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SPECTRUM AND ISOTROPY OF EAS

Journal Article · · J. Phys. Soc. Japan
OSTI ID:4764025
The number spectrum of EAS has been found to extend to showers of more than 10/sup 10/ particles without noticeable increase in steepness. The logarithmic slope has some uncertainty because of an unknown variation of lateral distribution near the axis with shower size; the corrected value of gamma is about 1.7 for 6 x 10/sup 6/ < N < 6 x 10/sup 9/ particles. Assuming a lateral distribution corresponding to an age parameter s = 1, the largest shower recorded had 2 6 x 10/sup 10/ particles. Large showers (N > 10/sup 7/) seem to exhibit substantial anisotropy, but the statistical significance of this observation is not very great. The persistent feature is a pronounced minimum around 15 hours local sidereal time. In the showers of 5 x 10/sup 6/ < N < 10/sup 8/ such a minimum appeared associated with a large second harmonic (17%) in the Fourier amplitudes, while in the showers of N > 10/sup 8/ this minimum appeared to be associated with a large first harmonic (35%). A minimum in the third quadrant also appears in the MIT Agassiz data for showers of N > 10/sup 8/, and in the MIT Volcano Ranch data, as well as in Japanese data on mu rich'' showers, mu - less'' showers, and multiple penetrating particles observed underground. Fourier analysis of the frequencies of smaller showers reveals no second harmonics, but a possibly significant first harmonic of amplitude about 0.4% with maxima in the range 13 to 20 hours local sidereal time, for EAS of 10/sup 4/ < N < 10/sup 6/ particles. Because of the complexity of solar periodic atmospheric effects on EAS, this apparent anisotropy of the primaries may be spurious; but is is suspicious that many experimenters in different places on the earth have found maxima at approximately the same local sidereal time, both in the rates of small EAS and in the background cosmic-ray intensity. (auth)
Research Organization:
Cornell Univ., Ithaca, N.Y.
NSA Number:
NSA-17-013021
OSTI ID:
4764025
Journal Information:
J. Phys. Soc. Japan, Journal Name: J. Phys. Soc. Japan Vol. Vol: 17: Suppl. A-III
Country of Publication:
Country unknown/Code not available
Language:
English

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