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How can redox titrations measure the concentration of oxidising or reducing species in a sample?

Use redox titrations, including permanganate titrations, to determine the concentration of an analyte from balanced half-equations and stoichiometry.

Permanganate and iodine/thiosulfate redox titrations: combining half-equations to find the mole ratio, self-indicating endpoints, and fully worked SACE-style calculations from titre to analyte concentration.

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  1. What this dot point is asking
  2. Lead worked calculation
  3. Self-indicating endpoints
  4. Building the overall equation
  5. Iodine/thiosulfate (iodometric) titrations
  6. Why it matters for monitoring

What this dot point is asking

SACE expects you to construct the balanced overall equation from half-equations, read off the correct (often non 1:11:1) ratio, and complete the stoichiometric calculation, including multi-step iodine/thiosulfate analyses.

Lead worked calculation

Self-indicating endpoints

Potassium permanganate is its own indicator. MnO4\text{MnO}_4^- is intensely purple, while the product Mn2+\text{Mn}^{2+} is almost colourless. While reductant remains, each drop is decolourised; at the endpoint the first tiny excess of MnO4\text{MnO}_4^- gives the solution a faint permanent pink. No separate indicator is needed. Iodine titrations are nearly self-indicating (the brown I2\text{I}_2 fades), but a starch indicator is added near the endpoint to give a sharp blue-black to colourless change.

Building the overall equation

The crux of redox titration calculations is the ratio, which is rarely 1:11:1.

  1. Write each half-equation with its electrons.
  2. Multiply each so the electrons lost equal the electrons gained.
  3. Add and cancel electrons, H+\text{H}^+ and H2O\text{H}_2\text{O} where possible.
  4. Read the mole ratio of analyte to titrant directly from the coefficients.

Common ratios to know: MnO4:Fe2+=1:5\text{MnO}_4^- : \text{Fe}^{2+} = 1:5; MnO4:C2O42=2:5\text{MnO}_4^- : \text{C}_2\text{O}_4^{2-} = 2:5; Cr2O72:Fe2+=1:6\text{Cr}_2\text{O}_7^{2-} : \text{Fe}^{2+} = 1:6; I2:S2O32=1:2\text{I}_2 : \text{S}_2\text{O}_3^{2-} = 1:2.

Iodine/thiosulfate (iodometric) titrations

Many oxidisers are measured indirectly. The oxidiser first liberates iodine from excess iodide (oxidiser+II2\text{oxidiser} + \text{I}^- \rightarrow \text{I}_2), and the liberated I2\text{I}_2 is then titrated with standard thiosulfate. Because two steps are chained, you must apply two ratios in sequence, as in the dissolved-oxygen example above. This indirect approach lets a single standard (thiosulfate) measure many different oxidising analytes.

Why it matters for monitoring

Redox titrations quantify species that acid-base methods cannot, such as dissolved oxygen, chemical oxygen demand, iron content in water and ores, and the concentration of disinfectants. The Winkler dissolved-oxygen analysis and permanganate-based oxygen-demand tests are standard tools in environmental water monitoring.

Exam-style practice questions

Practice questions written in the style of SACE Board exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.

SACE 20225 marksA 25.00 mL25.00\ \text{mL} sample of a solution containing iron(II) ions was acidified and titrated with 0.0200 mol L10.0200\ \text{mol L}^{-1} potassium permanganate. The average titre was 21.30 mL21.30\ \text{mL}. The reaction is MnO4+5Fe2++8H+Mn2++5Fe3++4H2O\text{MnO}_4^- + 5\text{Fe}^{2+} + 8\text{H}^+ \rightarrow \text{Mn}^{2+} + 5\text{Fe}^{3+} + 4\text{H}_2\text{O}. Calculate the concentration of Fe2+\text{Fe}^{2+} in the sample.
Show worked answer →

Step 1: n(MnO4)=cV=0.0200×0.02130=4.260×104 moln(\text{MnO}_4^-) = cV = 0.0200 \times 0.02130 = 4.260 \times 10^{-4}\ \text{mol}. (1 mark)

Step 2: the equation gives a 1:51:5 ratio of MnO4\text{MnO}_4^- to Fe2+\text{Fe}^{2+}, so n(Fe2+)=5×4.260×104=2.130×103 moln(\text{Fe}^{2+}) = 5 \times 4.260 \times 10^{-4} = 2.130 \times 10^{-3}\ \text{mol}. (2 marks)

Step 3: c(Fe2+)=nV=2.130×1030.02500=0.0852 mol L1c(\text{Fe}^{2+}) = \dfrac{n}{V} = \dfrac{2.130 \times 10^{-3}}{0.02500} = 0.0852\ \text{mol L}^{-1}. (2 marks)

SACE 20205 marksThe dissolved oxygen in a water sample was measured by a Winkler-type method in which the liberated iodine was titrated with sodium thiosulfate: I2+2S2O322I+S4O62\text{I}_2 + 2\text{S}_2\text{O}_3^{2-} \rightarrow 2\text{I}^- + \text{S}_4\text{O}_6^{2-}. A 50.0 mL50.0\ \text{mL} sample required 8.40 mL8.40\ \text{mL} of 0.0100 mol L10.0100\ \text{mol L}^{-1} thiosulfate. Given that O2+4I+4H+2I2+2H2O\text{O}_2 + 4\text{I}^- + 4\text{H}^+ \rightarrow 2\text{I}_2 + 2\text{H}_2\text{O}, calculate the concentration of dissolved oxygen in mol L1\text{mol L}^{-1}.
Show worked answer →

Step 1: n(S2O32)=0.0100×0.00840=8.40×105 moln(\text{S}_2\text{O}_3^{2-}) = 0.0100 \times 0.00840 = 8.40 \times 10^{-5}\ \text{mol}. (1 mark)

Step 2: I2:S2O32=1:2\text{I}_2 : \text{S}_2\text{O}_3^{2-} = 1:2, so n(I2)=12(8.40×105)=4.20×105 moln(\text{I}_2) = \tfrac{1}{2}(8.40 \times 10^{-5}) = 4.20 \times 10^{-5}\ \text{mol}. (1 mark)

Step 3: from O22I2\text{O}_2 \rightarrow 2\text{I}_2, the ratio is 1:21:2, so n(O2)=12(4.20×105)=2.10×105 moln(\text{O}_2) = \tfrac{1}{2}(4.20 \times 10^{-5}) = 2.10 \times 10^{-5}\ \text{mol}. (1 mark)

Step 4: c(O2)=2.10×1050.0500=4.20×104 mol L1c(\text{O}_2) = \dfrac{2.10 \times 10^{-5}}{0.0500} = 4.20 \times 10^{-4}\ \text{mol L}^{-1}. (2 marks)

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