Experimental determination of the muon range–energy relation

1968 ◽  
Vol 46 (10) ◽  
pp. S332-S336 ◽  
Author(s):  
W. R. Sheldon ◽  
N. M. Duller

Calculations of the zenithal distribution of cosmic-ray muons indicate the appearance of peaks at near-horizontal directions in the relative muon intensity I(θ)/I0 for Eμ > a few tens of GeV. The magnitude of the peak value of I(θ)/I0 increases monotonically with energy, representative values being 1.15 for Eμ > 50 GeV and 1.58 for Eμ > 120 GeV. Using this phenomenon, an independent evaluation can be made of the muon range–energy relation. Absolute measurements of the muon flux underground at zenith angles of 69° to 77° are compared to the calculated zenithal distribution to determine the muon range–energy relation in rock at 25–100 GeV. Suggestions are advanced for extending the energy range to a few thousand GeV and for making a purely experimental determination by utilizing magnetic spectrometer results in a context which would avoid the need to normalize the spectrometer data and would largely eliminate the problem of possible energy bias. The usefulness of these data in determining the pion attenuation length in the atmosphere is discussed.

2016 ◽  
Vol 49 (5) ◽  
pp. 464-468
Author(s):  
Paul M. Dietrich ◽  
Dieter Treu ◽  
Henryk Kalbe ◽  
Michael Krumrey ◽  
Thomas Gross ◽  
...  

2011 ◽  
Vol 605 (9-10) ◽  
pp. 878-882 ◽  
Author(s):  
Tina Graber ◽  
Frank Forster ◽  
Achim Schöll ◽  
Friedrich Reinert

2015 ◽  
Vol 1 (2) ◽  
pp. 91-96 ◽  
Author(s):  
Василий Кузьменко ◽  
Vasiliy Kuzmenko ◽  
Валерий Янчуковский ◽  
Valery Yanchukovsky

When studying variations of cosmic ray intensity, by the use of muon telescopes located deep in the atmosphere it is necessary to take into account changes in atmospheric parameters, mainly pressure and temperature. The density distribution of temperature coefficients of the atmosphere muon intensity needs to be estimated from observations. To this purpose, the method of principal components regression and meth-ods of projection to latent structures (PLS-1 and PLS-2). We used data of continuous recording of muons, as well as Novosibirsk 2004–2010 aerological data. As shown by comparing results, PLS-2 method allows us to esti-mate the density distribution of muon intensity temperature coefficients with minimal errors.


1999 ◽  
Vol 96 (6) ◽  
pp. 1111-1116 ◽  
Author(s):  
E. Falcon ◽  
S. Fauve ◽  
C. Laroche

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