To estimate the amount of dissolved oxygen present in the given water sample.
Winkler’s method.
The given sample is treated with manganous sulphate followed by alkaline iodide. First, manganous sulphate reacts with potassium hydroxide resulting in potassium sulphate and manganous hydroxide.
Manganous hydroxide thus formed reacts with the dissolved oxygen present in the sample and forms manganic hydroxide.
Manganic hydroxide thus formed reacts with potassium iodide in the presence of concentrated sulphuric acid; as a result, potassium sulphate and manganous sulphate are formed liberating free iodine. This liberated iodine is equivalent to the amount of oxygen dissolved in the given water sample.
The liberated iodine is titrated against 0.025 N sodium thiosulphate (hypo) solution by using 1% starch solution as the indicator. The disappearance of the blue colour is the end point of titration.
The dissolved oxygen content is calculated using the following formula:
(At normal temperature and pressure, 8 g of oxygen is present in 1 litre of water; 1 mg = 1.43 ml and 1 ml = 0.698 mg.)
Amount of oxygen dissolved in the given sample at room temperature = _____ cc or ml/L.
Amount of oxygen dissolved in the given sample at 70° C = _____ cc or ml/L.
Oxygen is one of the most limiting abiotic factors and is essential for living organisms. Living cells require energy to perform metabolic activities. This energy is liberated or generated by the oxidation of food stuff within the cells in the presence of oxygen.
The actual quantity of oxygen present in water under the most favourable conditions is much less than that present in the atmosphere. The amount of oxygen present in the atmosphere is 210 cc or ml/L, whereas that present in 1 L of water does not exceed 10 cc or ml/L. Hence, dissolved oxygen acts as a limiting factor in the distribution of aquatic animals because most living organisms require oxygen for respiration. The oxygen supply in water comes chiefly from the following sources:
It depends on temperature, salinity, pressure, humidity, pollution etc., which greatly affect the capacity of water to retain oxygen for organisms. For example, as the temperature of the water increases, its oxygen-retaining capacity decreases, irrespective of whether it is fresh or marine water. The surface of water, which is in contact with air, will have greater amount of oxygen when compared to lower parts.
It is evident from the experiment that the amount of oxygen present in the sample at room temperature (28°C) is greater than that at 70°C. This is because as the temperature increases, the water gets heated up; its capacity to retain oxygen is reduced and oxygen may be released into the atmosphere.
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