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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Computational nanotechnology</journal-id><journal-title-group><journal-title xml:lang="en">Computational nanotechnology</journal-title><trans-title-group xml:lang="kk"><trans-title>Computational nanotechnology</trans-title></trans-title-group><trans-title-group xml:lang="pt"><trans-title>Computational nanotechnology</trans-title></trans-title-group><trans-title-group xml:lang="ru"><trans-title>Computational nanotechnology</trans-title></trans-title-group><trans-title-group xml:lang="zh"><trans-title>Computational nanotechnology</trans-title></trans-title-group></journal-title-group><issn publication-format="print">2313-223X</issn><issn publication-format="electronic">2587-9693</issn><publisher><publisher-name xml:lang="en">YUR-VAK</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">529803</article-id><article-id pub-id-type="doi">10.33693/2313-223X-2020-7-3-72-76</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Articles</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Статьи</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">The mechanism of anomaly of charged particles before the earthquake</article-title><trans-title-group xml:lang="ru"><trans-title>Механизм аномалии заряженных частиц до землетрясения</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Rakhimov</surname><given-names>Rustam Kh.</given-names></name><name xml:lang="ru"><surname>Рахимов</surname><given-names>Рустам Хакимович</given-names></name></name-alternatives><bio xml:lang="en"><p>Dr. Sci. (Eng.); Head at the Laboratory No. 1</p></bio><bio xml:lang="ru"><p>доктор технических наук, профессор; зав. лабораторией № 1</p></bio><email>rustam-shsul@yandex.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Makhsudov</surname><given-names>Asatulla U.</given-names></name><name xml:lang="ru"><surname>Максудов</surname><given-names>Асатулла Урманович</given-names></name></name-alternatives><bio xml:lang="en"><p>senior researcher</p></bio><bio xml:lang="ru"><p>старший научный сотрудник</p></bio><email>asaduz50@rambler.ru</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Institute of Materials Science, SPA “Physics-Sun”, Academy of Science of Uzbekistan</institution></aff><aff><institution xml:lang="ru">Институт материаловедения Научно-производственного объединения «Физика-Солнце» Академии наук Республики Узбекистан</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2020-09-15" publication-format="electronic"><day>15</day><month>09</month><year>2020</year></pub-date><volume>7</volume><issue>3</issue><issue-title xml:lang="en">VOL 7, NO3 (2020)</issue-title><issue-title xml:lang="ru">ТОМ 7, №3 (2020)</issue-title><fpage>72</fpage><lpage>76</lpage><history><date date-type="received" iso-8601-date="2023-07-05"><day>05</day><month>07</month><year>2023</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2020, Yur-VAK</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2020, Юр-ВАК</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="en">Yur-VAK</copyright-holder><copyright-holder xml:lang="ru">Юр-ВАК</copyright-holder><ali:free_to_read xmlns:ali="http://www.niso.org/schemas/ali/1.0/"/><license><ali:license_ref xmlns:ali="http://www.niso.org/schemas/ali/1.0/">https://journals.eco-vector.com/2313-223X/about/editorialPolicies</ali:license_ref></license></permissions><self-uri xlink:href="https://journals.eco-vector.com/2313-223X/article/view/529803">https://journals.eco-vector.com/2313-223X/article/view/529803</self-uri><abstract xml:lang="en"><p>Some mechanisms are considered in the form of analysis of the propagation and origin of charged particles involved in acting forces in energy transfer processes that lead to a highly deformed seismically active state and create the necessary conditions for the occurrence of an earthquake. The results of monitoring the registration of charged particles of radioactive radiation of the earth’s crust for the purpose of earthquake forecasting are analyzed. During monitoring, responses to the origin of an event - an earthquake-are observed in the behavior of charged particles, which are located on remote parts of the earth’s crust relative to the place where charged particles are registered. In this case, wide horizons of the earth’s crust are involved, where tectonic disturbances are developed, covering not only the deep layers of the earth’s crust, but also the sections that appear in the upper parts. These tectonic disturbances can be considered as through-current channels that facilitate the transfer of energy from great depths. On the earth’s surface, the behavior of charged particles should be considered within the framework of the action of geomagnetic and atmospheric electricity fields. These fields at the earth’s surface are a carrier field that provides a special transfer of not only energy and matter. Thus, the propagation of charged particle flows over considerable distances from the epicenter of earthquakes can be caused by the carrier fields of deep change processes.</p></abstract><trans-abstract xml:lang="ru"><p>Рассмотрены некоторые механизмы в виде анализа распространения и происхождения заряженных частиц, участвующих в действующих сил в процессах по переносу энергии, приводящих в сейсмоактивное сильно деформированное состояние, и создающие необходимые условия возникновения землетрясения. Проанализированы результаты мониторинга по регистрации заряженных частиц радиоактивных излучений земной коры в целях прогнозирования землетрясений. При мониторинге, в поведении заряженных частиц наблюдаются отклики на происхождение события - землетрясения, которые находятся на удаленных частях земной коры относительно места регистрации заряженных частиц. В этом случае задействованы широкие горизонты земной коры, где развиты тектонические нарушения, охватывающие не только глубокие слои земной коры, но и проявляющихся в верхних частях разрезов. Эти тектонические нарушения можно рассматривать как сквозные токовые каналы, способствующие переносу энергии из больших глубин. На поверхности земли поведение заряженных частиц целесообразно рассматривать в рамках действия полей геомагнитного и атмосферного электричества. Указанные поля у земной поверхности являются несущим полем, которое обеспечивает особенный перенос не только энергии и вещества. Таким образом, распространение потоков заряженных частиц на значительные расстояния от эпицентра землетрясений, могут быть вызваны несущими полями процессов глубинных изменений.</p></trans-abstract><kwd-group xml:lang="en"><kwd>gas emissions</kwd><kwd>decay</kwd><kwd>intensity</kwd><kwd>nuclear interactions</kwd><kwd>charged particles</kwd><kwd>neutron flux</kwd><kwd>soliton</kwd><kwd>seismic activity</kwd><kwd>forecast</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>газовыделение</kwd><kwd>распад</kwd><kwd>интенсивность</kwd><kwd>ядерные взаимодействия</kwd><kwd>заряженные частицы</kwd><kwd>нейтронный поток</kwd><kwd>солитон</kwd><kwd>сейсмическая активность</kwd><kwd>прогноз</kwd></kwd-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Ginzburg V.L. Theoretical basis of astrophysics. Moscow, 1975. P. 355.</mixed-citation></ref><ref id="B2"><label>2.</label><mixed-citation>Ostapenko V.F., Zhusunov M.A., Krasnoperov V.A. et al. 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