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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_3_7</article-id><article-id custom-type="elpub" pub-id-type="custom">dpg-487</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>ARTICLES</subject></subj-group></article-categories><title-group><article-title>ЭФФЕКТ САДОВСКОГО</article-title><trans-title-group xml:lang="en"><trans-title>THE SADOVSKY EFFECT</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-1640-0522</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Адушкин</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Adushkin</surname><given-names>V. V.</given-names></name></name-alternatives><email xlink:type="simple">adushkin@idg.ras.ru</email><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 Geosphere 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>06</day><month>11</month><year>2024</year></pub-date><volume>16</volume><issue>3</issue><fpage>7</fpage><lpage>10</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Адушкин В.В., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Адушкин В.В.</copyright-holder><copyright-holder xml:lang="en">Adushkin V.V.</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/487">https://www.dyngeo.ru/jour/article/view/487</self-uri><abstract><p>На основе результатов физического моделирования рассмотрено взаимодействие воздушной ударной волны, вызванной приземным взрывом заряда ВВ, с теплым слоем. Показано, что наличие прогревного слоя обусловливает сильный эффект, связанный с качественным изменением эпюры давления в ударной волне, снижению амплитуды волны сжатия и увеличению ее длительности.</p></abstract><trans-abstract xml:lang="en"><p>Based on the results of physical modeling, the interaction of an air shock wave caused by a surface explosion of an explosive charge with a warm layer is considered. It is shown that the presence of a heating layer causes a strong effect associated with a qualitative change in the pressure diagram in the shock wave, a decrease in the amplitude of the compression wave and an increase in its duration.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>взрыв</kwd><kwd>ударная волна</kwd><kwd>амплитуда</kwd><kwd>длительность</kwd><kwd>нагретый слой</kwd><kwd>экспериментальные данные</kwd></kwd-group><kwd-group xml:lang="en"><kwd>explosion</kwd><kwd>shock wave</kwd><kwd>amplitude</kwd><kwd>duration</kwd><kwd>heated layer</kwd><kwd>experimental data</kwd></kwd-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>
