When the exhaust gas of marine engine is passing the supercharger, it needs to cool the water way of the supercharger by sea water or fresh water for preventing over heat. A lot of corrosion product was formed in its water way. Sometimes, it blocked the stream of cooling water and made corrosion hole. Present paper is the study of comparison the corrosion products and oxidation processes of cast iron between flowing sea and fresh water. The test pieces were made of the same cast iron as the supercharger, and the corrosion tests were performed as a function of the surface temperatures of the test pieces and the rate of cooling water in the both test equipments of sea and fresh water. The crystalline iron oxides in both corrosion products were analyzed by the powder method of X-ray diffractometer. The intensity of diffracted X-ray of a certain iron oxide was expressed by the percentage intensity in the total counts of iron oxides measured. A temperature of the cooling water 60°C and the surface temperature of test pieces 80°C, hematite, Fe(OH)
2 and goethite presented less than 20%, respectively, and the intensities of them decreased with increasing in cooling water rate in sea water. These iron oxides were a few in fresh water. The quantities of γ-Fe
2O
3, Fe(OH)
3 and magnetite were a little larger in fresh water than those in sea water. The corrosion rate in sea water was about 1.7 times larger than that in fresh water.
The oxidation processes of iron were proposed as follows; Fe
3+→Fe(OH)
3→goethite→hematite and Fe
2+→Fe(OH)
2→magnetite→lepidocrocite→γ-Fe
2O
3→hematite. The relationships of diffracted X-ray intensities between the neighboring iron oxides along with the oxidation process were examined. At 45°C of unheated test piece surface in sea water, the processes of magnetite→lepidocrocite and lepidocrocite→γ-Fe
2O
3 were estimated to be 1% level of significance, and were considered as predominant processes. At the temperature range of 45°-55°C heated, the process of magnetite→lepidocrocite→γ-Fe
2O
3 were estimated to be 1% level of significance. At the temperature range of 60°-80°C heated, lepidocrocite was not detected in sea water and the process of Fe(OH)
3→goethite→hematite were estimated to be 1% level of significance. In the fresh water at the temperature range of 80°-100°C, the oxidation process of Fe(OH)
3→goethite←hematite were estimated to be 1% level of significance. From these results, it was found that the corrosion products and the oxidation processes of iron were different depending on sea and fresh waters and the temperatures of test pieces.
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