A corpuscular ray may be absorbed: A. with a definite range, or B~ more or less exponentially with an absorption coefficient. The experiments discussed seem to require mechanism B with x = 0.3 per meter water for primary cosmic rays of energy around 10 lยฐ volt in air, but mechanism A for the sameray
Results of the dutch cosmic ray expedition 1933: IX. The ionisation-balance for cosmic rays on the ocean
โ Scribed by J. Clay; M. Rutgers van der Loeff
- Publisher
- Elsevier Science
- Year
- 1936
- Weight
- 638 KB
- Volume
- 3
- Category
- Article
- ISSN
- 0031-8914
No coin nor oath required. For personal study only.
โฆ Synopsis
In the following pages the results are given of the measurements of the number and the average life of ions, and of the number of charged and uncharged condensation-nuclei in the air on the open sea.
The number of fast ions was constantly recorded with the aid of an E be r t-aspirator combined with an electrometer-triode. We watched the diurnal variation in Bandoeng, the influence of our approach to the coast, of fog and of rain and we tried to determine the mobility-spectrum. The average of all the measurements of ions caught in the aspirator was 213 ions per cc of air.
Following S c h wei die r's ,,~Iethod II" the "half-value voltage" was determined; as an average we find H = 0.80 Volt, corresponding to an average life .& = 63 sec.
. Calculation of the ionisation on the ocean from the balance (see preceding paper) gives as an average q = 2.0 J. in sufficient agreement with the value q between 1,8 and 2,1 J, due to cosmic radiation only.
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