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<article article-type="research-article" dtd-version="1.3" 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" xml:lang="ru"><front><journal-meta><journal-id journal-id-type="publisher-id">dpg</journal-id><journal-title-group><journal-title xml:lang="ru">Динамические процессы в геосферах</journal-title><trans-title-group xml:lang="en"><trans-title>Dynamic Processes in Geospheres</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2222-8535</issn><issn pub-type="epub">2949-0995</issn><publisher><publisher-name>ИДГ РАН</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.26006/29490995_2024_16_1_8</article-id><article-id custom-type="elpub" pub-id-type="custom">dpg-186</article-id><article-categories><subj-group subj-group-type="heading"><subject>Research Article</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>ЭЛЕКТРОДИНАМИЧЕСКИЕ ПРОЦЕССЫ В ГЕОСФЕРАХ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>ELECTRODYNAMIC PROCESSES IN GEOSPHERES</subject></subj-group></article-categories><title-group><article-title>МОНИТОРИНГ УРОВНЯ ИНФРАЗВУКОВОГО ФОНА В Г. ГУБКИН БЕЛГОРОДСКОЙ ОБЛАСТИ</article-title><trans-title-group xml:lang="en"><trans-title>MONITORING OF THE INFRASOUND BACKGROUND LEVEL IN GUBKIN, BELGOROD REGION</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-4387-2733</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Рыбнов</surname><given-names>Ю. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Rybnov</surname><given-names>Yu. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Старший научный сотрудник</p></bio><email xlink:type="simple">rybnov.y@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-3267-2851</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Соловьев</surname><given-names>С. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Soloviev</surname><given-names>S. P.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7102-6353</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Крашенинников</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Krasheninnikov</surname><given-names>A. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-2970-8363</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Рыбнов</surname><given-names>С. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Rybnov</surname><given-names>S. Yu.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт динамики геосфер имени академика М.А. Садовского РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Sadovsky Institute of Geospheres Dynamics of Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>13</day><month>05</month><year>2024</year></pub-date><volume>16</volume><issue>1</issue><fpage>8</fpage><lpage>14</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Рыбнов Ю.С., Соловьев С.П., Крашенинников А.В., Рыбнов С.Ю., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Рыбнов Ю.С., Соловьев С.П., Крашенинников А.В., Рыбнов С.Ю.</copyright-holder><copyright-holder xml:lang="en">Rybnov Y.S., Soloviev S.P., Krasheninnikov A.V., Rybnov S.Y.</copyright-holder><license xml:lang="ru" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>Данная работа распространяется под лицензией Creative Commons Attribution 4.0.</license-p></license><license xml:lang="en" license-type="creative-commons-attribution" xlink:href="https://creativecommons.org/licenses/by/4.0/" xlink:type="simple"><license-p>This work is licensed under a Creative Commons Attribution 4.0 License.</license-p></license></permissions><self-uri xlink:href="https://www.dyngeo.ru/jour/article/view/186">https://www.dyngeo.ru/jour/article/view/186</self-uri><abstract><p>Описаны инструментальные наблюдения за уровнем инфразвукового фона в полосе частот 1–20 Гц от работающей техники при вывозе руды из карьеров Лебединского и Стойленского ГОКов. Ежедневно в карьерах работают более 130 единиц основной горной техники, которые являются источником интенсивных инфразвуковых колебаний. Измерения проводились в период с июня по октябрь 2022 и 2023 гг. Проведенные исследования показали, что увеличение количества массовых взрывов в 2023 г. и, как следствие, интенсификация вывоза руды, привело к возрастанию инфразвукового фона на 4–9 дБ по сравнению с 2022 г. Однако его значение не превышает предельно допустимые уровни для территории жилой застройки 75÷90 дБ.</p></abstract><trans-abstract xml:lang="en"><p>Instrumental observations of the level of the infrasound background in the frequency band of 1–20 Hz from working equipment during the export of ore from the Lebedinsky and Stoilensky quarries are described. More than 130 units of basic mining equipment operate in the quarries every day, which are a source of intense infrasound vibrations. The measurements were carried out between June and October 2022 and 2023. The conducted studies have shown that an increase in the number of mass explosions in 2023 and, as a result, the intensification of ore export, led to an increase in the infrasound background by 4–9 dB compared to 2022. However, its value does not exceed the maximum permissible levels for residential areas of 75–90 dB.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>работающая техника</kwd><kwd>уровень инфразвукового фона</kwd></kwd-group><kwd-group xml:lang="en"><kwd>working equipment</kwd><kwd>the level of infrasound background</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследования выполнены в рамках государственного задания Министерства науки и высшего образования РФ (тема № 122032900185-5)</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
