1992
DOI: 10.1103/physrevlett.69.1010
|View full text |Cite
|
Sign up to set email alerts
|

Search for muon neutrino oscillations with the Irvine-Michigan-Brookhaven detector

Abstract: Muon neutrinos produced as a result of cosmic-ray interactions with the atmosphere are used to search for v^ oscillations into v z by comparing the measured rate of upward-going muons in the Irvine-Michigan-Brookhaven detector with the expected rate. In addition, the ratio of upward-going muons which stop in the detector to those which exit is used to search for deviations from the expected spectrum. This latter technique is free of flux and cross-section normalization uncertainties. No evidence for oscillatio… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

6
88
0

Year Published

1994
1994
2009
2009

Publication Types

Select...
5
4
1

Relationship

0
10

Authors

Journals

citations
Cited by 125 publications
(94 citation statements)
references
References 17 publications
6
88
0
Order By: Relevance
“…Recent detectors [241] are divided into two classes: water Cherenkov detectors where the neutrino target is a large volume of water surveyed by a huge array of photomultiplier tubes sitting on the surface of the volume (the Kamiokande [49,242,243], SuperKamiokande [2] and IMB [50,244,245] collaborations) and iron plate calorimeters where neutrino-induced charged particles ionize the gas between the plates and the particle paths are reconstructed electronically (the Fréjus [246], NUSEX [247] and Soudan-2 [51] collaborations). In contrast to the early detectors the recent detectors are sensitive to the direction of tracks and can thus distinguish between up and down through-going tracks.…”
Section: Experiments With Atmospheric Neutrinosmentioning
confidence: 99%
“…Recent detectors [241] are divided into two classes: water Cherenkov detectors where the neutrino target is a large volume of water surveyed by a huge array of photomultiplier tubes sitting on the surface of the volume (the Kamiokande [49,242,243], SuperKamiokande [2] and IMB [50,244,245] collaborations) and iron plate calorimeters where neutrino-induced charged particles ionize the gas between the plates and the particle paths are reconstructed electronically (the Fréjus [246], NUSEX [247] and Soudan-2 [51] collaborations). In contrast to the early detectors the recent detectors are sensitive to the direction of tracks and can thus distinguish between up and down through-going tracks.…”
Section: Experiments With Atmospheric Neutrinosmentioning
confidence: 99%
“…The atmospheric neutrino anomaly was discovered in the late 1980s in the Kamiokande [34] and IMB [35] experiments. In 1998 the Super-Kamiokande experiment found a model independent evidence of muon (anti)neutrino disappearance in atmospheric neutrino data [36].…”
Section: Phenomenologymentioning
confidence: 99%
“…One should also note that the IMB collaboration has in the past measured a stopping/passing ratio for upward-going muons in agreement with a no oscillation Montecarlo prediction [28] (see [29] for a critical analysis).…”
Section: Discussionmentioning
confidence: 92%