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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">10.19047/0136-1694-2010-65-75-86</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-482</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>Содержание лантанидов (Y, La, Ce, Pr, Nd, Sm) и актинидов (Th, U) в почвах Хибинско-Ловозерской провинции</article-title><trans-title-group xml:lang="en"><trans-title>LANTANIDES (Y, La, Ce, Pr, Nd, Sm) AND ACTINIDS (Th, U) IN SOILS OF THE HIBINO-LOVOZERO PROVINCE</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>Водяницкий</surname><given-names>Ю. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Vodianitsky</surname><given-names>Yu.</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>Косарева</surname><given-names>Н. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kosareva</surname><given-names>N.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Савичев</surname><given-names>А. Т.</given-names></name><name name-style="western" xml:lang="en"><surname>Savichev</surname><given-names>A.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Почвенный институт им. В.В. Докучаева Россельхозакадемии</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V.V. Dokuchaev Soil Science Institute</institution><country>Russian Federation</country></aff></aff-alternatives><aff xml:lang="ru" id="aff-2"><institution>Географический факультет Московского педагогического государственного университета</institution><country>Russian Federation</country></aff><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Геологический институт РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V.V. Dokuchaev Soil Science Institute</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2010</year></pub-date><pub-date pub-type="epub"><day>30</day><month>06</month><year>2010</year></pub-date><volume>0</volume><issue>65</issue><fpage>75</fpage><lpage>86</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Водяницкий Ю.Н., Косарева Н.В., Савичев А.Т., 2010</copyright-statement><copyright-year>2010</copyright-year><copyright-holder xml:lang="ru">Водяницкий Ю.Н., Косарева Н.В., Савичев А.Т.</copyright-holder><copyright-holder xml:lang="en">Vodianitsky Y., Kosareva N., Savichev 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/482">https://bulletin.esoil.ru/jour/article/view/482</self-uri><abstract><p>В районе Хибинско-Ловозерской провинции на Кольском п-ове территория делится на три геохимически разных участка. На фоновой территории вблизи Умбозера как в минеральных, так и в оторфованных образцах содержание всех редких металлов ниже кларкового: лантаниды и актиниды сильно выщелачиваются из кислых подзолистых почв. В районе слабой геохимической аномалии (вблизи Ловозера) от лопаритсодержащей породы наследуются все лантаниды, а из актинидов - Th: их содержание в 1.3-5.4 раза превышает кларковое значение. В зоне сильной геохимической аномалии (на северном берегу Сейдозера и на берегу р. Эльморайок) концентрация лантанидов и актинидов еще выше: в 4-9 раз превышает кларковое значение. Проявляется влияние биологического барьера, препятствующего чрезмерному накоплению тяжелых металлов во мхах на территории геохимической аномалии.</p></abstract><trans-abstract xml:lang="en"><p>In the Khibinsko-Lovozero district of the Kola Peninsula, the territory is divided into three geochemically different areas. In the background area near Umbozero, both mineral and peated samples contain all rare metals below clark: lanthanides and actinides are leaching heavily from acidic podzolic soils. В in the area of weak geochemical anomaly (near Lovozero), all lanthanides are inherited from the loparite-containing rock, and all actinides - Th: their content is 1.3-5.4 times higher than the clark value. In the zone of a strong geochemical anomaly (on the northern shore of Seidozero and on theThe concentration of lanthanides and actinides is even higher: 4-9 times higher than the clark value. There is an impact of a biological barrier that prevents excessive accumulation of of heavy metals in the mosses of a geochemical anomaly.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>лантаниды</kwd><kwd>актиниды</kwd><kwd>почвы</kwd><kwd>Хибинско-Ловозерская провинция</kwd></kwd-group><kwd-group xml:lang="en"><kwd>lanthanides</kwd><kwd>actinides</kwd><kwd>soils</kwd><kwd>Khibinsko-Lovozero province</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">Александрова Л.Н., Найденова О.А. Лабораторно-практические занятия по почвоведению. Л.: Колос, 1976. 279 с.</mixed-citation><mixed-citation xml:lang="en">Alexandrova L.N., Naidenova O.A. Laboratory of practical classes in soil science. L.: Kolos, 1976. 279 с.</mixed-citation></citation-alternatives></ref><ref id="cit2"><label>2</label><citation-alternatives><mixed-citation xml:lang="ru">Водяницкий Ю.Н., Савичев А.Т. 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