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From Gravimetry to Precipitation Titrimetry
Precipitation gravimetry: form a precipitate and weigh the solid to determine the analyte.
Precipitation titrimetry: measure the volume of titrant needed to react with the analyte and form a precipitate.
Same precipitation chemistry, but a different measurement:
Gravimetry → mass of precipitate
Precipitation titration → volume of titrant
A standard solution (titrant) of known concentration is added from a burette to the unknown solution.
Titrant is added until the endpoint is reached.
Endpoint can be detected by an indicator or coloured precipitate.
Precipitation titrations need a precipitate that forms quickly enough for practical analysis.
Precipitation titrimetry is faster and better for routine analysis, while gravimetry is very accurate but more time-consuming. Week 5 Precipitation Titrimetry…
Example: chloride + AgNO₃
\[ AgNO_3 \rightarrow Ag^+ + NO_3^- \]\[ \boxed{Ag^+ + Cl^- \rightarrow AgCl(s)} \]
Ag⁺ reacts with Cl⁻ to make the AgCl precipitate.
NO₃⁻ is a spectator ion.
Ag⁺ : Cl⁻ is 1:1, so moles Ag⁺ needed to react with all Cl⁻ = original moles Cl⁻.
🧠 Memory line
Gravimetry = weigh the precipitate ⚖
Precipitation titrimetry = measure titrant volume 🧪
Effects of Acidity on the Solubility of Precipitates
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Alpha Fractions (\(\alpha\))
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Effects of Acidity on the Solubility of Precipitates — Notes
Effects of Acidity on the Solubility of Precipitates — Notes
Calcium oxalate (CaC₂O₄) is sparingly soluble, meaning only a small amount dissolves in water.
When it dissolves, it separates into calcium ions (Ca²⁺) and oxalate ions (C₂O₄²⁻).
Ksp = 2.6 × 10⁻⁹ describes the solubility equilibrium.
Adding a strong acid increases H⁺ concentration and lowers the pH.
H⁺ attaches to free oxalate, converting it first into HC₂O₄⁻ and then H₂C₂O₄.
This reduces the amount of free oxalate in solution, causing more calcium oxalate solid to dissolve to restore equilibrium.
Three Forms of Oxalate
H₂C₂O₄: Has two H⁺ attached (α₀).
HC₂O₄⁻: Has one H⁺ attached (α₁).
C₂O₄²⁻: Has no H⁺ attached (α₂).
OxT represents the total concentration of all three oxalate forms.
Alpha (α) represents the fraction of total oxalate present in each form.
All three fractions add up to 1.
Effect of pH
Low pH: More H⁺, less free oxalate, and greater calcium oxalate solubility.
High pH: Less H⁺, more free oxalate, and lower calcium oxalate solubility.
Remember: Lower pH → More H⁺ → Less free oxalate → More solid dissolves.
Effects of Acidity on the Solubility of Precipitates — Notes
Solubility (s) is the total amount of calcium oxalate that dissolves in water.
When CaC₂O₄ dissolves, it releases equal amounts of calcium and oxalate, so s = [Ca²⁺] = OxT.
OxT represents the total concentration of all three dissolved oxalate forms (H₂C₂O₄, HC₂O₄⁻, and C₂O₄²⁻).
α₂ represents the fraction of total oxalate that is free C₂O₄²⁻.
To find the concentration of free oxalate, multiply OxT by α₂.
The Ksp expression only includes free calcium and free oxalate ions, so we replace the free oxalate concentration with OxT × α₂.
Ka₁ and Ka₂ are acid dissociation constants that help determine how much oxalate is in its free form at a certain pH.
The conditional solubility product (K′sp) accounts for how acidity affects solubility.
When pH decreases, more H⁺ attaches to oxalate, reducing the amount of free oxalate and making α₂ smaller.
As α₂ decreases, K′sp increases, meaning more calcium oxalate can dissolve.
Effects of Complexation on the Solubility of Precipitates.
Complexation occurs when a ligand attaches to a metal ion, forming a complex.
Complexing agents compete for free metal ions, while acids can react with anions.
AgBr dissolves slightly, releasing Ag⁺ and Br⁻.
When NH₃ is added, it binds to Ag⁺ and forms silver-ammonia complexes.
This decreases free Ag⁺, causing more AgBr to dissolve to restore equilibrium.
AgT represents the total concentration of dissolved silver in all forms.
αM represents the fraction of total silver present as free Ag⁺.
The Ksp expression can be rewritten using AgT and αM to account for complexation.
Remember: More ligand → Less free metal ion → More precipitate dissolves.
Conditional Solubility Product (AgBr + NH₃)
Solubility (s) = the amount of AgBr solid that dissolves in water.
When AgBr dissolves, it releases equal amounts of Ag⁺ and Br⁻.
AgT = total dissolved silver, including free Ag⁺ and silver attached to NH₃.
Therefore, s = [Br⁻] = AgT.
αM = the fraction of total dissolved silver that is free Ag⁺.
Formula: αM = [Ag⁺] / AgT.
Ksp only includes free Ag⁺, not silver attached to NH₃.
Original formula: Ksp = [Ag⁺][Br⁻].
With complexation: Ksp = AgT × αM × [Br⁻].
Conditional Ksp (K′sp) accounts for the effect of ammonia on solubility.
Formula: K′sp = Ksp / αM = s².
More NH₃ → less free Ag⁺ → smaller αM → larger K′sp → more AgBr dissolves.