Surface water is generally coloured by natural organic materials such as humic, fulvic and tannic acids. These compounds result from the decay of vegetative materials and are generally related to phenol like compounds; having conjugated carbon/carbon double bonds. When the series of double bonds cross over about twenty, the colour absorption shows up in the visible spectrum. Ozone breaks this organic double bonds, and as more of these double bonds are broken, the colour disappears. Surface water can usually be decolourized when treated with 2 to 4 ppm of ozone. Chlorination of humic material leads to chlorophenols which are carcinogenic, have bad odour and bad taste. Most of the odour can be removed by treatment with ozone. Even some sulphur compounds such as hydrogen sulphide, mercaptans or organic sulphides can be oxidised to sulphates with ozone. Chlorine reacts with organic materials to form chloro compounds like chloroform, carbon tetrachloride, chloromethane and others, generally known as Trihalomethanes (THMs). Ozone reacts with organics to break them down into simpler compounds. Combined with activated charcoal, these can be removed. This water can then be treated with low level of Chlorine, say 0.2 - 0.3 ppm to maintain sanitation in the distribution system. This way no THMs will be formed. The THMs have been implicated as carcinogens in the development of kidney, bladder and colon cancer. |