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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">biologyscience</journal-id><journal-title-group><journal-title xml:lang="ru">Тимирязевский биологический журнал</journal-title><trans-title-group xml:lang="en"><trans-title>Timiryazev Biological Journal</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2949-4710</issn><publisher><publisher-name>ФГБОУ ВО РГАУ-МСХА имени К.А. Тимирязева (ФГБОУ ВО РГАУ-МСХА имени К.А. Тимирязева)</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.26897/2949-4710-2023-3-13-28</article-id><article-id custom-type="elpub" pub-id-type="custom">biologyscience-91</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>1 - БИОЛОГИЧЕСКИЕ РЕСУРСЫ, ЭКОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>1 - BIOLOGICAL RESOURCES, ECOLOGY</subject></subj-group></article-categories><title-group><article-title>Эколого-геохимическая оценка накопления тяжелых металлов в почве разновозрастных ампелоценозов в условиях склонового ландшафта горной гряды Фрушка гора Республики Сербия</article-title><trans-title-group xml:lang="en"><trans-title>Ecological and Geochemical Assessment of Heavy Metal Accumulation in Soil of Different-Aged Ampelocoenoses in the Slope Landscape of the Fruška Gora Mountain Range, Republic of Serbia</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-0760-665X</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Андреева</surname><given-names>И. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Andreeva</surname><given-names>I. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Ирина Викторовна Андреева, канд. биол. наук, доцент кафедры экологии</p><p>127434, г. Москва, ул. Тимирязевская, 49</p></bio><bio xml:lang="en"><p>Irina V. Andreeva, CSc (Bio), Associate Professor of the Department of Ecology</p><p>49, Timiryazevskaya Str., Moscow, 127434</p></bio><email xlink:type="simple">i.andreeva@rgau-msha.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/0000-0002-5621-6308</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Габечая</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Gabechaya</surname><given-names>V. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Валерия Вячеславовна Габечая, аспирант, ассистент кафедры экологии</p><p>127434, г. Москва, ул. Тимирязевская, 49</p></bio><bio xml:lang="en"><p>Valeriya V. Gabechaya, post-graduate student, Assistant of the Department of Ecology</p><p>49, Timiryazevskaya Str., Moscow, 127434</p></bio><email xlink:type="simple">lera.gabechaya@mail.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/0000-0003-2482-1949</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Морев</surname><given-names>Д. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Morev</surname><given-names>D. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Дмитрий Владимирович Морев, канд. биол. наук, доцент кафедры экологии</p><p>127434, г. Москва, ул. Тимирязевская, 49</p></bio><bio xml:lang="en"><p>Dmitriy V. Morev, CSc (Bio), Associate Professor of the Department of Ecology</p><p>49, Timiryazevskaya Str., Moscow, 127434</p></bio><email xlink:type="simple">dmorev@rgau-msha.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/0000-0001-8372-2209</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Таллер</surname><given-names>Е. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Taller</surname><given-names>E. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Евгений Борисович Таллер, канд. с.-х. наук, доцент кафедры экологии</p><p>127434, г. Москва, ул. Тимирязевская, 49</p></bio><bio xml:lang="en"><p>Evgeniy B. Taller, CSc (Ag), Associate Professor of the Department of Ecology</p><p>49, Timiryazevskaya Str., Moscow, 127434</p></bio><email xlink:type="simple">etallereb@rgau-msha.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Российский государственный аграрный университет – МСХА имени К.А. Тимирязева</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Russian State Agrarian University – Moscow Timiryazev Agricultural Academy</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>23</day><month>11</month><year>2023</year></pub-date><volume>1</volume><issue>3</issue><fpage>13</fpage><lpage>28</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Андреева И.В., Габечая В.В., Морев Д.В., Таллер Е.Б., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Андреева И.В., Габечая В.В., Морев Д.В., Таллер Е.Б.</copyright-holder><copyright-holder xml:lang="en">Andreeva I.V., Gabechaya V.V., Morev D.V., Taller E.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://www.bioscience-journal.com/jour/article/view/91">https://www.bioscience-journal.com/jour/article/view/91</self-uri><abstract><p>Цель исследований заключалась в эколого-геохимической оценке латеральной миграции тяжелых металлов в верхних горизонтах бурой лесной остаточно-карбонатной почвы в транзитном геохимическом ландшафте под разновозрастными виноградниками, выращиваемыми на склонах горной гряды Фрушка гора в Республике Сербия. Практическая значимость работы состояла в уточнении уровня экологического риска при культивировании разновозрастных виноградников в условиях проявления склоновых эрозионных процессов. Отбор почвенных проб проводили в рядах винограда в пределах сопряженных транзитных ландшафтов склонов с глубины 0-5, 5-15 и 15-30 см. Валовое содержание тяжелых металлов в почве и ягодах винограда определяли атомно-адсорбционным методом после микроволнового разложения. Результаты исследований показали высокую активность миграции меди и хрома в почве 15-летнего действующего виноградника от трансэлювиальной к трансаккумулятивной фации с усилением в горизонте 15-30 см. В почве выведенного из эксплуатации 100-летнего виноградника преобладала радиальная миграция с накоплением железа, марганца, кобальта и интенсивным накоплением меди с коэффициентом латеральной дифференциации 3,21 в горизонте 15-30 см в средней части склона. Максимальное содержание меди в почве возрастного виноградника составило 115,4 мг/кг, что на 28% превышает установленную в Республике Сербия величину максимально допустимого количества для среднесуглинистых почв. Близкие к нормативному значения содержания меди в почве молодого ампелоценоза (87,4-93,2 мг/кг) были обнаружены в нижней части склона по всей исследуемой глубине 0-30 см, которые были достигнуты всего за 15 лет выращивания. Максимальное накопление меди в ягодах (7,7 мг/кг) обнаружено в 100-летнем винограднике, расположенном в нижней части склона, где верхние горизонты почвы в отсутствие пестицидных обработок обеднены медью. Это косвенно свидетельствует о многолетней миграции меди в нижележащие горизонты почвы в условиях трансаккумулятивного элементарного ландшафта во влажный сезон года и о ее извлечении глубокой корневой системой старых виноградных растений.</p></abstract><trans-abstract xml:lang="en"><p>The aim of the present research was the ecological and geochemical assessment of the lateral migration of heavy metals in the upper horizons of brown forest residual-calcareous soil (Eutric Cambisol) in a transit geochemical landscape under different-aged vineyards grown on the slopes of the Fruska Gora mountain range in the Republic of Serbia. The practical significance of the work was to clarify the level of ecological risk in the cultivation of different-aged vineyards in the conditions of slope erosion processes. Soil samples were taken from rows of vines in transit slope landscapes at depths of 0-5, 5-15 and 15-30 cm. The total content of heavy metals in soil and grape berries was determined by atomic adsorption method after microwave decomposition. The results of the study showed a high activity of copper and chromium migration in the soil of a 15-year-old active vineyard from trans-eluvial to trans-accumulative facies with intensification in the 15-30 cm horizon. Radial migration with accumulation of iron, manganese, cobalt and intensive accumulation of copper with a lateral differentiation coefficient of 3.21 in the 15-30 cm horizon in the middle part of the slope prevailed in the soil of the abandoned 100-year-old vineyard. The highest copper concentration found in the soil of the old vineyard was 115.4 mg/kg, which is 28% higher than the maximum permissible copper content established for medium loamy soils in the Republic of Serbia. Copper content levels in the soils of the young ampelocoenosis were close to the normative values (87.4-93.2 mg/kg), found in the lower part of the slope up to a depth of 30 cm, which were achieved after only 15 years of cultivation. The highest copper concentration in grapes (7.7 mg/kg) was found in a 100-year-old vineyard located in the lower part of the slope, where the upper soil horizons were copper-depleted in the absence of pesticide treatments. This indirectly indicates the perennial migration of copper to the underlying soil horizons under trans-accumulative elemental landscape conditions during the wet season of the year and its extraction by the deep root system of old vines.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>почвы ампелоценозов</kwd><kwd>виноградник</kwd><kwd>склоновый ландшафт</kwd><kwd>почвы склонов</kwd><kwd>геохимический ландшафт</kwd><kwd>тяжелые металлы</kwd><kwd>загрязнение почвы</kwd><kwd>медь</kwd><kwd>миграция тяжелых металлов</kwd><kwd>бурая лесная почва</kwd><kwd>Фрушка гора</kwd><kwd>Сербия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>ampelocoenosis soils</kwd><kwd>vineyard</kwd><kwd>slope landscape</kwd><kwd>slope soils</kwd><kwd>geochemical landscape</kwd><kwd>heavy metals</kwd><kwd>soil pollution</kwd><kwd>copper</kwd><kwd>heavy metal migration</kwd><kwd>brown forest residual-calcareous soil (Eutric Cambisol)</kwd><kwd>Fruška Gora Mountain</kwd><kwd>Serbia</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">Перельман А.И. 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