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Ground water that is obtained from a deep‐well source seldom contains many bacteria or contaminants. Adding chlorine to relatively pure ground water produces an immediate, noticeable change in taste and odor qualities. Chlorine dioxide, however, has been shown to yield a chlorine residual that is hardly noticeable through taste or odor, yet maintains USPHS standards.
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Harold W. Augenstein (1974) studied this question.
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