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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">melio</journal-id><journal-title-group><journal-title xml:lang="ru">Мелиорация</journal-title><trans-title-group xml:lang="en"><trans-title>Land Reclamation</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2070-4828</issn><publisher><publisher-name>Институт мелиорации</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">melio-1102</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>МЕЛИОРАЦИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>LAND IMPROVEMENT</subject></subj-group></article-categories><title-group><article-title>Режим наносов в р. Хуанхэ и их аккумуляция в водохранилищах</article-title><trans-title-group xml:lang="en"><trans-title>Sediment regime in the Yellow River and its accumulation in reservoirs</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>Михневич</surname><given-names>Э. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Mikhnevich</surname><given-names>E. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>доктор технических наук</p><p>г. Минск</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>Ли</surname><given-names>Цзэмин</given-names></name><name name-style="western" xml:lang="en"><surname>Li</surname><given-names>Zemin</given-names></name></name-alternatives><bio xml:lang="ru"><p>аспирант</p><p>г. Фушунь</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Белорусский национальный технический университет</institution><country>Belarus</country></aff><aff xml:lang="ru" id="aff-2"><institution>Шэньянский технологический институт</institution><country>China</country></aff><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>04</day><month>04</month><year>2024</year></pub-date><volume>0</volume><issue>1</issue><fpage>34</fpage><lpage>42</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Михневич Э.И., Ли Ц., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Михневич Э.И., Ли Ц.</copyright-holder><copyright-holder xml:lang="en">Mikhnevich E.I., Li Z.</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://melio.belal.by/jour/article/view/1102">https://melio.belal.by/jour/article/view/1102</self-uri><abstract><p>Река Хуанхэ – важнейший источник воды, подаваемой на орошение. Однако в ней отмечается очень высокая концентрация взвешенных наносов, среднемноголетнее значение которой составляет порядка 30 кг/м3. Для обеспечения гарантированной подачи воды на ирригационные системы, нормальной работы магистральных каналов требуется снижение мутности потока в реке. Для определения необходимой степени ее снижения изучен режим наносов в реке, предложена методика расчета транспортирующей способности взвесенасыщенного потока, установлены корреляционные связи между годовым стоком, содержанием наносов в речном потоке, проходящем через створы реки, в которых расположены гидрологические станции. Транспорт наносов в нижнем створе реки тесно связан с годовым стоком воды, содержанием наносов в потоке, проходящем через верхнюю станцию. Дана оценка аккумулирующей способности водохранилища Сяоланди, методика определения объемов и сроков его заиления.</p></abstract><trans-abstract xml:lang="en"><p>The Yellow River (Huang He) is the most important source of water supplied for irrigation. However, it has a very high concentration of suspended sediment, the long-term average value of which is about 30 kg/m3. To ensure a guaranteed supply of water to irrigation systems and normal operation of main canals, a reduction in the turbidity of the flow in the river is required. To determine the required degree of its reduction, the sediment regime in the river was studied, a methodology was proposed for calculating the transport capacity of a suspended saturated flow, and correlations were established between the annual runoff and sediment content in the river flow passing through the river sections in which hydrological stations are located. Sediment transport in the lower section of the river is closely related to the annual water flow and sediment content in the flow passing through the upper station. An assessment of the storage capacity of the Xiaolandi reservoir and a method for determining the volume and timing of its siltation are given.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>режим наносов</kwd><kwd>русловые процессы</kwd><kwd>транспортирующая способность потока</kwd><kwd>незаиляющая скорость</kwd><kwd>аккумуляция наносов</kwd><kwd>заиление водохранилища</kwd></kwd-group><kwd-group xml:lang="en"><kwd>sediment regime</kwd><kwd>channel processes</kwd><kwd>transporting capacity of the flow</kwd><kwd>non-silting speed</kwd><kwd>sediment accumulation</kwd><kwd>siltation of the reservoir</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Study on the characteristics of sediment erosion and siltation in flooded areas with high sediment content in the lower reaches of the Yellow River / Qian Sheng [et al.] // People's Yellow River. – 2021. – 43 (S2). – P. 20–22. https:// doi: 10.3969/j.issn.1000-1379.2021.S2.008</mixed-citation><mixed-citation xml:lang="en">Study on the characteristics of sediment erosion and siltation in flooded areas with high sediment content in the lower reaches of the Yellow River / Qian Sheng [et al.] // People's Yellow River. – 2021. – 43 (S2). – P. 20–22. https:// doi: 10.3969/j.issn.1000-1379.2021.S2.008</mixed-citation></citation-alternatives></ref><ref id="cit2"><label>2</label><citation-alternatives><mixed-citation xml:lang="ru">Чалов, Р. 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