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In this experiment, dissolved oxygen (D.O.) in a water sample is estimated using Winkler's method, a redox titration.
The dissolved oxygen in the water sample reacts with manganese (II) sulfate to form manganese (IV) hydroxide, which is then acidified to release iodine from potassium iodide. The iodine produced is titrated with sodium thiosulfate to estimate the amount of oxygen in the sample. The dissolved oxygen concentration is calculated in parts per million (ppm).
Measurement | Value |
---|---|
Rough titre | 13.3 cmÂł |
Second titre | 13.0 cmÂł |
Third titre | 13.0 cmÂł |
Average of accurate titres | 13.0 cmÂł |
Volume of water sample | 50.0 cmÂł |
Molarity of thiosulfate | 0.005 M |
Moles of thiosulfate used:
Moles of dissolved oxygen (Oâ‚‚):
Dissolved oxygen in ppm:
Manganese (II) sulfate reacts with dissolved oxygen to form a brown precipitate of manganese (IV) hydroxide, which is necessary to indirectly measure the dissolved oxygen.
The sulfuric acid dissolves the manganese (IV) hydroxide, releasing iodine from potassium iodide, which can then be titrated with sodium thiosulfate.
The endpoint is reached when the blue colour from the starch-iodine complex disappears, indicating that all iodine has reacted with thiosulfate.
To ensure no air is trapped, which could introduce additional oxygen and give inaccurate results.
Low dissolved oxygen levels may indicate pollution or high levels of organic matter, leading to oxygen depletion, which can harm aquatic life.
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