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Precipitation Titration
Precipitation Reactions
Precipitation is the formation of a solid in a solution
solid formed is called the precipitate
A precipitation reaction occurs when water solutions of two different
ionic compounds are mixed and an insoluble solid separates out of
solution.
KCl + AgNO3 AgCl + KNO3
The precipitate is itself ionic; the cation comes from one solution and
the anion from another.
Cl- solution Precipitating
agent
White
precipitate
Precipitation Titrations
• Precipitation titration is a titration method based on the formation of precipitate,
which is slightly soluble
• The basic requirements are:
• The reaction must be sufficiently rapid and complete, lead to a product of
reproducible composition and of low solubility.
• And a method must exist to locate the end point.
• Precipitation titrations are not so popular in present–day routine analysis. Why????
Some difficulties in meeting these requirements must be noted. (Precipitation
reactions are generally)
• Slow
• Involving periods of digestion, cooling, filtration etc.
• This tends to limit the reactions that are available for titration.
3
Argentometric titration:
• Titrations involving silver are termed argentometric, from the Latin name for
silver, argentum.
• The major precipitation reaction used is that of silver with a range of anions.
These anions include:
• Halides (Cl-, Br-, I-)
• Pseudohalides (S2-, HS-, CN-, SCN-)
• The reaction rates for the silver salt precipitation is rapid.
• The reaction ratio is 1:1 and silver salts formed are generally quite insoluble.
• Argentometric methods involving precipitation titrimetry:
• Mohr’s Method
• Fajan’s Method
• Volhard’s Method
4
Mohr’s Method:
• This direct method uses potassium chromate (chromate ions
(CrO4
2)) as an indicator in the titration of (Cl-, Br-, and CN- )ions
(analyte) with a silver nitrate standard solution (titrant).
• After all the chloride has been precipitated as white silver chloride,
the first excess of titrant results in the formation of a silver
chromate precipitate,
• which signals the end point (1). The reactions are:
Ag +(aq) + Cl - (aq) → AgCl(s) Ksp = 1.8 x 10–10
white precipitate
• End point determination by brick red color precipitate, Ag2CrO4(s):
2 Ag +(aq) + CrO4
2-(aq) → Ag2CrO4(s) Ksp = 1.2 x 10–12
• AgCl is less soluble than Ag2CrO4 so it will precipitate first
5
Conditions for Mohr’s method:
• The titrations are performed only in neutral or slightly basic medium to
prevent silver hydroxide formation (at pH > 10).
2Ag+ + 2OH- 2AgOH(s) Ag2O(s) + H2O
black precipitate
• Or the formation of chromic acid at pH < 7.
CrO42- + H3O+ HCrO4- + H2O
2 CrO42- + 2 H3O+ Cr2O7
2- + H2O
bright-orange
• Reducing [CrO42-] will delay the formation of the precipitate although more
Ag+ to be added to reach end point, which cause error.
6
• This method uses a back titration with potassium thiocyanate and is suitable for
the determination of chlorides, bromides and iodides in acidic solutions.
• First, Cl- is precipitated by excess AgNO3
• Removing AgCl(s) by filtration / washing
• Excess Ag+ is titrated with KSCN in the presence of Fe3+
• When Ag+ has been consumed, a red complex forms as a result of:
The Volhard titration can be used for any anion that forms an insoluble salt with
silver
Volhard method:
(s)
(aq)
(aq) AgCl
Cl
Ag -



(s)
(aq)
(aq) AgSCN
SCN
Ag -



(aq)
(aq)
(aq) 


 2
-
3
FeSCN
SCN
Fe
Red complex
•Conditions for Volhard’s method:
• The solution must be acidic, with a concentration of about 1 M in nitric
acid to ensure the complex formed is stable, and to prevent the
precipitation of Iron(III) as hydrated oxide.
• The indicator concentration should not be more than 0.2M.
• In case of I-, indicator should not be added until all the I- is precipitated
with Ag+, since it would be oxidized by the Fe(III).
2Fe3+ + 2I- 2Fe2+ + I2
The AgX ↓precipitate must be filtered off, before titrating with SCN- to
prevent any error, for example in the case of chloride ion, AgCl will react
with the titrant (SCN- ) and cause a diffuse end point.
AgCl + SCN- AgSCN + Cl-
OR
Use tartrazine as indicator instead of Iron(III) . 8
Fajan’s Method
• This method uses an adsorption indicator such of Fluorescein
(Dichlorofluorescein) and Eosin.
• The indicator adsorb onto the surface of the silver salt precipitate at the
endpoint.
• The adsorption process causes a change in the color of the indicator.
• Common Fajans adsorption indicators are weakly acidic organic
compounds and in alkaline conditions will exist as the conjugate base,(or
Ind-).
• This form of the indicator which interacts with the precipitate.
9
The mechanism of indicators action:
• The best–known adsorption indicator is fluorescein, which
is used to indicate the equivalence point in the titration of
Cl- with Ag+ . Fluorescein is a weak acid, which partially
dissociates in water to form fluoresceinate anion.
• The fluoresceinate anion has a yellow–green colour in
solution.
10
• When Cl- is titrated with Ag+ in the presence of fluorescein, the negatively
charged fluoresceinate anions are initially repelled by the negatively
charged AgCl colloidal particles, with their primary adsorption layer of Cl-
ions.
• Thus the fluorescein remains in a yellow–green colour prior to the
equivalence point.
• At the equivalence point, the colloidal AgCl particles undergo an abrupt
change from a negative charge to a positive charge by virtue of Ag+ ions
adsorbed in the primary adsorption layer.
• The fluoresceinate ions are strongly adsorbed in the counter–ion layer of
the AgCl colloids, giving these particles a red colour and providing an end
point colour change from yellow–green to red or pink.
11
• Adsorption indicator whose color when adsorbed to the precipitate is
different from that when it is in solution
12
Comparison of argentometric titration methods
Method Advantages Disadvantages
Mohr Simple
• Alkaline solution only
• Not suitable for I-
• Requires a blank
Volhard
• Capable for direct Ag+ and indirect halide
analyses
• Very clear colour change
• Must use 1M of nitric
acid solution
• Some problems with
some ions
Fajans
• Capability for different pH ranges and
selectivity with different indicators
• Difficult with dilute
solutions
• Should not be a high
background ionic level
Titration Curves for Argentometric Methods
Plots of titration curves are normally sigmoidal curves consisting of pAg (or pAnalyte)
versus volume of AgNO3 solution added.
Example: Titration of chloride with silver.
The points on the curve can be calculated, given the analyte concentration, AgNO3
concentration and the appropriate Ksp.
A useful relationship can be derived by taking
the negative logarithm of both sides of a
solubility-product expression. Thus, for silver
chloride,
𝐾𝑠𝑝 = 𝐴𝑔
+
[𝐶𝑙
−
]
𝑙𝑜𝑔𝐾𝑠𝑝 = −log( 𝐴𝑔
+
𝐶𝑙
−
)
𝑙𝑜𝑔𝐾𝑠𝑝 = − log 𝐴𝑔
+
− 𝑙𝑜𝑔 𝐶𝑙
−
𝑝𝐾𝑠𝑝 = 𝑝𝐴𝑔
+
+𝑝𝐶𝑙
−
• Consider titration of Cl- with a standard solution of AgNO3.
• Titration curve prepared by plotting pCl (-log[Cl-]) against the volume of AgNO3
in a manner similar to acid-base titration.
• Before titration started – only have Cl-.
pCl = - log[Cl-]
• Titration proceed – part of Cl- is removed from solution by precipitation as AgCl.
pCl = -log [remaining Cl-]
• At equivalence point - we have solution a saturated solution of AgCl.
[Cl-]= √Ksp
• Excess AgNO3 added – excess Ag+. [Cl-] is determine from the concentration of
Ag+ and Ksp.
[Cl-] = Ksp/[Ag+]
Plotting precipitation titration curves
Example
Calculate pCl for the titration of 100.0 ml 0.100 M NaCl with 0.100 M
AgNO3 for the addition of 0.0, 20.0, 99.0, 99.5, 100.0 and 110.0 ml AgNO3.
Ksp AgCl is 1.0 x10-10
Solution
a) Addition of 0.0 ml Ag+
[Cl-] = 0.100 M
pCl = -log [Cl-]
= -log 0.100
= 1
b) Addition of 20.0 ml Ag+
Initial mmol Cl- = 100.0 ml x 0.100 M = 10.0 mmol
mmol added Ag+ = 20.0 ml x 0.100 M = 2.0 mmol
mmol Cl- left = 8.0 mmol
[Cl-] left = 8.0 = 0.0667 M
(100+20) ml
pCl = -log [Cl-]
= -log 0.0667
= 1.18
c) Addition of 99.0 ml Ag d) Addition of 100.0 ml
Initial mmol Cl- = 100.0 ml x 0.100 M = 10.0 mmol
mmol added Ag+ = 100.0 ml x 0.100 M= 10.0 mmol
Equivalence point is reached. The solution contain
saturated AgCl solution
Ksp = [Ag+][Cl-] = 1.0 x10-10
[Cl-] = √Ksp = √1.0 x10-10
= 1.0 x 10-5
pCl = -log 1.0 x10-5
= 5
e) Addition of 100.5 ml Ag+
Initial mmol Cl = 100.0 ml x 0.100 M = 10.0 mmol
mmol added Ag+= 100.5 ml x 0.100 M =10.05 mmol
mmol Ag+ excess = = 0.05 mmol
[Ag+] excess = 0.05/200.5 ml = 2.5 x 10-4 M
Ksp = [Ag+][Cl-] = 1.0 x10-10
[Cl-] = Ksp = 1.0 x10-10 = 4.0 x 10-7
[Ag+] 2.5 x 10-4 M
pCl = - log 4.0 x 10-7
= 6.4

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Lecture 4 Analytical Chemistry.pdf

  • 2. Precipitation Reactions Precipitation is the formation of a solid in a solution solid formed is called the precipitate A precipitation reaction occurs when water solutions of two different ionic compounds are mixed and an insoluble solid separates out of solution. KCl + AgNO3 AgCl + KNO3 The precipitate is itself ionic; the cation comes from one solution and the anion from another. Cl- solution Precipitating agent White precipitate
  • 3. Precipitation Titrations • Precipitation titration is a titration method based on the formation of precipitate, which is slightly soluble • The basic requirements are: • The reaction must be sufficiently rapid and complete, lead to a product of reproducible composition and of low solubility. • And a method must exist to locate the end point. • Precipitation titrations are not so popular in present–day routine analysis. Why???? Some difficulties in meeting these requirements must be noted. (Precipitation reactions are generally) • Slow • Involving periods of digestion, cooling, filtration etc. • This tends to limit the reactions that are available for titration. 3
  • 4. Argentometric titration: • Titrations involving silver are termed argentometric, from the Latin name for silver, argentum. • The major precipitation reaction used is that of silver with a range of anions. These anions include: • Halides (Cl-, Br-, I-) • Pseudohalides (S2-, HS-, CN-, SCN-) • The reaction rates for the silver salt precipitation is rapid. • The reaction ratio is 1:1 and silver salts formed are generally quite insoluble. • Argentometric methods involving precipitation titrimetry: • Mohr’s Method • Fajan’s Method • Volhard’s Method 4
  • 5. Mohr’s Method: • This direct method uses potassium chromate (chromate ions (CrO4 2)) as an indicator in the titration of (Cl-, Br-, and CN- )ions (analyte) with a silver nitrate standard solution (titrant). • After all the chloride has been precipitated as white silver chloride, the first excess of titrant results in the formation of a silver chromate precipitate, • which signals the end point (1). The reactions are: Ag +(aq) + Cl - (aq) → AgCl(s) Ksp = 1.8 x 10–10 white precipitate • End point determination by brick red color precipitate, Ag2CrO4(s): 2 Ag +(aq) + CrO4 2-(aq) → Ag2CrO4(s) Ksp = 1.2 x 10–12 • AgCl is less soluble than Ag2CrO4 so it will precipitate first 5
  • 6. Conditions for Mohr’s method: • The titrations are performed only in neutral or slightly basic medium to prevent silver hydroxide formation (at pH > 10). 2Ag+ + 2OH- 2AgOH(s) Ag2O(s) + H2O black precipitate • Or the formation of chromic acid at pH < 7. CrO42- + H3O+ HCrO4- + H2O 2 CrO42- + 2 H3O+ Cr2O7 2- + H2O bright-orange • Reducing [CrO42-] will delay the formation of the precipitate although more Ag+ to be added to reach end point, which cause error. 6
  • 7. • This method uses a back titration with potassium thiocyanate and is suitable for the determination of chlorides, bromides and iodides in acidic solutions. • First, Cl- is precipitated by excess AgNO3 • Removing AgCl(s) by filtration / washing • Excess Ag+ is titrated with KSCN in the presence of Fe3+ • When Ag+ has been consumed, a red complex forms as a result of: The Volhard titration can be used for any anion that forms an insoluble salt with silver Volhard method: (s) (aq) (aq) AgCl Cl Ag -    (s) (aq) (aq) AgSCN SCN Ag -    (aq) (aq) (aq)     2 - 3 FeSCN SCN Fe Red complex
  • 8. •Conditions for Volhard’s method: • The solution must be acidic, with a concentration of about 1 M in nitric acid to ensure the complex formed is stable, and to prevent the precipitation of Iron(III) as hydrated oxide. • The indicator concentration should not be more than 0.2M. • In case of I-, indicator should not be added until all the I- is precipitated with Ag+, since it would be oxidized by the Fe(III). 2Fe3+ + 2I- 2Fe2+ + I2 The AgX ↓precipitate must be filtered off, before titrating with SCN- to prevent any error, for example in the case of chloride ion, AgCl will react with the titrant (SCN- ) and cause a diffuse end point. AgCl + SCN- AgSCN + Cl- OR Use tartrazine as indicator instead of Iron(III) . 8
  • 9. Fajan’s Method • This method uses an adsorption indicator such of Fluorescein (Dichlorofluorescein) and Eosin. • The indicator adsorb onto the surface of the silver salt precipitate at the endpoint. • The adsorption process causes a change in the color of the indicator. • Common Fajans adsorption indicators are weakly acidic organic compounds and in alkaline conditions will exist as the conjugate base,(or Ind-). • This form of the indicator which interacts with the precipitate. 9
  • 10. The mechanism of indicators action: • The best–known adsorption indicator is fluorescein, which is used to indicate the equivalence point in the titration of Cl- with Ag+ . Fluorescein is a weak acid, which partially dissociates in water to form fluoresceinate anion. • The fluoresceinate anion has a yellow–green colour in solution. 10
  • 11. • When Cl- is titrated with Ag+ in the presence of fluorescein, the negatively charged fluoresceinate anions are initially repelled by the negatively charged AgCl colloidal particles, with their primary adsorption layer of Cl- ions. • Thus the fluorescein remains in a yellow–green colour prior to the equivalence point. • At the equivalence point, the colloidal AgCl particles undergo an abrupt change from a negative charge to a positive charge by virtue of Ag+ ions adsorbed in the primary adsorption layer. • The fluoresceinate ions are strongly adsorbed in the counter–ion layer of the AgCl colloids, giving these particles a red colour and providing an end point colour change from yellow–green to red or pink. 11
  • 12. • Adsorption indicator whose color when adsorbed to the precipitate is different from that when it is in solution 12
  • 13. Comparison of argentometric titration methods Method Advantages Disadvantages Mohr Simple • Alkaline solution only • Not suitable for I- • Requires a blank Volhard • Capable for direct Ag+ and indirect halide analyses • Very clear colour change • Must use 1M of nitric acid solution • Some problems with some ions Fajans • Capability for different pH ranges and selectivity with different indicators • Difficult with dilute solutions • Should not be a high background ionic level
  • 14. Titration Curves for Argentometric Methods Plots of titration curves are normally sigmoidal curves consisting of pAg (or pAnalyte) versus volume of AgNO3 solution added. Example: Titration of chloride with silver. The points on the curve can be calculated, given the analyte concentration, AgNO3 concentration and the appropriate Ksp. A useful relationship can be derived by taking the negative logarithm of both sides of a solubility-product expression. Thus, for silver chloride, 𝐾𝑠𝑝 = 𝐴𝑔 + [𝐶𝑙 − ] 𝑙𝑜𝑔𝐾𝑠𝑝 = −log( 𝐴𝑔 + 𝐶𝑙 − ) 𝑙𝑜𝑔𝐾𝑠𝑝 = − log 𝐴𝑔 + − 𝑙𝑜𝑔 𝐶𝑙 − 𝑝𝐾𝑠𝑝 = 𝑝𝐴𝑔 + +𝑝𝐶𝑙 −
  • 15. • Consider titration of Cl- with a standard solution of AgNO3. • Titration curve prepared by plotting pCl (-log[Cl-]) against the volume of AgNO3 in a manner similar to acid-base titration. • Before titration started – only have Cl-. pCl = - log[Cl-] • Titration proceed – part of Cl- is removed from solution by precipitation as AgCl. pCl = -log [remaining Cl-] • At equivalence point - we have solution a saturated solution of AgCl. [Cl-]= √Ksp • Excess AgNO3 added – excess Ag+. [Cl-] is determine from the concentration of Ag+ and Ksp. [Cl-] = Ksp/[Ag+] Plotting precipitation titration curves
  • 16. Example Calculate pCl for the titration of 100.0 ml 0.100 M NaCl with 0.100 M AgNO3 for the addition of 0.0, 20.0, 99.0, 99.5, 100.0 and 110.0 ml AgNO3. Ksp AgCl is 1.0 x10-10 Solution a) Addition of 0.0 ml Ag+ [Cl-] = 0.100 M pCl = -log [Cl-] = -log 0.100 = 1 b) Addition of 20.0 ml Ag+ Initial mmol Cl- = 100.0 ml x 0.100 M = 10.0 mmol mmol added Ag+ = 20.0 ml x 0.100 M = 2.0 mmol mmol Cl- left = 8.0 mmol [Cl-] left = 8.0 = 0.0667 M (100+20) ml pCl = -log [Cl-] = -log 0.0667 = 1.18
  • 17. c) Addition of 99.0 ml Ag d) Addition of 100.0 ml Initial mmol Cl- = 100.0 ml x 0.100 M = 10.0 mmol mmol added Ag+ = 100.0 ml x 0.100 M= 10.0 mmol Equivalence point is reached. The solution contain saturated AgCl solution Ksp = [Ag+][Cl-] = 1.0 x10-10 [Cl-] = √Ksp = √1.0 x10-10 = 1.0 x 10-5 pCl = -log 1.0 x10-5 = 5
  • 18. e) Addition of 100.5 ml Ag+ Initial mmol Cl = 100.0 ml x 0.100 M = 10.0 mmol mmol added Ag+= 100.5 ml x 0.100 M =10.05 mmol mmol Ag+ excess = = 0.05 mmol [Ag+] excess = 0.05/200.5 ml = 2.5 x 10-4 M Ksp = [Ag+][Cl-] = 1.0 x10-10 [Cl-] = Ksp = 1.0 x10-10 = 4.0 x 10-7 [Ag+] 2.5 x 10-4 M pCl = - log 4.0 x 10-7 = 6.4