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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">esoil</journal-id><journal-title-group><journal-title xml:lang="ru">Бюллетень Почвенного института имени В.В. Докучаева</journal-title><trans-title-group xml:lang="en"><trans-title>Dokuchaev Soil Bulletin</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0136-1694</issn><issn pub-type="epub">2312-4202</issn><publisher><publisher-name>V.V. Dokuchaev Soil Science Institute</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.19047/0136-1694-2024-119-172-210</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-802</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>Изменение элементного состава компонентов агроценоза на серой лесной почве при длительном применении минеральных и органических удобрений</article-title><trans-title-group xml:lang="en"><trans-title>Changes in the elemental composition of agrocenosis components on gray forest soil under long-term application of mineral and organic fertilizers</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-0515-6114</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Котельникова</surname><given-names>А. Д.</given-names></name><name name-style="western" xml:lang="en"><surname>Kotelnikova</surname><given-names>A. D.</given-names></name></name-alternatives><email xlink:type="simple">a.d.kotelnikova@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>Борисочкина</surname><given-names>Т. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Borisochkina</surname><given-names>T. I.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Колчанова</surname><given-names>К. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kolchanova</surname><given-names>K. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Шишкин</surname><given-names>М. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Shishkin</surname><given-names>M. A.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Егоров</surname><given-names>Ф. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Egorov</surname><given-names>F. S.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Окорков</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Okorkov</surname><given-names>V. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Рогова</surname><given-names>О. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Rogova</surname><given-names>O. B.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ФИЦ “Почвенный институт им. В.В. Докучаева”</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Federal Research Centre “V.V. Dokuchaev Soil Science Institute”</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Верхневолжский федеральный аграрный научный центр</institution><country>Россия</country></aff><aff xml:lang="en"><institution>State Scientific Institution Vladimir Research Institute of Agriculture</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>25</day><month>06</month><year>2024</year></pub-date><volume>0</volume><issue>119</issue><fpage>172</fpage><lpage>210</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Котельникова А.Д., Борисочкина Т.И., Колчанова К.А., Шишкин М.А., Егоров Ф.С., Окорков В.В., Рогова О.Б., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Котельникова А.Д., Борисочкина Т.И., Колчанова К.А., Шишкин М.А., Егоров Ф.С., Окорков В.В., Рогова О.Б.</copyright-holder><copyright-holder xml:lang="en">Kotelnikova A.D., Borisochkina T.I., Kolchanova K.A., Shishkin M.A., Egorov F.S., Okorkov V.V., Rogova O.B.</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://bulletin.esoil.ru/jour/article/view/802">https://bulletin.esoil.ru/jour/article/view/802</self-uri><abstract><p>Проанализирован элементный состав почв и растений агроценоза на серой лесной почве Владимирского Ополья при длительном применении минеральных и органических удобрений. Оценивалось валовое содержание и содержание подвижных форм Ni, Cu, Zn, Co, Mn, Fe, содержание этих элементов в надземных органах растений, а также изменения основных агрохимических характеристик, способных влиять на доступность элементов для растений. Показано, что внесение минеральных удобрений способствует подкислению почвы, увеличению содержания органического углерода, подвижных форм фосфора. При этом варианты с совместным внесением минеральных и органических удобрений подвержены меньшему изменению данных характеристик, что может быть обусловлено увеличению буферной способности почвы в отношении компонентов, поступающих с минеральными солями, за счет вносимого органического вещества. Привнос в агроценоз Ni, Cu, Zn, Co, Mn, Fe с удобрениями (органическими и минеральными) не отразился на валовом содержании металлов в почве. Произошло изменение содержания подвижных форм металлов в почве, обусловленное изменением агрохимических параметров почв. Зафиксировано изменение содержания микроэлементов в растительной продукции. Снижение содержания Zn, Cu в растениях в вариантах с более интенсивным использованием удобрений (и с более высокой урожайностью) объясняется “эффектом разбавления”. Требует контроля низкое содержание Со в почве и недостаточное его поступление в растения. Совместное использование данных по изменению элементного состава почв и растений позволяет лучше дифференцировать варианты опыта в пространстве главных компонент при анализе этим методом и перспективно для мониторинга последствий агрогенной нагрузки разной степени. Полученные результаты могут учитываться при формировании критериев оценки минерального питания растений и норм внесения удобрений.</p></abstract><trans-abstract xml:lang="en"><p>The paper analyzes the elemental composition of soils and plants of agrocenosis on the gray forest soil of Vladimir opolye under long-term application of mineral and organic fertilizers. The content of total and mobile forms of Ni, Cu, Zn, Co, Mn, Fe and the content of these elements in aboveground plant organs, as well as changes in the main agrochemical characteristics that can affect the availability of elements to plants were evaluated. It is shown that the application of mineral fertilizers contributes to soil acidification, increase in the content of organic carbon, mobile forms of phosphorus. At the same time, the variants with joint application of mineral and organic fertilizers are subject to less change of these characteristics, which may be due to the increased buffering capacity of the soil with respect to the components coming with mineral salts, due to the applied organic matter. Introduction of Ni, Cu, Zn, Co, Mn, Fe into agrocenosis with fertilizers (organic and mineral) did not affect the gross content of metals in soil. There was a change in the content of mobile forms of metals in the soil due to changes in agrochemical parameters of soils. Changes in the content of trace elements in plant products were recorded. The reduction of Zn, Cu content in plants on the variants with more intensive use of fertilizers (and with higher yield) is explained by "dilution effect". The low content of Co in the soil and its insufficient supply to the plants must be controlled. The joint use of data on changes in the elemental composition of soils and plants allows better differentiation of experimental variants in the space of principal components when analyzed by this method and is promising for monitoring the consequences of agrogenic load of different degrees. The results obtained can be taken into account in the formation of criteria for assessing the mineral nutrition of plants and fertilizer application rates.  </p></trans-abstract><kwd-group xml:lang="ru"><kwd>микроэлементы</kwd><kwd>полевой опыт</kwd><kwd>оптико-эмиссионная спектрометрия с индуктивно-связанной плазмой</kwd><kwd>метод главных компонент</kwd></kwd-group><kwd-group xml:lang="en"><kwd>trace elements</kwd><kwd>field experiment</kwd><kwd>inductively coupled plasma optical emission spectrometry</kwd><kwd>principal component analysis</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Часть работы выполнена по теме НИР № 0439-2022-0010 “Изучить элементный состав системы почва – растение как фактор-индикатор состояния агроценоза и дисбаланс как критерий рисков химической деградации почв” (отбор образцов, анализ элементного состава образцов, обработка данных), и часть работ выполнена за счет гранта Российского научного фонда № 22-74-00003, https://rscf.ru/project/22-74-00003/ (пробоподготовка образцов, определение агрохимических характеристик образцов).</funding-statement><funding-statement xml:lang="en">Part of the work was carried out under the R&amp;D plan No. 0439-2022-0010 “To study the elemental composition of the system soil – plant as a factor-indicator of the state of the agrocenosis and imbalance as a criterion of the risks of soil chemical degradation” (sampling, analysis of the elemental composition of samples, data processing), and part of the work was supported by the Russian Science Foundation № 22-74-00003, https://rscf.ru/project/22-74-00003/ (sample preparation, determination of agrochemical characteristics of samples).</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">Важенин И.Г. 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