A detector-volume-averaging correction factor converts a specified spatially averaged absorbed dose into the point value associated with that measurement. It depends on the radiation field and the detector geometry. The IAEA defines this comparison in undisturbed water, with the detector absent, so the factor isolates detector volume averaging from perturbations caused by inserting an ionization chamber.[ref]
For a normalized nonnegative spatial weighting function , let
assuming the denominator is positive. Multiplication by then recovers the point value in this response model. The averaging law is developed in detector volume averaging; the correction requires additional information about the spatial field, not just one scalar detector reading.
For an original exact example, take a uniformly sensitive one-dimensional detector of full width centred at a smooth peak. Over its footprint stipulate with and . Direct integration gives
With and , the average is and . A small local under-response becomes a factor greater than one.
At a valley with and the same parameters, the factor is instead . Thus an averaging correction need not exceed one. A uniform field gives exactly one. Reusing a peak-derived factor at a different location can therefore introduce an error.
In a proposed characterization, obtain a sufficiently resolved beam profile, account for the profiling detector's own spatial resolution, and integrate that profile with the intended detector's geometric weighting. The IAEA's geometric models explicitly distinguish different weightings across the projected detector area.[ref] A factor derived this way addresses spatial averaging under the stated field conditions; it does not independently correct energy response, recombination or an erroneous measurement calibration.

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