Multiple choice, drill bank
From the lesson bank: excess reagent drives precipitation to completion; Step 1 uses MM of precipitate; desiccator cools without absorbing moisture; AgCl mole ratio 1:1; very low Ksp of BaSO₄ ensures complete precipitation.
Short answer model answers
Q1 (5 marks):
(a) m(BaSO₄) = 1.5566 − 1.1234 = 0.4332 g
(b) n(BaSO₄) = 0.4332 ÷ 233.39 = 1.857 × 10⁻³ mol = n(SO₄²⁻) (1:1)
(c) c(SO₄²⁻) = 1.857 × 10⁻³ ÷ 0.250 = 7.43 × 10⁻³ mol L⁻¹
Q2 (5 marks): Add excess AgNO₃(aq) to the 500 mL tap water sample and stir. The precipitate formed is AgCl(s), a white, insoluble solid, via: Ag⁺(aq) + Cl⁻(aq) → AgCl(s). Excess AgNO₃ is used to ensure all Cl⁻ ions react and are converted to precipitate, driving the reaction to completion. Filter the precipitate through a pre-weighed filter paper, washing with distilled water to remove soluble impurities. Dry the precipitate in an oven at ~100°C and cool in a desiccator. The precipitate must be completely dry before weighing because any remaining water would add mass to the measurement, causing the calculated Cl⁻ content to be overestimated. Weigh the dry precipitate and subtract the filter paper mass to get m(AgCl), then calculate: n(AgCl) = m ÷ 143.32; n(Cl⁻) = n(AgCl); m(Cl⁻) = n × 35.453.
Q3 (6 marks):
MM(AgCl) = 107.87 + 35.453 = 143.32 g mol⁻¹ [1]
n(AgCl) = n(Cl⁻) = 2.3145 ÷ 143.32 = 0.016148 mol [1]
Let x = mass of NaCl, then (1.000 − x) = mass of KCl [1]
n(Cl⁻) from NaCl = x ÷ 58.443; n(Cl⁻) from KCl = (1.000 − x) ÷ 74.551 [1]
x ÷ 58.443 + (1.000 − x) ÷ 74.551 = 0.016148
0.017110x + 0.013413(1.000 − x) = 0.016148
0.003697x = 0.002735 → x = 0.7398 g NaCl [1]
% NaCl = (0.7398 ÷ 1.000) × 100 = 74.0% [1]
Q4 (5 marks): The CO₂ explanation is plausible [1]. In acidic or neutral solution, CO₂ would not react significantly with Ba²⁺ (BaCO₃ Ksp ≈ 5.1 × 10⁻⁹, slightly soluble). However, if the solution became basic over time, BaCO₃ could co-precipitate with BaSO₄ [1]. Another plausible explanation: over 24 hours, the BaSO₄ particles could adsorb impurities from solution onto their surface (adsorption), adding mass without extra SO₄²⁻ [1]. A third explanation: incomplete drying, water trapped in the precipitate mass is also a possibility if drying was not repeated to constant mass [1]. Overall, the student should filter promptly and dry to constant mass to avoid these errors [1].
Q5 (7 marks):
Step 1: Weigh ~1 g of iron ore sample accurately on an analytical balance. Record mass m₁ [1].
Step 2: Dissolve in excess dilute HCl, heating gently. Filter to remove insoluble silica. The filtrate contains Fe³⁺(aq) [1].
Step 3: Add dilute NH₃ solution dropwise until pH ≈ 9 to precipitate Fe(OH)₃(s): Fe³⁺ + 3OH⁻ → Fe(OH)₃(s) [1].
Step 4: Filter through a pre-weighed crucible. Ignite in muffle furnace at 800°C: 2Fe(OH)₃ → Fe₂O₃ + 3H₂O. Cool in desiccator and weigh. Repeat to constant mass [1].
Calculation: n(Fe₂O₃) = m(Fe₂O₃) ÷ 159.69 [1]. n(Fe) = 2 × n(Fe₂O₃) [1]. m(Fe) = n(Fe) × 55.845. % Fe = (m(Fe) ÷ m₁) × 100 [1].