Multiplicity distributions of gluon and quark jets and tests of QCD analytic predictions

dc.creatorThe OPAL Collaboration
dc.creatoral, K. Ackerstaff et
dc.date1997-08-19
dc.date.accessioned2026-07-07T11:46:49Z
dc.date.available2026-07-07T11:46:49Z
dc.descriptionGluon jets are identified in e+e- hadronic annihilation events by tagging two quark jets in the same hemisphere of an event. The gluon jet is defined inclusively as all the particles in the opposite hemisphere. Gluon jets defined in this manner have a close correspondence to gluon jets as they are defined for analytic calculations, and are almost independent of a jet finding algorithm. The charged particle multiplicity distribution of the gluon jets is presented, and is analyzed for its mean, dispersion, skew, and curtosis values, and for its factorial and cumulant moments. The results are compared to the analogous results found for a sample of light quark (uds) jets, also defined inclusively. We observe differences between the mean, skew and curtosis values of gluon and quark jets, but not between their dispersions. The cumulant moment results are compared to the predictions of QCD analytic calculations. A calculation which includes next-to-next-to-leading order corrections and energy conservation is observed to provide a much improved description of the data compared to a next-to-leading order calculation without energy conservation. There is agreement between the data and calculations for the ratios of the cumulant moments between gluon and quark jets.
dc.description32 pages, LaTeX, uses a4p.sty, 9 eps figures included (plus in colour), submitted to Zeit. Phys. C
dc.identifierhttps://arxiv.org/abs/hep-ex/9708029
dc.identifierhttp://arxiv.org/abs/hep-ex/9708029
dc.identifierEur.Phys.J.C1:479-494,1998
dc.identifierdoi:10.1007/s100520050097
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/202359
dc.subjectHigh Energy Physics - Experiment
dc.titleMultiplicity distributions of gluon and quark jets and tests of QCD analytic predictions
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