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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">hydrophysics</journal-id><journal-title-group><journal-title xml:lang="ru">Фундаментальная и прикладная гидрофизика</journal-title><trans-title-group xml:lang="en"><trans-title>Fundamental and Applied Hydrophysics</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2073-6673</issn><issn pub-type="epub">2782-5221</issn><publisher><publisher-name>St. Petersburg Research Center of the Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">hydrophysics-1030</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>ГИДРОФИЗИЧЕСКИЕ И БИОГЕОХИМИЧЕСКИЕ ПОЛЯ И ПРОЦЕССЫ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>HYDROPHYSICAL AND BIOGEOCHEMICAL FIELDS AND PROCESSES</subject></subj-group></article-categories><title-group><article-title>Воспроизведение взмучивания и переноса донных осадков в Невской губе на основе трехмерной модели циркуляции</article-title><trans-title-group xml:lang="en"><trans-title>Simulation of the Resuspension and Transport of Bottom Sediments in the Neva Bay Using a 3D Circulation Model</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Мартьянов</surname><given-names>С. Д.</given-names></name><name name-style="western" xml:lang="en"><surname>Martyanov</surname><given-names>S. D.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург </p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Рябченко</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Ryabchenko</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Санкт-Петербург </p></bio><email xlink:type="simple">vla-ryabchenko@yandex.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Российский государственный гидрометеорологический университет<country>Россия</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru">Санкт-Петербургский филиал Института океанологии им. П.П.Ширшова РАН<country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2013</year></pub-date><pub-date pub-type="epub"><day>27</day><month>11</month><year>2022</year></pub-date><volume>6</volume><issue>4</issue><fpage>32</fpage><lpage>43</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Мартьянов С.Д., Рябченко В.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Мартьянов С.Д., Рябченко В.А.</copyright-holder><copyright-holder xml:lang="en">Martyanov S.D., Ryabchenko V.A.</copyright-holder><license 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://hydrophysics.spbrc.ru/jour/article/view/1030">https://hydrophysics.spbrc.ru/jour/article/view/1030</self-uri><abstract><p>Трехмерная модель Невской губы, описывающая процессы взмучивания донных и переноса взвешенных осадков, дополнена включением в нее переменной скорости гравитационного опускания взвешенных частиц и новой методики расчета суммарного придонного напряжения за счет течений и ветровых волн. При расчете критического придонного напряжения учитываются эффекты когезии. Ветровое волнение рассчитывается по модели SWAN. Наилучшее соответствие между спутниковыми и модельными данными о концентрации взвешенных частиц достигается при задании коэффициента поправки на когезию донных иловых осадков, равного 1.5, а также нулевого и 10 %- ного содержания глины соответственно в песчаных и иловых осадках.</p></abstract><trans-abstract xml:lang="en"><p>.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>взмучивание</kwd><kwd>донные осадки</kwd><kwd>моделирование</kwd><kwd>Невская губа</kwd></kwd-group><funding-group xml:lang="ru"><funding-statement>Работа выполнена в Российском государственном гидрометеорологическом университете в рамках гранта Правительства РФ (договор № 11.G34.31.0078) для поддержки исследований под руководством ведущих ученых</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Grant W.D., Madsen O.S. Combined wave and current interaction with a rough bottom // J. 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