w3 Flashcards

1
Q

Common Ion Effect

A

occurs when the ionisation of an acid (or base) is limited by the presence of a significant concentration of its conjugate base (or acid)

The addition of sodium acetate pushes the equilibrium to the left, creating
acetic acid and raising the pH (sodium does not effect pH).
– Before adding a common ion, the equilibrium condition Q = Ka is satisfied.
– After adding a common ion, Q > Ka
– Restoration of equilibrium would be achieved by net reaction in the direction that reduces Q.
The presence of conjugate base limits ionisation of the acid

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2
Q

Controlling pH: Buffer Solutions

A
  • The pH meter indicates the pH of water that contains a trace of acid, as well as some bromophenol blue acid-base indicator. (pH = 5.04)
  • The solution at left is a buffer
    solution with a pH of about 7,
    also with the indicator.
  • 5 mL of 0.1 mol L- 1 HCl is
    added to each solution
  • The pH of the water drops by
    several units (pH = 2.33) also
    shown by the indicator colour
    change).
  • The unchanged indicator
    colour indicates the pH of the
    buffer solution hardly changes.
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3
Q

Composition and Mode of Operation of Buffers

A
  • Minimize the change in pH when a strong acid or base is added.
  • Contain large amounts of both a weak acid and its conjugate base, relative to the amounts of acid or base that are added.
  • Function because the weak acid and base are in equilibrium:
    – Added H3O+ (aq) ions are “mopped up” by the conjugate base
    – Added OH- (aq) ions are “mopped up”’ by the weak acid.
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4
Q

Commonly used buffering reagents

A

phthalic acid - hydrogenphthalate ion, 1.3x10-3 (2.89), 1.9-3.9

acetic acid, acetate ion, 1,8x10-5 (4.74), 3.7-5.8

hydrogenphosphate ion, phosphate ion, 3.6x10-13 (12.44), 11.3-13.3

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5
Q

Quantitative Calculations of Buffer
Solution pH

A

[H3O+] = [HA]/[A-] x Ka

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6
Q

Henderson-Hasselbalch equation (Log form):

A

pH = pKa + log10 [A-]/[HA] (conjugate base/acid)

determined largely by the pKa of the acid - adjusted by the ratio acid:conjugate base

actual concentrations of [acid] and [conjugate base] are not important, but the molar ratio is.

Diluting a buffer solution does not change its pH

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7
Q

Design of a Buffer Solution of Specified pH

A

To design a buffer solution for a particular pH, choose a weak acid with pKa within 1 unit of the target pH.

  • Calculate the [weak acid]/[conjugate base] ratio that will adjust the solution pH to the target value.
  • Make a solution containing both the weak acid and its conjugate base with the appropriate ratio.
  • Use amounts of the weak acid and conjugate base well in excess of the amounts of strong acid or base that are likely to be added.

(Henderson-Hasselbalch equation)

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8
Q

pH Change of Buffer Solutions

A

To calculate how much pH changes on addition of a specified amount of H3O+
(aq) to a buffer solution, calculate

a) the amounts of weak acid and conjugate base in the buffer solution,
b) the amount of H3O+ (aq) added
c) the amount of acid that reacts and base that is formed,
d) the new ratio n(acid)/n(base), and
e) the new pH using the above ratio, and Ka of HA(aq).

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9
Q

Buffer Capacity

A

the ability of a buffer solution to minimize pH change upon addition of strong acids or bases.

  • The more concentrated the weak acid and base are in a solution, the higher the buffer capacity, and:

(a) for a given amount of added strong acid or base, the less is the pH change;
(b) the more strong acid or base can be added before the solution loses its effectiveness.

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10
Q

Acid-Base Titrations

A

a method of quantitative analysis, based on a reaction of known stoichiometry. It depends on finding the volume of a solution containing the amount of acid (or base) that reacts exactly with a known amount of base (or acid).

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11
Q

The Equivalence point

A
  • Occurs when acid or base has been titrated with an equivalent amount of the corresponding species

– For strong acid and base this results in a neutral solution at a pH of 7.0
– For other combinations, the pH at equivalence is not 7
* Strong acid + weak base, pH < 7
* Strong base + weak acid, pH > 7

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12
Q

Strong Acid- strong base (HCL and NaOH titration

A

Initially the solution is 0.1M HCl so pH=1.
* As NaOH is added the amount of HCl
decreases;
* that which remains is in an ever
increasing volume; the pH slowly increases.
* Just before the equivalence point the
solution is still quite acidic e.g. at 49
mls pH=3.
* The equivalence point in any titration is the midpoint of the vertical section.
* In this case the pH rises very rapidly
around the midpoint: 8 pH units
between 49 and 50 mls (8 orders of magnitude)

At the equivalence point in titration of a solution of a strong base into a solution of a strong acid, pH = 7.0.

  • The pH at any point prior to the
    equivalence point can be calculated
    from the amount of unreacted acid.
  • Immediately after the equivalence point the addition of a very small amount of base causes a dramatic increase in pH:
    essentially adding a strong base to
    water.
  • After a bit more base has been added, the rate of increase decreases.
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13
Q

Weak Acid- Strong base (Acetic acid and NaOH

A
  • The initial pH is found from the [acid] and the acid pKa
  • At the equivalence point the acetic acid and NaOH have been consumed.
    – pH is controlled by the acetate ion (conjugate base)
  • At the ½ equivalence point ½ of the acid has been neutralised.
    – [CH3COOH]=[CH3COO-]
    (CH3COO-Na+ 100% dissociates)
  • Because:

[H3O+] = [HA]/[A-] x Ka

at the half equivalence point pH=pKa
i.e. we have worked out the acid pKa
* The slow change in pH between 0 and 90 mls is because the solution is buffered, known as the buffer region.
* Above equiv. point pH rises sharply as before

pH > 7 at the equivalence point
for a weak acid with a strong
base. The pH can be calculated
using Kb of the conjugate base.

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14
Q

Polyprotic weak acids and strong base (H2C2O4 and NaOH)

A
  • The initial pH comes from the acid
    concentration and pKa1.
  • The first rise occurs at about 100mls
    – the first H has been titrated.
    – HC2O4
  • controls the pH
    (conjugate base)
  • When the 2nd H is titrated the pH again rises, this time more sharply
    – C2O4 2- controls the pH
    (conjugate base)

C2O42- + H20 → HC2O4- + OH
Kb = 1.6 x 10-10
Therefore pH = 8.5

Kb =Kw/Ka

In diprotic weak acid with Ka1&raquo_space; Ka2 titration, the most acidic proton is removed from nearly all molecules before the second one is removed.

  • Prior to the first equivalence point, the solution is a buffer solution, and when the volume of NaOH solution is
    exactly half that needed to
    reach the first equivalence point, pH = pKa1.

Between the first and second equivalence points, the solution is a buffer solution, and when the volume added is midway between the first and
second equivalence points, pH = pKa2.

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15
Q

Weak Base - Strong Acid (NH3 and HCl)

A
  • The initial pH is a function of the base
    concentration and its pKa (or pKb)
  • At the half equivalence point half of the NH3 has been converted to NH4+Cl-

– Therefore [NH4+] = [NH4+Cl-]
* As (Henderson-Hasselbalch equation)

at this concentration pH = pKa
* As more HCl is added the pH falls slowlydue to the buffer effect.
* At the equivalence point, the pH of the solution is due to the weakly acidic NH4+(aq) ions, and the pH is about 5.
* As more HCl is added NH4+Cl- is formed and the pH falls do to the dissociation of NH4+

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16
Q

Biochemical Acid-Base Speciation

A
  • Maintenance of pH in cellular fluids of living organisms is vital, because enzyme activity is influenced by pH.
  • The main protection against harmful
    pH changes in cells is provided by buffers.
  • In most cells, the pH is maintained
    between 6.9 and 7.4 through the
    action of phosphate (H2PO4-/HPO4 2-)
    and carbonate (H2CO3/HCO3-) buffers.
  • Just as increasing CO2(g) in the
    atmosphere causes acidification of sea water, increased CO2 (g) concentration
    in the lungs can affect blood pH.
17
Q

Colligative Properties

A

When water contains dissolved substances, the properties of the solution are affected:
– Equilibrium vapour pressure
– Boiling point
– Freezing point
– Osmotic pressure

depend only on the conc of solute particles and are independent of the identity of the particles in solution.

18
Q

Lowering of vapour pressure by non-volatile solutes

A
  • is the pressure of the vapour above it
  • when the liquid and the vapour are in equilibrium.

If we form a solution by dissolving a nonvolatile solute, the equilibrium vapour pressure of the solvent above the solution is lower than for the pure solvent.

For an ideal solution, the vapour pressure of the solvent is proportional to the mole fraction of solvent (x) at a specified temperature (Raoult’s law).

19
Q

Raoult’s law

A

p(solvent) = x(solvent) × p°
solvent

a good approximation at
low solute concentration, and in solutions where solute and solvent are similar, e.g. octane and octanol.

20
Q

An ideal solution…

A

a good approximation at
low solute concentration, and in solutions where solute and solvent are similar, e.g. octane and octanol.

21
Q

Lowering of vapour pressure by non-volatile solutes

A

Vapour pressure: determined only by volatile solvent

In 1:1 solvent:solute solution, surface is covered equally by the solvent and
non-volatile solute.

This means the number of solvent molecules able to escape the liquid and contribute to the vapour pressure is reduced.

This lowers the vapour pressure. The reduction is calculated using Raoults Law.

The decrease depends on the quantity of the non-volatile solvent, not its nature.

22
Q

Freezing Point Depression is

A

lower than that of the pure solvent.

  • At low solute concentrations, the difference between the freezing point of solvent and that of solution is directly proportional to the molality (m-solute) of the solution:
    ∆ Tf = Kf × m(solute)
23
Q

Kf (in kg mol-1)

A

molal freezing point depression constant - the characteristic of the solvent.

24
Q

Fractional crystallization

A

As more ice forms, the solute conc in the residual solution increases, and the freezing point falls lower.

Cooling is stopped before freezing and residual solution is run off. Process is repeated to purify.

25
Q

Solutions of Electrolytes

A

Colligative properties depend only on the concentration of solute particles, not their identity

When the solute is an electrolyte, the freezing point depression depends on the total concentration of ions in solution.

26
Q

van’t Hoff factor

A

∆ Tf (measured)/∆ Tf (calculated) = ∆ Tf (measured) / Kf x m

∆ Tf = Kf x m x i

  • approaches whole numbers (2, 3, and so on) only with very dilute solutions.

In more concentrated solutions, the experimental freezing point depressions tell us that the solutions behave as if there are fewer ions in solution than expected.

Attributed to: ion attractions in solutions. If some of the positive and negative ions are paired, decreasing the total concentration of particles.
Ion pairing reduces particle conc, so the freezing point depression is less than expected number of moles of ions .

27
Q

Determinants of van’t Hoff

A

– Ionization of the solute
– The effective concentration of the solute (or Activity, a, which accounts for ion pairing). The activity is different from the labelled concentration.

28
Q

Osmosis

A

the movement of solvent molecules through a semipermeable membrane from a solution of lower solute conc (or pure solvent) to a solution of higher solute concentration.

29
Q

Osmotic Pressure

A

the pressure that must be applied against the spontaneous direction of osmosis just sufficient to prevent osmotic flow.

For dilute solutions, the osmotic
pressure is related to the molar
concentration by the temperature
and the gas constant:

Π = cRT

30
Q

Determine Molecular Weight from Osmosis

A

Strategy
Calculate the solution concentration from its osmotic pressure. Then, use the volume and concentration of the solution to calculate the amount of solute.
Finally, find the molar mass of the solute from its mass and amount.

31
Q

Osmotic Pressures of Solutions of Electrolytes

A

Osmotic pressures depend on the total activities of ions in solution, rather than the labelled solute concentration.

Π = i × cRT
where c is the solution labelled concentration and i is the van’t Hoff factor.

The van’t Hoff factor
corrects for things like
ion pairing.

32
Q

Reverse Osmosis in Water Purification

A

Applying sufficient pressure can overcome the natural osmotic
flow across a semipermeable
membrane.

33
Q

Osmosis in biological systems

A

a) A cell placed in an isotonic solution would have zero net movement of water into and out of the cell because the solute concentration inside and outside the cell is equal.

b) In a hypertonic solution, the solute concentration outside the cell is greater than inside. There is a net flow of water out of the cell, causing the cell to shrivel (crenate).

c) In a hypotonic solution, the solute concentration outside the cell is less than inside. There is a net flow of water
into the cell, causing the cell to swell and perhaps burst (or lyse).

34
Q

Speciation and Plots

A

the distribution between
any weak acid-conjugate base pair as pH is changed.
* The generalized equation for weak acid–conjugate base equilibrium:
HA(aq) + H2O(ℓ) ⇌ A- (aq) + H3O- (aq)

35
Q

A zwitterion…

A

The isoelectric pH for an amino acid is the pH at which the species has a site with positive charge and a site with a negative charge, but zero overall charge