Search for high energy neutrino induced cascades with the AMANDA-B10 detector

The Antarctic Muon And Neutrino Detector Array, AMANDA, is a Cherenkov detector deployed deep in the ice cap at the South Pole. Charged particles traveling faster than the speed of light in ice produce Cherenkov radiation that is detected by Photo-Multiplier Tubes. Using the information obtained by...

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Main Author: Toboada Fermin, Ignacio Jose
Format: Text
Language:English
Published: ScholarlyCommons 2002
Subjects:
Online Access:https://repository.upenn.edu/dissertations/AAI3043964
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spelling ftunivpenn:oai:repository.upenn.edu:dissertations-3116 2023-05-15T13:40:32+02:00 Search for high energy neutrino induced cascades with the AMANDA-B10 detector Toboada Fermin, Ignacio Jose 2002-01-01T08:00:00Z https://repository.upenn.edu/dissertations/AAI3043964 ENG eng ScholarlyCommons https://repository.upenn.edu/dissertations/AAI3043964 Dissertations available from ProQuest Particle physics|Astronomy|Astrophysics text 2002 ftunivpenn 2021-01-04T22:16:00Z The Antarctic Muon And Neutrino Detector Array, AMANDA, is a Cherenkov detector deployed deep in the ice cap at the South Pole. Charged particles traveling faster than the speed of light in ice produce Cherenkov radiation that is detected by Photo-Multiplier Tubes. Using the information obtained by the Photo-Multiplier Tubes, the physical characteristics, such as direction and energy, can be reconstructed. High energy neutrinos of all flavors can produce particle cascades when interacting with matter. In ice, cascades are typically a few meters long, much smaller than the dimensions of AMANDA. Electron neutrinos produce cascades via both the charged and neutral current interactions. Muon and tau neutrinos produce cascades via the neutral current interaction. Isolated cascades are also produced by tau neutrinos via charged current interactions, because the resulting tau, at energies below a few hundred TeV, will travel only a few meters before decaying. Advantages of the cascade channel, compared to neutrino induced muons are better energy resolution and an order of magnitude lower background from atmospheric neutrinos when searching for extra terrestrial neutrinos. Data collected in 1997 were searched for high energy neutrino induced cascades. A total of 1.18 × 109 events were recorded for an effective live-time of 130.1 days. The overwhelming majority of the events recorded were produced by down-going cosmic-ray induced muons. Bright muon energy losses are the main background when searching for high energy extra-terrestrial neutrino induced cascades. The sensitivity of the detector to cascades has been studied using in-situ light sources. No evidence for the existence of a diffuse flux of high energy neutrinos has been found. Limits have been set for fluxes following an E −2 power law spectrum. For [special characters omitted] the limit is[special characters omitted]For [special characters omitted] the limit is[special characters omitted]For both cases the limits are shown with and without the effect of systematic errors. The flux limits were obtained for neutrino energies between 5 TeV and 300 TeV. The effective detector volume has also been calculated for every neutrino flavor, allowing the calculation of fluxes for any neutrino flux model. Text Antarc* Antarctic Ice cap South pole South pole University of Pennsylvania: ScholaryCommons@Penn Antarctic The Antarctic South Pole
institution Open Polar
collection University of Pennsylvania: ScholaryCommons@Penn
op_collection_id ftunivpenn
language English
topic Particle physics|Astronomy|Astrophysics
spellingShingle Particle physics|Astronomy|Astrophysics
Toboada Fermin, Ignacio Jose
Search for high energy neutrino induced cascades with the AMANDA-B10 detector
topic_facet Particle physics|Astronomy|Astrophysics
description The Antarctic Muon And Neutrino Detector Array, AMANDA, is a Cherenkov detector deployed deep in the ice cap at the South Pole. Charged particles traveling faster than the speed of light in ice produce Cherenkov radiation that is detected by Photo-Multiplier Tubes. Using the information obtained by the Photo-Multiplier Tubes, the physical characteristics, such as direction and energy, can be reconstructed. High energy neutrinos of all flavors can produce particle cascades when interacting with matter. In ice, cascades are typically a few meters long, much smaller than the dimensions of AMANDA. Electron neutrinos produce cascades via both the charged and neutral current interactions. Muon and tau neutrinos produce cascades via the neutral current interaction. Isolated cascades are also produced by tau neutrinos via charged current interactions, because the resulting tau, at energies below a few hundred TeV, will travel only a few meters before decaying. Advantages of the cascade channel, compared to neutrino induced muons are better energy resolution and an order of magnitude lower background from atmospheric neutrinos when searching for extra terrestrial neutrinos. Data collected in 1997 were searched for high energy neutrino induced cascades. A total of 1.18 × 109 events were recorded for an effective live-time of 130.1 days. The overwhelming majority of the events recorded were produced by down-going cosmic-ray induced muons. Bright muon energy losses are the main background when searching for high energy extra-terrestrial neutrino induced cascades. The sensitivity of the detector to cascades has been studied using in-situ light sources. No evidence for the existence of a diffuse flux of high energy neutrinos has been found. Limits have been set for fluxes following an E −2 power law spectrum. For [special characters omitted] the limit is[special characters omitted]For [special characters omitted] the limit is[special characters omitted]For both cases the limits are shown with and without the effect of systematic errors. The flux limits were obtained for neutrino energies between 5 TeV and 300 TeV. The effective detector volume has also been calculated for every neutrino flavor, allowing the calculation of fluxes for any neutrino flux model.
format Text
author Toboada Fermin, Ignacio Jose
author_facet Toboada Fermin, Ignacio Jose
author_sort Toboada Fermin, Ignacio Jose
title Search for high energy neutrino induced cascades with the AMANDA-B10 detector
title_short Search for high energy neutrino induced cascades with the AMANDA-B10 detector
title_full Search for high energy neutrino induced cascades with the AMANDA-B10 detector
title_fullStr Search for high energy neutrino induced cascades with the AMANDA-B10 detector
title_full_unstemmed Search for high energy neutrino induced cascades with the AMANDA-B10 detector
title_sort search for high energy neutrino induced cascades with the amanda-b10 detector
publisher ScholarlyCommons
publishDate 2002
url https://repository.upenn.edu/dissertations/AAI3043964
geographic Antarctic
The Antarctic
South Pole
geographic_facet Antarctic
The Antarctic
South Pole
genre Antarc*
Antarctic
Ice cap
South pole
South pole
genre_facet Antarc*
Antarctic
Ice cap
South pole
South pole
op_source Dissertations available from ProQuest
op_relation https://repository.upenn.edu/dissertations/AAI3043964
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