Search for high energy neutrino induced cascades with the AMANDA-B10 detector
Search for high energy neutrino induced cascades with the AMANDA-B10 detector
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使用 AMANDA-B10 探测器搜索高能中微子诱发级联
DOI:
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发表时间:
2002
期刊:
影响因子:
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通讯作者:
I. Jose
中科院分区:
文献类型:
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作者:
Toboada Fermin;I. Jose
SEARCH FOR HIGH ENERGY NEUTRINO INDUCED CASCADES WITH THE AMANDA-B10 DETECTOR Ignacio José Taboada Fermı́n Douglas F. Cowen 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 × 10 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