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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">serp</journal-id><journal-title-group><journal-title xml:lang="ru">Эрозия почв и русловые процессы</journal-title><trans-title-group xml:lang="en"><trans-title>Soil erosion and river channel processes</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">3034-4638</issn><publisher><publisher-name>Limited Liability Company “Expert laboratory ”Hydroinformational systems”</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.71367/3034-4638-2025-2-2-33-50</article-id><article-id custom-type="elpub" pub-id-type="custom">serp-34</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>ПОЛЕВОЙ МОНИТОРИНГ АЛЛЮВИАЛЬНОГО ОСАДКОНАКОПЛЕНИЯ В ПОЙМЕ СРЕДНЕГО ТЕЧЕНИЯ Р. ОКИ</article-title><trans-title-group xml:lang="en"><trans-title>FIELD MONITORING OF ALLUVIAL SEDIMENT ACCUMULATION IN THE OKA RIVER FLOODPLAIN (IN THE MIDDLE PART OF THE ITS BASIN)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-7110-4232</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Воробьев</surname><given-names>А. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Vorobyov</surname><given-names>A. Y.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Воробьев Алексей Юрьевич, доцент кафедры гео- графии, экологии и туризма, кандидат географических наук </p><p>г. Рязань</p></bio><bio xml:lang="en"><p>Aleksey Y. Vorobyov, Candidate of Geographical Sciences, Associate Professor, Department of Geography, Ecology, and Tourism, Candidate of Geographical Sciences</p><p>Ryazan</p></bio><email xlink:type="simple">a.vorobyov90@mail.ru</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>Кривцов</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Krivtsov</surname><given-names>V. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кривцов Вячеслав Андреевич, профессор, профессор кафедры географии, экологии и туризма, доктор географических наук</p><p>г. Рязань</p></bio><bio xml:lang="en"><p>Vyacheslav A. Krivtsov, Doctor of Geographical Sciences, Professor, Full Professor of the Department of Geography, Ecology and Tourism</p><p>Ryazan</p></bio><email xlink:type="simple">v.krivtsov@rzn-rsu.ru</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>Водорезов</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Vodorezov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Водорезов Алексей Владимирович, доцент, заведующий кафедрой географии, экологии и туризма, кандидат географических наук</p><p>г. Рязань</p></bio><bio xml:lang="en"><p>Alexey V. Vodorezov, Candidate of Geographical Sciences, Associate Professor, Head of the Department of Geography, Ecology and Tourism</p><p>Ryazan</p></bio><email xlink:type="simple">a.vodorezov@rzn-rsu.ru</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>Варнаков</surname><given-names>А. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Varnakov</surname><given-names>A. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Варнаков Алексей Николаевич, доцент кафедры географии, экологии и туризма, кандидат технических наук</p><p>г. Рязань</p></bio><bio xml:lang="en"><p>Alexey N. Varnakov, Candidate of Technical Sciences, Associate Professor, Department of Geography, Ecology and Tourism</p><p>Ryazan</p></bio><email xlink:type="simple">a.varnakov@rzn-rsu.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0009-0007-1416-7898</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Кадыров</surname><given-names>А. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Kadyrov</surname><given-names>A. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кадыров Александр Сергеевич, аспирант, лаборант кафедры географии, экологии и туризма</p><p>г. Рязань</p></bio><bio xml:lang="en"><p>Aleksandr S. Kadyrov, post-graduate student, assistant, Department of Geography, Ecology, and Tourism</p><p>Ryazan</p></bio><email xlink:type="simple">alieksandr.kadyrov93@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Рязанский государственный университет имени С.А. Есенина</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Ryazan State University named after S.A. Yesenin</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>14</day><month>07</month><year>2025</year></pub-date><volume>0</volume><issue>2</issue><fpage>33</fpage><lpage>50</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Воробьев А.Ю., Кривцов В.А., Водорезов А.В., Варнаков А.Н., Кадыров А.С., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Воробьев А.Ю., Кривцов В.А., Водорезов А.В., Варнаков А.Н., Кадыров А.С.</copyright-holder><copyright-holder xml:lang="en">Vorobyov A.Y., Krivtsov V.A., Vodorezov A.V., Varnakov A.N., Kadyrov A.S.</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://journal.sediment.ru/jour/article/view/34">https://journal.sediment.ru/jour/article/view/34</self-uri><abstract><p>С помощью метода седиментационных ловушек-матов показаны возможности и результаты геоморфологического мониторинга скорости аллювиального осадконакопления в пойме р. Оки. За период 2014–2021 гг. прохождение только двух весенних половодий приводило к затоплению центральной (высокой) поймы и аккумуляции слоя наилка мощностью 0.45 мм. На низкой пойме осадконакопление наблюдалось ежегодно, средняя мощность слоя минеральных (по ГОСТ 25100-2020) наносов на матах достигает 19.8 мм/год. Вглубь пойменно-русловых комплексов рельефа транспортируются только пылевато-глинистые наносы, а на прирусловых участках регистрировалась и аккумуляция песчаных частиц. В среднем высокая пойма на задействованных позициях мониторинга затапливается на 15 дней, что соответствует средней поемности по градации В.И. Шрага. На прирусловых же участках прямое взаимодействие водных масс потока и береговых грунтов может растягиваться на 1–6 месяцев и сильно зависит от типа весны и параметров половодья. Это позволяет выделить подобные обстановки осадконакопления как участки с регулярным проявлением флювиального морфолитогенеза, восприимчивые к колебаниям мезоклимата окского бассейна.</p></abstract><trans-abstract xml:lang="en"><p>We present the results of using the method of sedimentation traps (mats) in geomorphological monitoring of alluvial sedimentation rates in the floodplain of the Oka River. Only two spring floods between 2014 and 2021 inundated the central (high) floodplain, resulting in the accumulation of a 0.45 mm layer of sediments. We observed sedimentation on the low floodplain annually. The average thickness of the mineral (according to National Standard 25100-2020) sediment layer on the mats reaches 19.8 mm/year. Only silty-clay sediments are transported far from the Oka River channel, and accumulation of sandy particles was noted in the river channel zone. We determined that the high floodplain at the monitoring points is inundated typically within 15 days, which corresponds to an average flood according to the V.I. Shrag's gradation. In riverine areas, the direct interaction between stream water masses and bank soils can extend for 1–6 months and is highly dependent on the type of spring and flood parameters. This allows us to identify such sedimentation settings as areas with regular manifestation of fluvial morpholithogenesis, sensitive to fluctuations in the climate of the Oka basin.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>река Ока</kwd><kwd>пойма</kwd><kwd>седиментационная ловушка</kwd><kwd>половодье</kwd><kwd>аллювий</kwd><kwd>гранулометрический анализ</kwd><kwd>органическое вещество</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Oka River</kwd><kwd>floodplain</kwd><kwd>sediment trap</kwd><kwd>spring flood</kwd><kwd>alluvium</kwd><kwd>granulometric analysis</kwd><kwd>organic carbon</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Исследование выполнено при поддержке РНФ, проект № 22-77-00050.</funding-statement><funding-statement xml:lang="en">The study was funded by the Russian Science Foundation, Project no. 22-77-00050.</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">Александровский А.Л., Гласко М.П. 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