Heat defect (calorimetry)
ID: heat-defect-calorimetry
The heat defect in water calorimetry measures the fraction of absorbed energy that does not appear as heat because of radiation-induced chemical changes. Writing absorbed energy as and the energy appearing as heat as , the convention used by Norman V. Klassen and Carl K. Ross isA positive value means less heat than the absorbed-energy equivalent; a negative value means the chemical response adds heat.[ref]
Water Calorimetry: The Heat Defect by Norman V. Klassen and Carl K. Ross. Printed p.63, Eqs1–2 and accompanying definition.
If other thermal corrections are treated separately, the absorbed dose isAn illustrative means that represents 98% of the dose, so the chemical correction multiplies that thermal estimate by . The example fixes a sign convention; it is not a measured universal value for water.
The motivating evidence included variations with dissolved gases and comparison of radiolysis calculations with chemical measurements of hydrogen peroxide. Those tests address chemical energy accounting. An external heat leak or a drifting thermometer can also alter a temperature reading, but belongs to a different correction mechanism.[ref]
Water Calorimetry: The Heat Defect by Norman V. Klassen and Carl K. Ross. Abstract and Introduction: radiolysis model and independently measured chemical product.
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