title: ÐÐ»Ð¸ÑÐ½Ð¸Ðµ Ð¼Ð°Ð³Ð½Ð¸ÑÐ½Ð¾Ð³Ð¾ Ð¿Ð¾Ð»Ñ ÐÐµÐ¼Ð»Ð¸ Ð½Ð° Ð³ÐµÐ½ÐµÑÐ°ÑÐ¸Ñ ÑÐ°Ð´Ð¸Ð¾Ð¸Ð·Ð¾ÑÐ¾Ð¿Ð¾Ð² Ð² Ð°ÑÐ¼Ð¾ÑÑÐµÑÐµ
title: Ð²ÑÐ¿ÑÑÐºÐ½Ð°Ñ ÐºÐ²Ð°Ð»Ð¸ÑÐ¸ÐºÐ°ÑÐ¸Ð¾Ð½Ð½Ð°Ñ ÑÐ°Ð±Ð¾ÑÐ° Ð±Ð°ÐºÐ°Ð»Ð°Ð²ÑÐ°
titleType: Subtitle
title: Influence of the Earth's magnetic field on the production of radioisotopes in the atmosphere.
Creators: name: ÐÐ°ÑÑÑÐ½Ð¾Ð²Ð°, ÐÐ½Ð½Ð°
Publisher: name: Ð¡Ð°Ð½ÐºÑ-ÐÐµÑÐµÑÐ±ÑÑÐ³ÑÐºÐ¸Ð¹ Ð¿Ð¾Ð»Ð¸ÑÐµÑÐ½Ð¸ÑÐµÑÐºÐ¸Ð¹ ÑÐ½Ð¸Ð²ÐµÑÑÐ¸ÑÐµÑ ÐÐµÑÑÐ° ÐÐµÐ»Ð¸ÐºÐ¾Ð³Ð¾
Year: 2022
Subjects: ÑÐ°Ð´Ð¸Ð¾ÑÐ³Ð»ÐµÑÐ¾Ð´
ÐºÐ¾ÑÐ¼Ð¸ÑÐµÑÐºÐ¸Ðµ Ð»ÑÑÐ¸
Ð´Ð¸Ð¿Ð¾Ð»ÑÐ½ÑÐ¹ Ð¼Ð°Ð³Ð½Ð¸ÑÐ½ÑÐ¹ Ð¼Ð¾Ð¼ÐµÐ½Ñ
Ð¿Ð¾ÑÐµÐ½ÑÐ¸Ð°Ð» Ð¼Ð¾Ð´ÑÐ»ÑÑÐ¸Ð¸
ÑÐºÐ¾ÑÐ¾ÑÑÑ Ð¾Ð±ÑÐ°Ð·Ð¾Ð²Ð°Ð½Ð¸Ñ ÑÐ°Ð´Ð¸Ð¾ÑÐ³Ð»ÐµÑÐ¾Ð´Ð°
radiocarbon
cosmic rays
dipole magnetic moment
modulation potential
radiocarbon formation rate

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description: The subject of the graduate qualification work is âInfluence of the Earth's magnetic field on radioisotope production in the atmosphere". The given work is devoted to studying the impact of the Earthâs geomagnetic field at different periods of time on rate of formation of 14C isotope in the atmosphere of the Earth. The influence of the modulation potential on radiocarbon generation in the atmosphere was also considered. The spectra of primary cosmic ray particles were examined and calculated, the yield function was constructed, and the necessary approximations were made. From these data the radiocarbon production rate was calculated. The influence of the ratio of the Earth's magnetic field moments was also explored as well as the impact of modulation potential.As a result of this work, it was shown that in fact the largest influence of the modulation potential on the isotope production rate can be observed at lower altitudes, and an approximation system was tested with which the result was obtained in good agreement with other values of rate. The global radiocarbon production rates were obtained and their dependence on different values of the magnetic moment was investigated. This work has both theoretical and practical importance. The results of the work may be used for further investigation and modelling of the processes in the atmosphere as well as for radiocarbon dating methods and for characterization of a historical processes.