Energy flow in a hadronic cascade: Application to hadron calorimetry

The hadronic cascade description developed in an earlier paper is extended to the response of an idealized fine-sampling hadron calorimeter. Calorimeter response is largely determined by the transfer of energy Eπ0 from the hadronic to the electromagnetic sector via π0 production. Fluctuations in thi...

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Veröffentlicht in:Nuclear instruments & methods in physics research. Section A, Accelerators, spectrometers, detectors and associated equipment Accelerators, spectrometers, detectors and associated equipment, 2007-03, Vol.572 (2), p.633-653
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description The hadronic cascade description developed in an earlier paper is extended to the response of an idealized fine-sampling hadron calorimeter. Calorimeter response is largely determined by the transfer of energy Eπ0 from the hadronic to the electromagnetic sector via π0 production. Fluctuations in this quantity produce the “constant term” in hadron calorimeter resolution. The increase of its fractional mean, fπ00=〈Eπ0〉/E, with increasing incident energy E causes the energy dependence of the π/e ratio in a noncompensating calorimeter. The mean hadronic energy fraction, fh0=1-fπ00, was shown to scale very nearly as a power law in E: fh0=(E/E0) m-1, where E0≈1GeV for pions, and m≈0.83. It follows that π/e=1-(1-h/e)(E/E0) m-1, where electromagnetic and hadronic energy deposits are detected with efficiencies e and h, respectively. If the mean fraction of fh0 which is deposited as nuclear gamma rays is fγ0, then the expression becomes π/e=1-(1-h′/e)(1-fγ0)(E/E0) m-1. Fluctuations in these quantities, along with sampling fluctuations, are incorporated to give an overall understanding of resolution, which is different from the usual treatments in interesting ways. The conceptual framework is also extended to the response to jets and the difference between π and p response.
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subjects Hadron calorimetry
Hadron cascades
Sampling calorimetry
title Energy flow in a hadronic cascade: Application to hadron calorimetry
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