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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">vmait</journal-id><journal-title-group><journal-title xml:lang="ru">Computational Mathematics and Information Technologies</journal-title><trans-title-group xml:lang="en"><trans-title>Computational Mathematics and Information Technologies</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2587-8999</issn><publisher><publisher-name>Донской государственный технический университет</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.23947/2587-8999-2018-2-76-90</article-id><article-id custom-type="elpub" pub-id-type="custom">vmait-71</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></article-categories><title-group><article-title>Построение и исследование корректности математической модели транспорта и осаждения взвесей с учетом изменений рельефа дна</article-title><trans-title-group xml:lang="en"><trans-title>About correctness of the suspension transport and sedimentation model, taking into account bottom relief changes</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-5875-1523</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Сухинов</surname><given-names>Александр Иванович</given-names></name><name name-style="western" xml:lang="en"><surname>Sukhinov</surname><given-names>Alexander Ivanovich</given-names></name></name-alternatives><bio xml:lang="ru"><p>Сухинов Александр Иванович, Донской государственный технический университет (344000 Ростов-на-Дону, пл. Гагарина, д. 1), доктор физико-математических наук, профессор</p></bio><bio xml:lang="en"><p>Sukhinov Alexander Ivanovich, Don State Technical University (1st Gagarin Square, Rostov-on-Don, Russian Federation), Doctor of Science in Physics and Maths, Professor</p></bio><email xlink:type="simple">sukhinov@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Сидорякина</surname><given-names>Валентина Владимировна</given-names></name><name name-style="western" xml:lang="en"><surname>Sidoryakina</surname><given-names>Valentina Vladimirovna</given-names></name></name-alternatives><bio xml:lang="ru"><p>Сидорякина Валентина Владимировна, Таганрогский институт им. А.П. Чехова (филиал) РГЭУ (РИНЭ) (347936 Таганрог, улица Инициативная, д. 48), кандидат физико-математических наук, доцент</p></bio><bio xml:lang="en"><p>Sidoryakina Valentina Vladimirovna, Taganrog Institute of A.P. Chekhov (branch) RSUE (Initiative Street, Taganrog, Russian Federation), Candidate of Science in Physics and Maths, Associate professor</p></bio><email xlink:type="simple">cvv9@mail.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Донской государственный технический университет&#13;
(344000 Ростов-на-Дону, пл. Гагарина, д. 1)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Don State Technical University &#13;
(1st Gagarin Square, Rostov-on-Don, Russian Federation)</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Таганрогский институт им. А.П. Чехова (филиал) РГЭУ (РИНЭ) &#13;
(347936 Таганрог, улица Инициативная, д. 48)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Taganrog Institute of A.P. Chekhov (branch) RSUE &#13;
(Initiative Street, Taganrog, Russian Federation)</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2018</year></pub-date><pub-date pub-type="epub"><day>28</day><month>03</month><year>2023</year></pub-date><volume>2</volume><issue>2</issue><elocation-id>71</elocation-id><permissions><copyright-statement>Copyright &amp;#x00A9; Сухинов А.И., Сидорякина В.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Сухинов А.И., Сидорякина В.В.</copyright-holder><copyright-holder xml:lang="en">Sukhinov A.I., Sidoryakina 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.cmit-journal.ru/jour/article/view/71">https://www.cmit-journal.ru/jour/article/view/71</self-uri><abstract><p>Настоящая работа посвящена исследованию пространственно-трехмерной модели транспорта и осаждения взвеси в прибрежной зоне с учетом изменения рельефа дна. Модель учитывает следующие процессы: адвективный перенос, обусловленный движением водной среды, микротурбулентную диффузию и гравитационное осаждение частиц взвеси, а также изменение геометрии дна, вызванное осаждением частиц взвеси или подъемом частиц донных отложений. Изменение рельефа дна приводит к необходимости решать начально-краевую задачу для уравнения параболического типа с младшими производными в области, геометрия которой зависит от искомой функции решения, что приводит, в общем случае, к нелинейной постановке задачи.Выполнена линеаризация модели на временной сетке за счет «замораживания» рельефа дна в пределах одного шага по времени и последующего пересчета функции поверхности дна на основе изменившейся функции концентрации взвешенного вещества, а также возможного изменения вектора скорости движения водной среды. Получена априорная оценка нормы решения в функциональном пространстве L2 в зависимости от интегральных оценок по времени правой части, граничных условий и начального условия, и, таким образом, доказана устойчивость решения исходной задачи от изменения начального и граничных условий и функции правой части. Модель может представлять ценность при прогнозе распространения загрязнений и изменения рельефа дна, как при антропогенном воздействии, так и в силу естественно протекающих природных процессов в прибрежной зоне.</p></abstract><trans-abstract xml:lang="en"><p>This paper is devoted to the study of the spatial-three-dimensional model of sedimentation of suspended particles in the coastal zone, taking into account changes in the bottom topography. The model takes into account the following processes: advective transfer due to movement of the aquatic environment, microturbulent diffusion and gravitational sedimentation of suspended particles, as well as changes in bottom geometry caused by sedimentation of suspended particles or rise of sediment particles. A change in the bottom relief leads to the need to solve an initial-boundary value problem for an equation of parabolic type with lower derivatives in a domain whose geometry depends on the desired solution function, which leads, in general, to a non-linear formulation of the problem. The model was linearized on a time grid due to the «freezing» of the bottom relief within one time step and the subsequent recalculation of the bottom surface function based on the changed function of suspended matter concentration, as well as a possible change in the velocity vector of the aquatic environment. For the linearized problem, a quadratic functional was constructed and the energy method proved the uniqueness of the solution of the corresponding initial-boundary problem within an arbitrary time step. Based on the transformation of the quadratic functional, an a priori estimate of the solution norm in the L2 functional space was obtained depending on the integral estimates for the right side and the initial condition, and, thus, the stability of the solution of the initial problem against the change of the initial and boundary conditions and functions of the right side. The model may be of value in predicting the spread of pollution and changes in the bottom topography, both under anthropogenic impact and due to naturally occurring natural processes in the coastal zone.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>прибрежные системы</kwd><kwd>математическая модель</kwd><kwd>диффузионно-конвективные задачи осаждения взвеси</kwd><kwd>изменение рельефа дна</kwd><kwd>единственность решения и устойчивость начально-краевой задачи</kwd></kwd-group><kwd-group xml:lang="en"><kwd>coastal systems</kwd><kwd>mathematical model</kwd><kwd>diffusion-convection problems of deposition of suspended matter</kwd><kwd>change of the bottom relief</kwd><kwd>uniqueness of the solution and stability of the initial-boundary value problem</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена по теме № 2.6905.2017/БЧ в рамках выполнения госзадания Минобрнауки России в части НИР.</funding-statement><funding-statement xml:lang="en">The research is done on theme no. 6905.2017/БЧ within the frame of the government task of the Ministry of Education and Science of the Russian Federation in R&amp;D.</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">Sukhinov, A.I., Sidoryakina, V.V., Sukhinov, A.A.: Sufficient convergence conditions</mixed-citation><mixed-citation xml:lang="en">Sukhinov, A.I., Sidoryakina, V.V., Sukhinov, A.A.: Sufficient convergence conditions</mixed-citation></citation-alternatives></ref><ref id="cit2"><label>2</label><citation-alternatives><mixed-citation xml:lang="ru">for positive solutions of linearized two-dimensional sediment transport problem. 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