Chemistry of the Environment – Water: Testing Purity
1. Objective
To describe how to test the purity of water using qualitative colour‑change tests and quantitative melting‑point (freezing‑point) and boiling‑point determinations, and to relate these techniques to the wider Cambridge IGCSE 0620 syllabus.
Extraction example: iron from Fe₂O₃ in a blast furnace using coke (C) as a reducing agent.
4. Water – Purity Testing
4.1 Why Test Purity?
Pure water freezes at 0 °C and boils at 100 °C (1 atm).
Any dissolved non‑volatile solute lowers the freezing point (freezing‑point depression) and raises the boiling point (boiling‑point elevation) – both are colligative properties.
Magnitude of the change is proportional to the total molality of solutes:
\[
\Delta T_f = iK_f m \qquad \Delta T_b = iK_b m
\]
where K_f = 1.86 °C·kg mol⁻¹, K_b = 0.512 °C·kg mol⁻¹ for water and i is the van t Hoff factor.
4.2 Typical Contaminants (Cambridge list)
Group
Examples
Effect on Colligative Properties?
Inorganic salts
NaCl, CaSO₄, Mg(NO₃)₂
↓ T_f, ↑ T_b
Organic matter
Sugars, ethanol, pesticides
↓ T_f, ↑ T_b
Dissolved gases
O₂, CO₂
Negligible (very low concentration)
Heavy‑metal ions
Fe³⁺, Pb²⁺ (as soluble salts)
↓ T_f, ↑ T_b
Micro‑organisms
Bacteria, algae
No direct effect on T_f/T_b (requires microbiological tests)
Sedimentation – removes suspended solids; does not change T_f or T_b.
Filtration – mechanical removal of fine particles; similarly no effect on colligative properties.
Activated‑carbon adsorption – removes many organic solutes; may reduce ΔT_f/ΔT_b if organics are the main impurity.
Chlorination – adds Cl₂/HOCl; the resulting chloride ions act as a very dilute non‑volatile solute, causing a <0.1 °C> rise in boiling point – essentially negligible for most school‑level measurements.
4.4 Qualitative Colour‑Change Tests (rapid indication of water & some ions)
Dry reagent
Colour change on addition of water
Interpretation
Anhydrous cobalt(II) chloride, CoCl₂·6H₂O
Blue → pink (monohydrate) → purple (excess water)
Detects presence of water (hydrolysis).
Anhydrous copper(II) sulfate, CuSO₄
White → blue (pentahydrate)
Detects water; persistent blue after drying also indicates sulphate ions.
Independent variable: type of water (distilled vs. sample).
Dependent variables: observed freezing point and boiling point.
Controlled variables: atmospheric pressure (~1 atm), volume of water, heating/cooling rate, thermometer calibration, composition of ice‑salt bath.
Include a control (distilled water) in each series of measurements.
Perform at least three repetitions per sample; report the mean ± standard deviation.
Record any anomalies (super‑cooling, premature bubbling, thermometer lag).
Procedure
4.5.1 Freezing‑Point (Melting‑Point of Ice) Determination
Prepare an ice‑salt bath in a polystyrene cup; stir until a stable temperature (e.g., –15 °C) is reached. Record the bath temperature.
Fill a thin‑walled glass tube with ~2 mL of the water sample, seal, and tap gently to remove trapped air.
Immerse the tube in the ice‑salt bath, ensuring the thermometer bulb lies within the liquid but does not touch the tube wall.
Allow the system to equilibrate. Observe the temperature at which the first ice crystals appear on cooling (or the first liquid droplets appear on warming). This temperature is the **freezing point**.
Repeat the same steps with distilled water as a reference.
Carry out three trials for each water type and calculate the average.
4.5.2 Boiling‑Point Determination
Measure 50 mL of the water sample into a clean beaker.
Place the beaker on a pre‑heated hot plate (or Bunsen burner). Insert the thermometer so the bulb is ~1 cm below the surface.
Heat gently, then increase to a steady boil. Record the temperature when a **continuous stream of bubbles** forms and the temperature stops rising – this is the boiling point.
Maintain the boil for at least 30 s and note the stable temperature.
Repeat with distilled water under identical conditions.
Perform three repetitions per sample and compute the mean.
Data‑Recording Table
Test
Pure (Distilled) Water
Sample Water (mean ± SD)
Interpretation
Freezing point (°C)
0.0
Boiling point (°C) at 1 atm
100.0
Calculations (optional – quantitative analysis)
Use the average temperature deviation to estimate the total concentration of dissolved non‑volatile solutes.
Solve for molality \(m\) (mol kg⁻¹). Set \(i = 1\) for a non‑electrolyte; for a 1:1 electrolyte use \(i = 2\); adjust for other electrolytes accordingly.
Interpretation of Results
Freezing point < 0 °C → dissolved solutes present.
Boiling point > 100 °C → same solutes raise the boiling temperature.
The magnitude of the deviation gives an estimate of total solute concentration, but not the identity of the impurity.
If both temperatures agree with the pure‑water values (within experimental error), the water can be considered chemically pure (microbial contamination would need separate tests).
Colour‑change tests that show no colour shift support the conclusion of purity.
Limitations of the Temperature Methods
Only detects **non‑volatile** solutes; gases and very low‑concentration contaminants may be missed.
Cannot distinguish between different solutes – a mixture of salts and organics gives the same overall ΔT.
Super‑cooling or premature nucleation can give falsely low freezing‑point readings.
Accurate boiling‑point measurement requires stable atmospheric pressure; altitude corrections are needed for field work.
5. Complementary Tests
Acid–base titration – determines hardness (Ca²⁺, Mg²⁺) by complexometric titration with EDTA or by neutralising carbonate hardness with a strong acid.
Conductivity measurement – a quick indicator of total ionic content; higher conductivity correlates with larger ΔT values.
Spectroscopic or chromatographic methods (advanced) – identify specific organic pollutants, but are beyond the IGCSE scope.
6. Safety Precautions
Wear safety goggles, lab coat and heat‑resistant gloves.
Handle hot equipment (boiling water, Bunsen burner) with tongs or heat‑proof gloves.
When preparing the ice‑salt bath, avoid skin contact with the extremely cold mixture.
Work in a well‑ventilated area if using a Bunsen burner.
Dispose of coloured reagent waste according to school safety guidelines.
7. Suggested Diagram
Schematic showing (a) a sealed glass tube with thermometer immersed in an ice‑salt bath for the freezing‑point test, and (b) a beaker on a hot plate with a thermometer positioned just below the surface for the boiling‑point test.
8. Summary
Testing water purity in the IGCSE curriculum combines rapid qualitative colour‑change tests (anhydrous CoCl₂ and CuSO₄) with quantitative melting‑point (freezing‑point) and boiling‑point determinations. Pure water freezes at 0 °C and boils at 100 °C (1 atm). Any deviation indicates dissolved non‑volatile solutes, and the size of the deviation can be used to estimate total solute concentration via the colligative‑property equations. The method fits within a broader environmental context that includes typical contaminants, water‑treatment processes, related fertilizer analysis, and links to air‑quality monitoring. A solid understanding of the core chemistry topics (states of matter, atoms, stoichiometry, electrochemistry, energetics, reactions, acids & bases, periodic trends, and metals) underpins the interpretation of the results.
9. Assessment Questions
Explain why a non‑volatile solute lowers the freezing point of water, including a brief discussion of vapour‑pressure lowering.
A water sample freezes at -2.5 °C. Assuming the solute is a non‑electrolyte, calculate its molality using K_f = 1.86 °C·kg mol⁻¹.
During a boiling‑point test the temperature stabilises at 101.2 °C. Estimate the molality of the solute if it is a 1:1 electrolyte (i = 2) using K_b = 0.512 °C·kg mol⁻¹.
List two limitations of using melting‑point and boiling‑point determinations for assessing water purity.
Describe how an acid–base titration could be used to complement the temperature tests when checking for water hardness.
Briefly discuss why chlorination does not significantly affect the boiling point of treated water.
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