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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">10.19047/0136-1694-2022-110-114-147</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-701</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>Массоперенос химических элементов и их соединений в агроценозах</article-title><trans-title-group xml:lang="en"><trans-title>The mass transfer of chemical elements and of their compounds in agrocenoses</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-6123-4407</contrib-id><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><email xlink:type="simple">geotibor@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>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">info@esoil.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>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><email xlink:type="simple">olga_rogova@inbox.ru</email><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><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>25</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>110</issue><fpage>114</fpage><lpage>147</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Борисочкина Т.И., Котельникова А.Д., Рогова О.Б., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Борисочкина Т.И., Котельникова А.Д., Рогова О.Б.</copyright-holder><copyright-holder xml:lang="en">Borisochkina T.I., Kotelnikova A.D., 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/701">https://bulletin.esoil.ru/jour/article/view/701</self-uri><abstract><p>Проведен обзор и анализ литературных источников, освещающих массоперенос химических элементов в агроценозе в системе почва – растение. Рассмотрены отечественные и зарубежные методики оценки содержаний подвижных форм химических соединений, поступающих из почвы в растения. Охарактеризованы явления антагонизма и синергизма, указано на необходимость их учета при планировании внесения удобрений. Показано, что явления синергизма и антагонизма элементов могут быть использованы в земледелии для регулирования поступления тяжелых металлов или радионуклидов в сельскохозяйственную продукцию. Дан анализ балансовой модели массопереноса химических элементов в агроценозе. Показано, что внесение органических удобрений в почву в большинстве случаев приводит к положительному балансу микроэлементов в агросистеме. Вынос микроэлементов сельскохозяйственными культурами увеличивается при применении минеральных удобрений в дозах, оптимальных для возделывания культур в данном регионе. В ряде случаев поступление тяжелых металлов с техногенными выпадениями может превосходить вынос металлов растениями из почвы, что может явиться причиной аккумуляции металлов в системе. На незагрязненных фоновых территориях уровни поступления микроэлементов из удобрений и атмосферных выпадений в агроценозах сопоставимы. </p></abstract><trans-abstract xml:lang="en"><p>The analysis of publications on the mass transfer of chemical elements in agrocenosis in the soil – plant system was carried out. Methods for estimating the content of mobile forms of chemical compounds coming from the soil into plants are considered. The phenomena of antagonism and synergism are characterized, and the necessity to consider them while planning fertilizer application is indicated. It is shown that the phenomena of synergism and antagonism of elements can be used in agriculture to regulate the flow of heavy metals or radionuclides into agricultural products. A balance model for mass transfer of chemical elements in agrocenosis is analyzed. It is shown that the introduction of organic fertilizers in soil mostly leads to a positive balance of microelements in the agrosystem. To characterize the efficiency of fertilizer use an assessment of the balance of nutrients in the agrosystem is required. The removal of trace elements by agricultural crops increases with the use of mineral fertilizers in doses that are optimal for the cultivation of crops in the region. In some cases, the input of heavy metals with technogenic fallout may exceed the removal of metals by plants from the soil. It may cause the accumulation of metals in the system. In uncontaminated background areas, the levels of microelement intake from fertilizers and atmospheric fallout in agrocenoses are comparable.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>почва</kwd><kwd>растение</kwd><kwd>агроценоз</kwd><kwd>балансовая модель</kwd><kwd>синергизм</kwd><kwd>антагонизм</kwd></kwd-group><kwd-group xml:lang="en"><kwd>mass transfer</kwd><kwd>soil</kwd><kwd>plant</kwd><kwd>agrocenosis</kwd><kwd>balance model</kwd><kwd>synergism</kwd><kwd>antagonism</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа 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”.</funding-statement><funding-statement xml:lang="en">The work was performed on the topic of the research 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”.</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">Алексеев Ю.В. 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