H2O(l)
Reducing the [H+] on the right
so more HIn ionises to replace the [H+]
and so increasing In- (colour 2)
to minimise 'enforced' rise in [OH-]
Theory of Acid Base Indicators
Acid-base titration indicators are also often weak
bases.
For the indicator MOH
The equilibrium can be simply expressed as
MOH(aq, colour 1)
OH-(aq) + M+(aq, colour 2)
Theory of Acid Base Indicators
Applying Le Chatelier's equilibrium principle:
Addition of base
•
favours the formation of more MOH (colour 1)
MOH(aq)
M+(aq) + OH-(aq)
because an increase on the right of [OH-]
causes a shift to left
increasing [MOH] (colour 1)
-
to minimise 'enforced' rise in [OH ].
Theory of Acid Base Indicators
Applying Le Chatelier's equilibrium principle:
Addition of acid
•
favours the formation of more M+ (colour 2)
MOH(aq)
M+(aq) + OH-(aq)
The increase in [H+] causes a shift to right
because the reaction
H+(aq) + OH-(aq) ==> H2O(l)
Reducing the [OH-] on the right
so more MOH ionises to replace the [OH-]
and so increasing M+ (colour 2)
to minimise 'enforced' rise in [H+]
Acid Base Titration Curves
Strong Acid – Strong Base
Weak Acid – Strong Base
Strong Acid – Weak Base
Weak Acid – Weak Base
Choice of Indicator for Titration
• Indicator must have a complete colour
change in the vertical part of the pH
titration curve
• Indicator must have a distinct colour
change
• Indicator must have a sharp colour change
Indicators for Strong Acid Strong Base Titration
Both phenolphthalein
and methyl orange
have a complete
colour change in the
vertical section of the
pH titration curve
Indicators for Strong Acid Weak Base Titration
Methyl Orange is
used as indicator for
this titration
Only methyl orange
has a complete
colour change in the
vertical section of the
pH titration curve
Phenolphthalein has
not a complete colour
change in the vertical
section on the pH
titration curve.
Indicators for Weak Acid Strong Base Titration
Phenolphthalein is
used as indicator for
this titration
Only phenolphthalein
has a complete
colour change in the
vertical section of the
pH titration curve
Methyl has not a
complete colour
change in the vertical
section on the pH
titration curve.
Indicators for Weak Acid Weak Base Titration
No indicator suitable
for this titration
because no vertical
section
Neither phenolphthalein
nor methyl orange have
completely change colour
in the vertical section on
the pH titration curve
indicator
pH range
litmus
5-8
methyl orange
3.1 - 4.4
phenolphthalein
8.3 - 10.0
Colour Changes and pH ranges
Methyl Orange
Phenolphthalein
Universal indicator components
Indicator
Low pH color
Transition pH range
High pH color
Thymol blue (first
transition)
red
1.2–2.8
orange
Methyl Orange
red
4.4–6.2
yellow
Bromothymol blue
yellow
6.0–7.6
blue
Thymol blue (second
transition)
yellow
8.0–9.6
blue
Phenolphthalein
colourless
8.3–10.0
purple