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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">vestich</journal-id><journal-title-group><journal-title xml:lang="ru">Известия Национальной академии наук Беларуси. Серия химических наук</journal-title><trans-title-group xml:lang="en"><trans-title>Proceedings of the National Academy of Sciences of Belarus, Chemical Series</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1561-8331</issn><issn pub-type="epub">2524-2342</issn><publisher><publisher-name>The Republican Unitary Enterprise Publishing House "Belaruskaya Navuka"</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">vestich-158</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>ГЕОХИМИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOCHEMISTRY</subject></subj-group></article-categories><title-group><article-title>Изменение форм нахождения и подвижности кадмия, свинца и урана в дерново-подзолистых почвах в результате внесения биоугля</article-title><trans-title-group xml:lang="en"><trans-title>Changes in species and mobility of cadmium, lead and uranium in sod podzol soils after biochar application</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Соколик</surname><given-names>Г. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Sokolik</surname><given-names>G. A.</given-names></name></name-alternatives><email xlink:type="simple">sokolikga@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>Овсянникова</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Ovsiannikova</surname><given-names>S. V.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.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>Попеня</surname><given-names>М. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Popenia</surname><given-names>M. V.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.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>Войникова</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Voinikava</surname><given-names>K. V.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.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>Иванова</surname><given-names>Т. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanova</surname><given-names>T. G.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Белорусский государственный университет</institution></aff><aff xml:lang="en"><institution>Belarusian State University</institution></aff></aff-alternatives><pub-date pub-type="collection"><year>2015</year></pub-date><pub-date pub-type="epub"><day>08</day><month>06</month><year>2016</year></pub-date><volume>0</volume><issue>4</issue><fpage>73</fpage><lpage>80</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Соколик Г.А., Овсянникова С.В., Попеня М.В., Войникова Е.В., Иванова Т.Г., 2016</copyright-statement><copyright-year>2016</copyright-year><copyright-holder xml:lang="ru">Соколик Г.А., Овсянникова С.В., Попеня М.В., Войникова Е.В., Иванова Т.Г.</copyright-holder><copyright-holder xml:lang="en">Sokolik G.A., Ovsiannikova S.V., Popenia M.V., Voinikava K.V., Ivanova T.G.</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://vestichem.belnauka.by/jour/article/view/158">https://vestichem.belnauka.by/jour/article/view/158</self-uri><abstract><p>Методом химического фракционирования изучено изменение запаса Сё, Pb и U в обменной (обратимо сорбированной) и подвижной (условно биологически доступной) формах в песчаной и супесчаной разновидностях почв дерново-подзолистого типа после добавления 1-5 мас.% биоугля. Установлено, что к заметному снижению запаса Сё, Pb и U в формах, определяющих их подвижность и биологическую доступность растениям, при сохранении благоприятных условий для выращивания сельскохозяйственных культур может приводить внесение в супесчаные почвы биоугля в дозе 3 мас.%, а в песчаные - 3-5 мас.%.</p></abstract><trans-abstract xml:lang="en"><p>By the chemical fractionation method, the effect of 1-5 w. % of biochar addition to sandy and sandy-loam sod podzol soils on the Сd, Pb and U reserves in exchangeable (sorbed reversibly) and mobile (conditionally bioavailable) forms has been investigated. It has been found that, under conditions favorable for growing of agricultural plants, an essential decrease of Cd, Pb and U reserves in forms determining their mobility and availability in sandy soils could be caused by 3-5 w. % of biochar, but in sandy-loam soils it can be obtained with 3 w. % of biochar.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>обменная и подвижная формы кадмия</kwd><kwd>свинца и урана в почве</kwd><kwd>влияние биоугля на формы нахождения химических элементов в почвенной среде</kwd><kwd>exchangeable and mobile forms of cadmium</kwd><kwd>lead and uranium in soil</kwd><kwd>influence of biochar on the chemical element species in the soil medium</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">Hydrothermal carbonization of biomass residuals: a comparative review of the chemistry, processes and applications of wet and dry pyrolysis / J. A. 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