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The surface detector array of the Pierre Auger Observatory can detect neutrinos with energy E-nu between 10(17) eV and 10(20) eV from point-like sources across the sky south of +55 degrees and north of -65 degrees declinations. A search has been performed for highly inclined extensive air showers produced by the interaction of neutrinos of all flavors in the atmosphere (downward-going neutrinos), and by the decay of tau leptons originating from tau neutrino interactions in Earth's crust (Earth-skimming neutrinos). No candidate neutrinos have been found in data up to 2010 May 31. This corresponds to an equivalent exposure of similar to 3.5 years of a full surface detector array for the Earth-skimming channel and similar to 2 years for the downward-going channel. An improved upper limit on the diffuse flux of tau neutrinos has been derived. Upper limits on the neutrino flux from point-like sources have been derived as a function of the source declination. Assuming a differential neutrino flux k(PS) . E-nu(-2). from a point-like source, 90% confidence level upper limits for k(PS) at the level of approximate to 5x10(-7) and 2.5x10(-6) GeV cm(-2) s(-1) have been obtained over a broad range of declinations from the searches for Earth-skimming and downward-going neutrinos, respectively. RI Petrolini, Alessandro/H-3782-2011; Albuquerque, Ivone/H-4645-2012; Chinellato, Carola Dobrigkeit /F-2540-2011; Muller, Marcio Aparecido/H-9112-2012; D'Urso, Domenico/I-5325-2012; Badescu, Alina/B-6087-2012; Bleve, Carla/J-2521-2012; martello, daniele/J-3131-2012; Valino, Ines/J-8324-2012; Brogueira, Pedro/K-3868-2012; de souza, Vitor/D-1381-2012; Alves Batista, Rafael/K-6642-2012; Chinellato, Jose Augusto/I-7972-2012; Yushkov, Alexey/A-6958-2013; Falcke, Heino/H-5262-2012; Beatty, James/D-9310-2011; Ebr, Jan/H-8319-2012; Anjos, Joao/C-8335-2013; Fauth, Anderson/F-9570-2012; Sarkar, Subir/G-5978-2011; Caramete, Laurentiu/C-2328-2011 OI D'Urso, Domenico/0000-0002-8215-4542; Brogueira, Pedro/0000-0001-6069-4073; Falcke, Heino/0000-0002-2526-6724; Ebr, Jan/0000-0001-8807-6162; Sarkar, Subir/0000-0002-3542-858X;
The surface detector array of the Pierre Auger Observatory can detect neutrinos with energy E ν between 1017 eV and 1020 eV from point-like sources across the sky south of +55° and north of -65° declinations. A search has been performed for highly inclined extensive air showers produced by the interaction of neutrinos of all flavors in the atmosphere (downward-going neutrinos), and by the decay of tau leptons originating from tau neutrino interactions in Earth's crust (Earth-skimming neutrinos). No candidate neutrinos have been found in data up to 2010 May 31. This corresponds to an equivalent exposure of ~3.5 years of a full surface detector array for the Earth-skimming channel and ~2 years for the downward-going channel. An improved upper limit on the diffuse flux of tau neutrinos has been derived. Upper limits on the neutrino flux from point-like sources have been derived as a function of the source declination. Assuming a differential neutrino flux k PS · E -2 ν from a point-like source, 90% confidence level upper limits for k PS at the level of ≈5 × 10-7 and 2.5 × 10-6 GeV cm-2 s-1 have been obtained over a broad range of declinations from the searches for Earth-skimming and downward-going neutrinos, respectively.
Search for Point-like Sources of Ultra-high Energy Neutrinos at the Pierre Auger Observatory and Improved Limit on the Diffuse Flux of Tau Neutrinos
The Pierre Auger Collaboration;Abreu P;Aglietta M;Ahlers M;Ahn E. J;Albuquerque I. F. M;Allard D;Allekotte I;Allen J;Allison P;Almela A;Alvarez Castillo J;Alvarez Muñiz J;Alves Batista R;Ambrosio M;Aminaei A;Anchordoqui L;Andringa S;Antiči'c T;Aramo C;Arganda E;Arqueros F;Asorey H;Assis P;Aublin J;Ave M;Avenier M;Avila G;Badescu A. M;Balzer M;Barber K. B;Barbosa A. F;Bardenet R;Barroso S. L. C;Baughman B;Bäuml J;Baus C;Beatty J. J;Becker K. H;Bellétoile A;Bellido J. A;BenZvi S;Berat C;Bertou X;Biermann P. L;Billoir P;Blanch Bigas O;Blanco F;Blanco M;Bleve C;Blümer H;Boháčová M;Boncioli D;Bonifazi C;Bonino R;Borodai N;Brack J;Brancus I;Brogueira P;Brown W. C;Bruijn R;Buchholz P;Bueno A;Buroker L;Burton R. E;Caballero Mora K. S;Caccianiga B;Caramete L;CARUSO, ROSSELLA;Castellina A;Catalano O;Cataldi G;Cazon L;Cester R;Chauvin J;Cheng S. H;Chiavassa A;Chinellato J. A;Chirinos Diaz J;Chudoba J;Cilmo M;Clay R. W;Cocciolo G;Collica L;Coluccia M. R;Conceição R;Contreras F;Cook H;Cooper M. J;Coppens J;Cordier A;Coutu S;Covault C. E;Creusot A;Criss A;Cronin J;Curutiu A;Dagoret Campagne S;Dallier R;Daniel B;Dasso S;Daumiller K;Dawson B. R;de Almeida R. M;De Domenico M;De Donato C;de Jong S. J;De La Vega G;de Mello Junior W. J. M;de Mello Neto J. R. T;De Mitri I;de Souza V;de Vries K. D;del Peral L;del Río M;Deligny O;Dembinski H;Dhital N;Di Giulio C;Díaz Castro M. L;Diep P. N;Diogo F;Dobrigkeit C;Docters W;D'Olivo J. C;Dong P. N;Dorofeev A;dos Anjos J. C;Dova M. T;D'Urso D;Dutan I;Ebr J;Engel R;Erdmann M;Escobar C. O;Espadanal J;Etchegoyen A;Facal San Luis P;Falcke H;Farrar G;Fauth A. C;Fazzini N;Ferguson A. P;Fick B;Figueira J. M;Filevich A;Filipčič A;Fliescher S;Fracchiolla C. E;Fraenkel E. D;Fratu O;Fröhlich U;Fuchs B;Gaior R;Gamarra R. F;Gambetta S;García B;Garcia Roca S. T;Garcia Gamez D;Garcia Pinto D;Gascon Bravo A;Gemmeke H;Ghia P. L;Giller M;Gitto J;Glass H;Gold M. S;Golup G;Gomez Albarracin F;Gómez Berisso M;Gómez Vitale P. F;Gonçalves P;Gonzalez J. G;Gookin B;Gorgi A;Gouffon P;Grashorn E;Grebe S;Griffith N;Grigat M;Grillo A. F;Guardincerri Y;Guarino F;Guedes G. P;Hansen P;Harari D;Harrison T. A;Harton J. L;Haungs A;Hebbeker T;Heck D;Herve A. E;Hojvat C;Hollon N;Holmes V. C;Homola P;Hörandel J. R;Horvath P;Hrabovský M;Huber D;Huege T;INSOLIA, Antonio;Ionita F;Italiano A;Jansen S;Jarne C;Jiraskova S;Josebachuili M;Kadija K;Kampert K. H;Karhan P;Kasper P;Katkov I;Kégl B;Keilhauer B;Keivani A;Kelley J. L;Kemp E;Kieckhafer R. M;Klages H. O;Kleifges M;Kleinfeller J;Knapp J;Koang D. H;Kotera K;Krohm N;Krömer O;Kruppke Hansen D;Kuempel D;Kulbartz J. K;Kunka N;La Rosa G;Lachaud C;LaHurd D;Latronico L;Lauer R;Lautridou P;Le Coz S;Leão M. S. A. B;Lebrun D;Lebrun P;Leigui de Oliveira M. A;Letessier Selvon A;Lhenry Yvon I;Link K;López R;Lopez Agüera A;Louedec K;Lozano Bahilo J;Lu L;Lucero A;Ludwig M;Lyberis H;Maccarone M. C;Macolino C;Maldera S;Maller J;Mandat D;Mantsch P;Mariazzi A. G;Marin J;Marin V;Maris I. C;Marquez Falcon H. R;Marsella G;Martello D;Martin L;Martinez H;Martínez Bravo O;Martraire D;Masías Meza J. J;Mathes H. J;Matthews J;Matthews J. A. J;Matthiae G;Maurel D;Maurizio D;Mazur P. O;Medina Tanco G;Melissas M;Melo D;Menichetti E;Menshikov A;Mertsch P;Meurer C;Meyhandan R;Mi'canovi'c S;Micheletti M. I;Minaya I. A;Miramonti L;Molina Bueno L;Mollerach S;Monasor M;Monnier Ragaigne D;Montanet F;Morales B;Morello C;Moreno E;Moreno J. C;Mostafá M;Moura C. A;Muller M. A;Müller G;Münchmeyer M;Mussa R;Navarra G;Navarro J. L;Navas S;Necesal P;Nellen L;Nelles A;Neuser J;Nhung P. T;Niechciol M;Niemietz L;Nierstenhoefer N;Nitz D;Nosek D;Nožka L;Oehlschläger J;Olinto A;Ortiz M;Pacheco N;Pakk Selmi Dei D;Palatka M;Pallotta J;Palmieri N;Parente G;Parizot E;Parra A;Pastor S;Paul T;Pech M;Peķala J;Pelayo R;Pepe I. M;Perrone L;Pesce R;Petermann E;Petrera S;Petrolini A;Petrov Y;Pfendner C;Piegaia R;Pierog T;Pieroni P;Pimenta M;PIRRONELLO, Valerio;Platino M;Plum M;Ponce V. H;Pontz M;Porcelli A;Privitera P;Prouza M;Quel E. J;Querchfeld S;Rautenberg J;Ravel O;Ravignani D;Revenu B;Ridky J;Riggi S;Risse M;Ristori P;Rivera H;Rizi V;Roberts J;Rodrigues de Carvalho W;Rodriguez G;Rodriguez Cabo I;Rodriguez Martino J;Rodriguez Rojo J;Rodríguez Frías M. D;Ros G;Rosado J;Rossler T;Roth M;Rouillé d'Orfeuil B;Roulet E;Rovero A. C;Rühle C;Saftoiu A;Salamida F;Salazar H;Salesa Greus F;Salina G;Sánchez F;Santo C. E;Santos E;Santos E. M;Sarazin F;Sarkar B;Sarkar S;Sato R;Scharf N;Scherini V;Schieler H;Schiffer P;Schmidt A;Scholten O;Schoorlemmer H;Schovancova J;Schovánek P;Schröder F;Schulte S;Schuster D;Sciutto S. J;Scuderi M;Segreto A;Settimo M;Shadkam A;Shellard R. C;Sidelnik I;Sigl G;Silva Lopez H. H;Sima O;'Smiałkowski A;Šmída R;Snow G. R;Sommers P;Sorokin J;Spinka H;Squartini R;Srivastava Y. N;Stanic S;Stapleton J;Stasielak J;Stephan M;Stutz A;Suarez F;Suomijärvi T;Supanitsky A. D;Šuša T;Sutherland M. S;Swain J;Szadkowski Z;Szuba M;Tapia A;Tartare M;Taşcău O;Tcaciuc R;Thao N. T;Thomas D;Tiffenberg J;Timmermans C;Tkaczyk W;Todero Peixoto C. J;Toma G;Tomankova L;Tomé B;Tonachini A;Travnicek P;Tridapalli D. B;Tristram G;Trovato E;Tueros M;Ulrich R;Unger M;Urban M;Valdés Galicia J. F;Valiño I;Valore L;van Aar G;van den Berg A. M;van Vliet A;Varela E;Vargas Cárdenas B;Vázquez J. R;Vázquez R. A;Veberič D;Verzi V;Vicha J;Videla M;Villaseñor L;Wahlberg H;Wahrlich P;Wainberg O;Walz D;Watson A. A;Weber M;Weidenhaupt K;Weindl A;Werner F;Westerhoff S;Whelan B. J;Widom A;Wieczorek G;Wiencke L;Wilczyńska B;Wilczyński H;Will M;Williams C;Winchen T;Wommer M;Wundheiler B;Yamamoto T;Yapici T;Younk P;Yuan G;Yushkov A;Zamorano Garcia B;Zas E;Zavrtanik D;Zavrtanik M;Zaw I;Zepeda A;Zhou J;Zhu Y;Zimbres Silva M;Ziolkowski M.
2012-01-01
Abstract
The surface detector array of the Pierre Auger Observatory can detect neutrinos with energy E-nu between 10(17) eV and 10(20) eV from point-like sources across the sky south of +55 degrees and north of -65 degrees declinations. A search has been performed for highly inclined extensive air showers produced by the interaction of neutrinos of all flavors in the atmosphere (downward-going neutrinos), and by the decay of tau leptons originating from tau neutrino interactions in Earth's crust (Earth-skimming neutrinos). No candidate neutrinos have been found in data up to 2010 May 31. This corresponds to an equivalent exposure of similar to 3.5 years of a full surface detector array for the Earth-skimming channel and similar to 2 years for the downward-going channel. An improved upper limit on the diffuse flux of tau neutrinos has been derived. Upper limits on the neutrino flux from point-like sources have been derived as a function of the source declination. Assuming a differential neutrino flux k(PS) . E-nu(-2). from a point-like source, 90% confidence level upper limits for k(PS) at the level of approximate to 5x10(-7) and 2.5x10(-6) GeV cm(-2) s(-1) have been obtained over a broad range of declinations from the searches for Earth-skimming and downward-going neutrinos, respectively. RI Petrolini, Alessandro/H-3782-2011; Albuquerque, Ivone/H-4645-2012; Chinellato, Carola Dobrigkeit /F-2540-2011; Muller, Marcio Aparecido/H-9112-2012; D'Urso, Domenico/I-5325-2012; Badescu, Alina/B-6087-2012; Bleve, Carla/J-2521-2012; martello, daniele/J-3131-2012; Valino, Ines/J-8324-2012; Brogueira, Pedro/K-3868-2012; de souza, Vitor/D-1381-2012; Alves Batista, Rafael/K-6642-2012; Chinellato, Jose Augusto/I-7972-2012; Yushkov, Alexey/A-6958-2013; Falcke, Heino/H-5262-2012; Beatty, James/D-9310-2011; Ebr, Jan/H-8319-2012; Anjos, Joao/C-8335-2013; Fauth, Anderson/F-9570-2012; Sarkar, Subir/G-5978-2011; Caramete, Laurentiu/C-2328-2011 OI D'Urso, Domenico/0000-0002-8215-4542; Brogueira, Pedro/0000-0001-6069-4073; Falcke, Heino/0000-0002-2526-6724; Ebr, Jan/0000-0001-8807-6162; Sarkar, Subir/0000-0002-3542-858X;
The surface detector array of the Pierre Auger Observatory can detect neutrinos with energy E ν between 1017 eV and 1020 eV from point-like sources across the sky south of +55° and north of -65° declinations. A search has been performed for highly inclined extensive air showers produced by the interaction of neutrinos of all flavors in the atmosphere (downward-going neutrinos), and by the decay of tau leptons originating from tau neutrino interactions in Earth's crust (Earth-skimming neutrinos). No candidate neutrinos have been found in data up to 2010 May 31. This corresponds to an equivalent exposure of ~3.5 years of a full surface detector array for the Earth-skimming channel and ~2 years for the downward-going channel. An improved upper limit on the diffuse flux of tau neutrinos has been derived. Upper limits on the neutrino flux from point-like sources have been derived as a function of the source declination. Assuming a differential neutrino flux k PS · E -2 ν from a point-like source, 90% confidence level upper limits for k PS at the level of ≈5 × 10-7 and 2.5 × 10-6 GeV cm-2 s-1 have been obtained over a broad range of declinations from the searches for Earth-skimming and downward-going neutrinos, respectively.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.11769/35135
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