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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">10.19047/0136-1694-2020-103-51-84</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-559</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>Особенности элементного состава почв Пур-Тазовского междуречья</article-title><trans-title-group xml:lang="en"><trans-title>Elemental composition of soils  of the Pur-Taz interfluve</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-6338-7669</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Московченко</surname><given-names>Д. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Moskovchenko</surname><given-names>D. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>сектор геоэкологии, зав. сектором </p><p>625026, Тюмень , ул. Малыгина, 86,</p></bio><email xlink:type="simple">moskovchenko1965@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>Романенко</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Romanenko</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>625026, Тюмень , ул. Малыгина, 86,</p></bio><email xlink:type="simple">leta-92@list.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ФИЦ Тюменский научный центр СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Tyumen Scientific Centre, Northern Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>28</day><month>09</month><year>2020</year></pub-date><volume>0</volume><issue>103</issue><fpage>51</fpage><lpage>84</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Московченко Д.В., Романенко Е.А., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Московченко Д.В., Романенко Е.А.</copyright-holder><copyright-holder xml:lang="en">Moskovchenko D.V., Romanenko E.A.</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/559">https://bulletin.esoil.ru/jour/article/view/559</self-uri><abstract><p>Проведена оценка элементного состава почв, сфагновых мхов и лишайников Пур-Тазовского междуречья (Западная Сибирь). Содержание химических элементов определено с применением метода рентген-флуоресцентной спектрометрии. Полученные результаты показывают, что почвы характеризуются относительно низкими концентрациями экологически опасных тяжелых металлов, среднее содержание которых либо ниже кларка земной коры (Cu, Pb, Zn, Ni, Sr), либо равно ему (Hg, Co), что подтверждает выводы предшествующих исследований. Крайне низкое содержание отмечено для физиологически важных Zn и Сu. Повышенные относительно кларка концентрации отмечены для малоподвижных элементов (Mo, Sn и Zr). Выявлены существенные различия в составе минеральных и органогенных горизонтов почв постлитогенного ствола. Средние концентрации P, Zn и S в органогенных горизонтах соответственно в 7.1, 8.1 и 18 раз выше, чем в иллювиальных минеральных горизонтах. Таким образом, химический состав почв в значительной степени определяется биологическим накоплением халькофильных элементов. В верховом торфе олиготрофных болот выше содержание халькофильных элементов, подвижных в кислой среде и интенсивно поглощаемых растениями (Zn, Cu, Cd, Hg). В торфе ерниково-кустарничково-мохово-лишайниковых тундр и лиственничных редколесий повышено содержание литофильных Al, Si, Ti, Zr, поступающих c пылевыми выпадениями из атмосферы. Выявленные особенности элементного состава почв необходимо учитывать при проведении мониторинга загрязнения тяжелыми металлами.</p></abstract><trans-abstract xml:lang="en"><p>In order to evaluate the chemical composition of natural background environments of Pur-Taz interfluve (Western Siberia), the mineral components of soils, peats, lichens, and sphagnum mosses have been analyzed. The samples were tested using X-ray fluorescence technology. The average contents of hazardous metals in the soils of the Pur-Taz interfluve are either lower (for Cu, Pb, Zn, Ni, Sr) or equal to (for Hg, Co) the average values of these elements in the Earth's crust. This finding corresponds to the commonly held view that the contents of elements in the soils located in the north of Western Siberia are lower than the world averages. Additionally, in our samples low concentrations of copper and zinc have been observed. Since these microelements are important for soil physiology, this finding indicates unfavorable biochemical conditions in the research area. On the other hand, high concentrations are observed for inactive elements such as Mo, Sn and Zr. The significant differences have been identified in the composition of mineral and organic soil horizons. For instance, the average concentrations of P, Zn and S in organic horizons are 7.1, 8.1 and 18 times greater than in the illuvial mineral horizons, respectively. The intense accumulation of Zn, Cu, Cd, Hg has been recorded, all of them are chalcophiles in the ombrotrophic peat. This means that the chemical composition of soil is largely determined by biological accumulation of chalcophile elements. The content of lithophilic Al, Si, Ti and Zr, coming with dust precipitation from the atmosphere increases in the peat of dwarf shrub-moss-lichen tundras and larch woodlands. The revealed values of the elemental composition of soils can be recommended as background in the course of the environmental monitoring.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>Западная Сибирь</kwd><kwd>тундра</kwd><kwd>микроэлементы</kwd><kwd>почвы</kwd><kwd>лишайники</kwd><kwd>сфагновые мхи</kwd></kwd-group><kwd-group xml:lang="en"><kwd>Western Siberia</kwd><kwd>tundra</kwd><kwd>trace elements</kwd><kwd>soil</kwd><kwd>lichens</kwd><kwd>sphagnum mosses</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">СО РАН (AAAA-A17-1117050-4000146-5); РФФИ (18-45-890002\18)</funding-statement><funding-statement xml:lang="en">Tyumen Scientific Centre (Northern Branch of the Russian Academy of Sciences) project No. AAAA-A17-1117050-4000146-5; RFBR - project No. 18-45-890002\18.</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">Агбалян Е.В., Шинкарук Е.В. 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