Apparatus for determining the ozone decay rate constant for an ozone-in-water solution. The apparatus includes a single ozone residual sensor, to which a sample flow is directed to measure the initial ozone residual concentration, and to which a delayed flow stream of the same solution is directed to measure the ozone residual concentration after passage of a particular time interval. The time delay of the flow stream is achieved by passing the flow stream through a chamber that includes a tubing coil through which the sample stream flows, after which the ozone residual concentration of the delayed sample stream is measured by the same ozone residual sensor. A portion of the incoming flow stream is diverted to flow through the chamber to maintain the delayed sample stream at substantially the same temperature as the incoming flow stream.
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