neutrinos: optimal detector locations

Abstract. A model-independent experimental signature for flavour oscillations in the neutrino signal from the next Galactic supernova (SN) would be the observation of Earth matter effects. We calculate the probability for observing a Galactic SN shadowed by the Earth as a function of the detector’s...

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Main Authors: A Mirizzi, G G Raffelt, P D Serpico
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2006
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5075
http://wwwth.mpp.mpg.de/members/raffelt/mypapers/200601.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.564.5075 2023-05-15T18:22:07+02:00 neutrinos: optimal detector locations A Mirizzi G G Raffelt P D Serpico The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5075 http://wwwth.mpp.mpg.de/members/raffelt/mypapers/200601.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5075 http://wwwth.mpp.mpg.de/members/raffelt/mypapers/200601.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://wwwth.mpp.mpg.de/members/raffelt/mypapers/200601.pdf supernova neutrinos neutrino detectors ArXiv ePrint astro-ph/0604300 c©2006 IOP Publishing Ltd and SISSA 1475-7516/06/05012+17$30.00 text 2006 ftciteseerx 2016-01-08T12:11:54Z Abstract. A model-independent experimental signature for flavour oscillations in the neutrino signal from the next Galactic supernova (SN) would be the observation of Earth matter effects. We calculate the probability for observing a Galactic SN shadowed by the Earth as a function of the detector’s geographic latitude. This probability depends only mildly on details of the Galactic SN distribution. A location at the North Pole would be optimal with a shadowing probability of about 60%, but a far-northern location such as Pyhäsalmi in Finland, the proposed site for a large-volume scintillator detector, is almost equivalent (58%). We also consider several pairs of detector locations and calculate the probability that only one of them is shadowed, allowing a comparison between a shadowed and a direct signal. For the South Pole combined with Kamioka, this probability is almost 75%; for the South Pole combined with Pyhäsalmi, it is almost 90%. One particular scenario consists of a large-volume scintillator detector located in Pyhäsalmi to measure the geo-neutrino flux in a continental location and another such detector in Hawaii to measure it in an oceanic location. The probability that only one of them is shadowed exceeds 50%, whereas the probability that at least one is shadowed is about 80%. We provide an online tool to calculate different shadowing probabilities for the one-and two-detector cases. Text South pole Unknown South Pole North Pole
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic supernova neutrinos
neutrino detectors ArXiv ePrint
astro-ph/0604300 c©2006 IOP Publishing Ltd and SISSA 1475-7516/06/05012+17$30.00
spellingShingle supernova neutrinos
neutrino detectors ArXiv ePrint
astro-ph/0604300 c©2006 IOP Publishing Ltd and SISSA 1475-7516/06/05012+17$30.00
A Mirizzi
G G Raffelt
P D Serpico
neutrinos: optimal detector locations
topic_facet supernova neutrinos
neutrino detectors ArXiv ePrint
astro-ph/0604300 c©2006 IOP Publishing Ltd and SISSA 1475-7516/06/05012+17$30.00
description Abstract. A model-independent experimental signature for flavour oscillations in the neutrino signal from the next Galactic supernova (SN) would be the observation of Earth matter effects. We calculate the probability for observing a Galactic SN shadowed by the Earth as a function of the detector’s geographic latitude. This probability depends only mildly on details of the Galactic SN distribution. A location at the North Pole would be optimal with a shadowing probability of about 60%, but a far-northern location such as Pyhäsalmi in Finland, the proposed site for a large-volume scintillator detector, is almost equivalent (58%). We also consider several pairs of detector locations and calculate the probability that only one of them is shadowed, allowing a comparison between a shadowed and a direct signal. For the South Pole combined with Kamioka, this probability is almost 75%; for the South Pole combined with Pyhäsalmi, it is almost 90%. One particular scenario consists of a large-volume scintillator detector located in Pyhäsalmi to measure the geo-neutrino flux in a continental location and another such detector in Hawaii to measure it in an oceanic location. The probability that only one of them is shadowed exceeds 50%, whereas the probability that at least one is shadowed is about 80%. We provide an online tool to calculate different shadowing probabilities for the one-and two-detector cases.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author A Mirizzi
G G Raffelt
P D Serpico
author_facet A Mirizzi
G G Raffelt
P D Serpico
author_sort A Mirizzi
title neutrinos: optimal detector locations
title_short neutrinos: optimal detector locations
title_full neutrinos: optimal detector locations
title_fullStr neutrinos: optimal detector locations
title_full_unstemmed neutrinos: optimal detector locations
title_sort neutrinos: optimal detector locations
publishDate 2006
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5075
http://wwwth.mpp.mpg.de/members/raffelt/mypapers/200601.pdf
geographic South Pole
North Pole
geographic_facet South Pole
North Pole
genre South pole
genre_facet South pole
op_source http://wwwth.mpp.mpg.de/members/raffelt/mypapers/200601.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.564.5075
http://wwwth.mpp.mpg.de/members/raffelt/mypapers/200601.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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