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28–29 mai 2018
IJCLab
Fuseau horaire Europe/Paris

Measurement of the top quark pole mass using double differential cross section with the ATLAS detector at the LHC

29 mai 2018, 16:15
1h
200/0-Auditorium - Auditorium P. Lehmann (IJCLab)

200/0-Auditorium - Auditorium P. Lehmann

IJCLab

Bâtiment 200, 91440 Orsay, France
250
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Orateur

Mme Tetiana Moskalets (CEA/IRFU/DPhP)

Description

The top quark mass (mt) is a key parameter of the Standard Model (SM). Its large size, of the order of the electroweak scale, is associated with a Yukawa coupling of order 1, that gives important contributions, via radiative corrections, to SM observables. After the Higgs boson discovery and the accurate measurement of its mass, the allowed values of the W boson and top quark masses have become strongly correlated, so that an accurate determination of both would lead to a SM test of considerable precision. The top mass value is also critical in the issue of vacuum stability in the SM.

The determination of the top quark pole mass (mt,pole) requires the measurement of quantities that can be calculated theoretically, for example the inclusive tt¯ production cross section, which depends on mt,pole. Therefore, its measurement allows to indirectly measure mt,pole.

The huge tt¯ samples collected at the LHC with ATLAS detector allow the measurement of differential production cross sections dσtt¯/dX, where X is a kinematical variable of the tt¯ system. The full information available in differential cross sections can be exploited for the determination of mt,pole if theoretical calculation for differential tt¯ production cross sections are available for different values of mt,pole. This technique has been recently applied by D0 experiment at Tevatron. 
The tt¯ samples available at the LHC after collection of 100 fb1 of collision data will allow the measurement of double-differential tt¯ production cross sections. Using these distributions to extract mt,pole has the advantage that possible correlations between variables are automatically taken into account.

The comparison between differential cross section measurements corrected at the parton-level and their theoretical calculations for different mt values will allow to extract mt,pole.

Auteur principal

Mme Tetiana Moskalets (CEA/IRFU/DPhP)

Documents de présentation

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