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Estimation of Dissolved Oxygen

Estimation of Dissolved Oxygen
The estimation of dissolved oxygen is done by titrimetric method. A known amount of the oxidizing agent, manganous sulphate is added to the water to be estimated. Manganous sulphate reacts with the oxygen present in the water. During the reaction, the oxygen is bound to the manganese (chemical element Mn), forming a brownish solid which settles to the bottom of the bottle (MnO2). This process is called fixing the oxygen.

In order for this fixation process to work however, the solution must e at high pH, so another reagent is added to facilitate the above requirement. Potassium iodide is added to function as a dye, and will react with the sulphuric acid added.

Upon addition of the sulphuric acid, the MnO2 from above is reduced to Mn2+, and the iodine from the potassium iodide above is oxidized by the MnO2 from I- to I2. This reaction step effectively causes the solution to take on a yellowish brown colour proportional to the number of I2 molecules present which in turn is proportional to the original amount of O2 molecules in the water. This iodine is titrated by sodium thiosulphate solution using starch as an indicator.

Sodium thiosulphate standard solution is added drop by drop to the mixing bottle, swirling to mix after each drop. The dropper is held vertically above the bottle and each drop is counted as it is added. As drops of this chemical enter the solution, the sodium separates from the thiosulphate ion. The thiosulphate then reacts with iodine (I2) molecules available in the water. When the iodine molecules react, they break up into iodide- ions which are colourless.

2S2O32- + I2 = S4O62- + 2I-

Thus 4 molecules of the sodium thiosulphate are required to change the colour resulting from one molecule of O2 in the original water. Thus we get a very accurate estimate of the number of O2 molecules in the original solution.

The dissolved oxygen in any water body diminishes due to various reasons which include:

Heterotrophic microbial activity in water.
Dissolved oxygen used up by aquatic microorganisms, plants and animals.
Addition of sewage or other organic wastes.
Decomposition of dead organic matter.

 

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