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Measurements of atmospheric neutrinos and antineutrinos in the MINOS Far Detector

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Measurements of atmospheric neutrinos and antineutrinos in the MINOS Far Detector. / MINOS Collaboration.
In: Physical Review D – Particles and Fields, Vol. 86, No. 5, 052007, 17.09.2012.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

MINOS Collaboration 2012, 'Measurements of atmospheric neutrinos and antineutrinos in the MINOS Far Detector', Physical Review D – Particles and Fields, vol. 86, no. 5, 052007. https://doi.org/10.1103/PhysRevD.86.052007

APA

MINOS Collaboration (2012). Measurements of atmospheric neutrinos and antineutrinos in the MINOS Far Detector. Physical Review D – Particles and Fields, 86(5), Article 052007. https://doi.org/10.1103/PhysRevD.86.052007

Vancouver

MINOS Collaboration. Measurements of atmospheric neutrinos and antineutrinos in the MINOS Far Detector. Physical Review D – Particles and Fields. 2012 Sept 17;86(5):052007. doi: 10.1103/PhysRevD.86.052007

Author

MINOS Collaboration. / Measurements of atmospheric neutrinos and antineutrinos in the MINOS Far Detector. In: Physical Review D – Particles and Fields. 2012 ; Vol. 86, No. 5.

Bibtex

@article{a9dea299ab9d4e8fa2d6bf4fb85a01eb,
title = "Measurements of atmospheric neutrinos and antineutrinos in the MINOS Far Detector",
abstract = "This paper reports measurements of atmospheric neutrino and antineutrino interactions in the MINOS Far Detector, based on 2553 live-days (37.9 kton-years) of data. A total of 2072 candidate events are observed. These are separated into 905 contained-vertex muons and 466 neutrino-induced rock-muons, both produced by charged-current νμ and ν̅ μ interactions, and 701 contained-vertex showers, composed mainly of charged-current νe and ν̅ e interactions and neutral-current interactions. The curvature of muon tracks in the magnetic field of the MINOS Far Detector is used to select separate samples of νμ and ν̅ μ events. The observed ratio of ν̅ μ to νμ events is compared with the Monte Carlo (MC) simulation, giving a double ratio of Rν̅ /νdata/Rν̅ /νMC=1.03±0.08(stat)±0.08(syst). The νμ and ν̅ μ data are separated into bins of L/E resolution, based on the reconstructed energy and direction of each event, and a maximum likelihood fit to the observed L/E distributions is used to determine the atmospheric neutrino oscillation parameters. This fit returns 90% confidence limits of |Δm2|=(1.9±0.4)×10-3  eV2 and sin⁡22θ>0.86. The fit is extended to incorporate separate νμ and ν̅ μ oscillation parameters, returning 90% confidence limits of |Δm2|-|Δm̅ 2|=0.6-0.8+2.4×10-3  eV2 on the difference between the squared-mass splittings for neutrinos and antineutrinos.",
author = "P. Adamson and Jaroslaw Nowak and {MINOS Collaboration}",
note = "{\textcopyright} 2012 American Physical Society",
year = "2012",
month = sep,
day = "17",
doi = "10.1103/PhysRevD.86.052007",
language = "English",
volume = "86",
journal = "Physical Review D – Particles and Fields",
issn = "1550-2368",
publisher = "American Physical Society",
number = "5",

}

RIS

TY - JOUR

T1 - Measurements of atmospheric neutrinos and antineutrinos in the MINOS Far Detector

AU - Adamson, P.

AU - Nowak, Jaroslaw

AU - MINOS Collaboration

N1 - © 2012 American Physical Society

PY - 2012/9/17

Y1 - 2012/9/17

N2 - This paper reports measurements of atmospheric neutrino and antineutrino interactions in the MINOS Far Detector, based on 2553 live-days (37.9 kton-years) of data. A total of 2072 candidate events are observed. These are separated into 905 contained-vertex muons and 466 neutrino-induced rock-muons, both produced by charged-current νμ and ν̅ μ interactions, and 701 contained-vertex showers, composed mainly of charged-current νe and ν̅ e interactions and neutral-current interactions. The curvature of muon tracks in the magnetic field of the MINOS Far Detector is used to select separate samples of νμ and ν̅ μ events. The observed ratio of ν̅ μ to νμ events is compared with the Monte Carlo (MC) simulation, giving a double ratio of Rν̅ /νdata/Rν̅ /νMC=1.03±0.08(stat)±0.08(syst). The νμ and ν̅ μ data are separated into bins of L/E resolution, based on the reconstructed energy and direction of each event, and a maximum likelihood fit to the observed L/E distributions is used to determine the atmospheric neutrino oscillation parameters. This fit returns 90% confidence limits of |Δm2|=(1.9±0.4)×10-3  eV2 and sin⁡22θ>0.86. The fit is extended to incorporate separate νμ and ν̅ μ oscillation parameters, returning 90% confidence limits of |Δm2|-|Δm̅ 2|=0.6-0.8+2.4×10-3  eV2 on the difference between the squared-mass splittings for neutrinos and antineutrinos.

AB - This paper reports measurements of atmospheric neutrino and antineutrino interactions in the MINOS Far Detector, based on 2553 live-days (37.9 kton-years) of data. A total of 2072 candidate events are observed. These are separated into 905 contained-vertex muons and 466 neutrino-induced rock-muons, both produced by charged-current νμ and ν̅ μ interactions, and 701 contained-vertex showers, composed mainly of charged-current νe and ν̅ e interactions and neutral-current interactions. The curvature of muon tracks in the magnetic field of the MINOS Far Detector is used to select separate samples of νμ and ν̅ μ events. The observed ratio of ν̅ μ to νμ events is compared with the Monte Carlo (MC) simulation, giving a double ratio of Rν̅ /νdata/Rν̅ /νMC=1.03±0.08(stat)±0.08(syst). The νμ and ν̅ μ data are separated into bins of L/E resolution, based on the reconstructed energy and direction of each event, and a maximum likelihood fit to the observed L/E distributions is used to determine the atmospheric neutrino oscillation parameters. This fit returns 90% confidence limits of |Δm2|=(1.9±0.4)×10-3  eV2 and sin⁡22θ>0.86. The fit is extended to incorporate separate νμ and ν̅ μ oscillation parameters, returning 90% confidence limits of |Δm2|-|Δm̅ 2|=0.6-0.8+2.4×10-3  eV2 on the difference between the squared-mass splittings for neutrinos and antineutrinos.

U2 - 10.1103/PhysRevD.86.052007

DO - 10.1103/PhysRevD.86.052007

M3 - Journal article

VL - 86

JO - Physical Review D – Particles and Fields

JF - Physical Review D – Particles and Fields

SN - 1550-2368

IS - 5

M1 - 052007

ER -