Carl K. Ross is a physicist associated with ionizing radiation standards and water calorimetry. His 1997 paper with Norman V. Klassen identifies both authors with the ionizing-radiation standards laboratory in Ottawa and examines a fundamental problem in radiation dosimetry: deposited energy and measured heat need not be equal when irradiation also produces chemical reactions.[ref]
Their analysis expresses the heat defect as
where is absorbed energy, is the energy appearing as heat, is absorbed dose, and is the specific heat capacity of water. The temperature rise supplies a measurable thermal signal, while the heat defect accounts for the energy balance associated with radiolysis.[ref]
For a hypothetical example, suppose the measured thermal quantity is and the heat defect is . The corrected absorbed dose is then . The illustrative correction is chosen for arithmetic, rather than quoted as an experimental result. A positive heat defect means that some absorbed energy does not appear as heat; a negative value means that the measured heat exceeds the absorbed energy, with the difference supplied by the accompanying chemical reactions.
Ross and Norman V. Klassen later published a correction to an input reaction rate constant in their computer simulation. Their 2002 paper provides an explicit example of revising a physical measurement model when a supporting parameter changes.[ref]

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