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- W2059392919 abstract "Meson intensity has been recorded by using a triple-coincidence arrangement with a lead absorber 25 cm. thick between the counters. The comparison of daily mean values with the height of a number of pressure-levels has led us to take into consideration the temperature of the air layer between 200 and 100 mb. The results show that this temperature appears to be a factor closely controlling the meson intensity at the surface of the earth; the intensity increases with increasing temperature at the rate of 0.12% per °C. Other factors in determining the intensity are the mass of air and the height of the 100 mb. level over the station. The corresponding coefficients of absorption and decay prove to be comparable with those obtained from other measurements for mesons of the same momentum. It has also been found that the coexistence of the three effects permits explanation of the variability exhibited by the barometric coefficient when evaluated from short periods of observations. These results may therefore be taken as evidence that the bulk of mesons is produced at the height of 100 mb. If the positive effect of temperature is interpreted as the result of processes of decay and interactions with air nuclei of π-mesons at the production level, then the coefficient 0.12% per °C. leads to a value of 4.9×10-8 sec. for the upper limit of the mean life of π-mesons." @default.
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- W2059392919 date "1949-11-01" @default.
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- W2059392919 title "The Meson Intensity at the Surface of the Earth and the Temperature at the Production Level" @default.
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- W2059392919 doi "https://doi.org/10.1088/0370-1298/62/11/302" @default.
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