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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">Fluid Dynamics</journal-id><journal-title-group><journal-title xml:lang="en">Fluid Dynamics</journal-title><trans-title-group xml:lang="ru"><trans-title>Известия Российской академии наук. Механика жидкости и газа</trans-title></trans-title-group></journal-title-group><issn publication-format="print">1024-7084</issn><issn publication-format="electronic">3034-5340</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">682520</article-id><article-id pub-id-type="doi">10.31857/S1024708424040041</article-id><article-id pub-id-type="edn">OYQTTI</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">Distinctive features of propagation of a turbulent pulsed gas-droplet eddy cloud</article-title><trans-title-group xml:lang="ru"><trans-title>Особенности распространения газокапельного турбулентного импульсного вихревого облака</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Pakhomov</surname><given-names>M. A.</given-names></name><name xml:lang="ru"><surname>Пахомов</surname><given-names>М. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>pma41976@yandex.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Terekhov</surname><given-names>V. P.</given-names></name><name xml:lang="ru"><surname>Терехов</surname><given-names>В. И.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>terekhov@itp.nsc.ru</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Kutateladze Institute of Thermophysics, Russian Academy of Sciences, Siberian Branch</institution></aff><aff><institution xml:lang="ru">Институт теплофизики им. С. С. Кутателадзе СО РАН</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2024-11-11" publication-format="electronic"><day>11</day><month>11</month><year>2024</year></pub-date><issue>4</issue><fpage>55</fpage><lpage>68</lpage><history><date date-type="received" iso-8601-date="2025-06-04"><day>04</day><month>06</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2024, Russian Academy of Sciences</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2024, Российская академия наук</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="en">Russian Academy of Sciences</copyright-holder><copyright-holder xml:lang="ru">Российская академия наук</copyright-holder></permissions><self-uri xlink:href="https://journals.eco-vector.com/1024-7084/article/view/682520">https://journals.eco-vector.com/1024-7084/article/view/682520</self-uri><abstract xml:lang="en"><p>We present the results of the numerical modeling of the formation and motion of a blown solitary pulsed turbulent gas-droplet jet under the conditions approximately corresponding to human cough. The calculations are performed for the pulse duration <italic>t</italic> = 0.6 s and the greatest velocity of the gas phase of 20 m/s at the mass content of droplets <italic>M</italic><sub>L1</sub> = 1%. The drop phase in the exit section is monodisperse, while the initial dimension of particles in the calculations varied in the range <italic>D</italic><sub>1</sub> = 5‒30 μm. Two zones of elevated vorticity are formed within the cloud in the initial period of motion. They are situated in the mixing layer and in the region of deceleration of two-phase pulsed jet. The greatest levels of the longitudinal velocity and the kinetic energy of turbulence are attained in the interval of pulse blow-off. At the subsequent moments of time the turbulence velocity and level monotonically decrease. The vortex cloud produced by the solitary pulse exists for a fairly long time (<italic>t</italic> ≈ 4 s) and has a time to penetrate into the surrounding space at a distance greater than 3 m.</p></abstract><trans-abstract xml:lang="ru"><p>Представлены результаты численного моделирования формирования и движения в процессе выдува одиночной импульсной турбулентной газокапельной струи примерно соответствующим условиям кашля человека. Расчеты проведены при длительности импульса <italic>t</italic> = 0.6 с и максимальной скорости газовой фазы 20 м/с при массовом содержании капель <italic>M</italic><sub>L</sub><sub>1</sub> = 1%. Капельная фаза в выходном сечении была монодисперсной, а начальный размер частиц в расчетах изменялся диапазоне <italic>D</italic><sub>1</sub> = 5‒30 мкм. В начальный период движения внутри облака формируются две зоны повышенной завихренности: в слое смешения и в области торможения импульсной двухфазной струи. Наибольший уровень продольной скорости и кинетической энергии турбулентности достигается в период выдува импульса. В последующие моменты времени происходит монотонное уменьшение скорости и уровня турбулентности. Вихревое облако, образованное одиночным импульсом, существует довольно продолжительное время (<italic>t</italic> ≈ 4 с) и за это время успевает проникнуть в окружающем затопленном пространстве на дистанцию более 3 м.</p></trans-abstract><kwd-group xml:lang="en"><kwd>pulsed gas-droplet jet</kwd><kwd>vortex cloud</kwd><kwd>numerical modeling</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>импульсная газокапельная струя</kwd><kwd>вихревое облако</kwd><kwd>численное моделирование</kwd></kwd-group><funding-group><award-group><funding-source><institution-wrap><institution xml:lang="ru">Министерство науки и высшего образования Российской Федерации</institution></institution-wrap><institution-wrap><institution xml:lang="en">Ministry of Science and Higher Education of the Russian Federation</institution></institution-wrap></funding-source><award-id>075-00383-21-00</award-id></award-group></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Ахметов Д.Г. 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