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Figure 3.41: Differential momentum spectra of muons at sea level for different zenith angles, 9. The ordinate is multiplied by the momentum to the third power to compress the spectra. In addition, the spectra had been divided by the scale factors, as indicated, to shift the successive curves downward for better presentation. Thus, the reading at the ordinate for a given point on a curve must be multiplied by the appropriate scale factor to get the true intensity. (Carstensen 1978, Allkofer et al. 1978b, c, Allkofer 1979b).

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