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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">10.19047/0136-1694-2011-67-67-79</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-494</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>Металлы в загрязненном нефтью торфе (Западная Сибирь)</article-title><trans-title-group xml:lang="en"><trans-title>METALS IN OILED PEAT (WESTERN SIBERIA)</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>Юрий Никифорович</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>Савичев</surname><given-names>Александр Тимофеевич</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-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Трофимов</surname><given-names>Сергей Яковлевич</given-names></name><name name-style="western" xml:lang="en"><surname>Trofimov</surname><given-names>S.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Шишконакова</surname><given-names>Екатерина Анатольевна</given-names></name><name name-style="western" xml:lang="en"><surname>Shishkonakova</surname><given-names>E.</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>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-alternatives id="aff-2"><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><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Факультет почвоведения МГУ им. М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2011</year></pub-date><pub-date pub-type="epub"><day>30</day><month>06</month><year>2011</year></pub-date><volume>0</volume><issue>67</issue><fpage>67</fpage><lpage>79</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Водяницкий Ю.Н., Савичев А.Т., Трофимов С.Я., Шишконакова Е.А., 2011</copyright-statement><copyright-year>2011</copyright-year><copyright-holder xml:lang="ru">Водяницкий Ю.Н., Савичев А.Т., Трофимов С.Я., Шишконакова Е.А.</copyright-holder><copyright-holder xml:lang="en">Vodianitsky Y., Savichev A., Trofimov S., Shishkonakova E.</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/494">https://bulletin.esoil.ru/jour/article/view/494</self-uri><abstract><p>Изучение металлов в торфе, загрязненном нефтью, имеет двоякое значение. Во-первых, диагностическое, как удобный и простой прием мониторинга состояния почвы, во-вторых, экологическое - для прогноза состояния торфяника, как элемента биоценоза. Все элементы-поллютанты в загрязненных торфах делятся на две группы. Одни из них (Ti, V, Cr, Ni, Zr, Ba, Y, La, Ce, Nd) накапливаются в верхнем, битуминозном слое торфа. Другие элементы (галоген хлор, а также металлы: Ca, Мn, Zn, Cu, Sr), напротив, мигрируют вглубь торфяной толщи вместе с легкими фракциями углеводородов. Для улавливания особо подвижных металлов Cu, Zn необходимо устройство искусственных геохимических барьеров, предотвращающих попадание поллютантов в грунтовые воды и открытые водоемы</p></abstract><trans-abstract xml:lang="en"><p>The study of metals in oil-contaminated peat has double meaning. Firstly, it is diagnostic as convenient and simple The method of soil condition monitoring, and secondly, the ecological method to predict the state of the peat bog as a biocenosis element. Every pollutant elements in contaminated peat are divided into two bands. Some of them (Ti, V, Cr, Ni, Zr, Ba, Y, La, Ce, Nd) accumulate in the upper, bituminous layer of peat. Other elements (halogen chlorine, as well as metals: Ca, Mp, Zn, Cu, Sr), on the contrary, migrate deep into the peat layer with light fractions hydrocarbons. For capturing particularly moving Cu metals, Zn needs to be equipped with artificial geochemical barriers to prevent pollutants from entering groundwater and open ponds.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>загрязнение нефтью</kwd><kwd>поллютанты</kwd><kwd>торф</kwd></kwd-group><kwd-group xml:lang="en"><kwd>oil pollution</kwd><kwd>pollutants</kwd><kwd>peat</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">Аветов Н.А., Шишконакова Е.А. Нефтяное загрязнение болот Западной Сибири // Природа. 2010. № 11. 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Determination of barium, lanthanum and cerium contents in soils by the X-ray radiometric method // Eurasian Soil Science. 2009. V. 42. № 13. P. 1461-1469.</mixed-citation></citation-alternatives></ref></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
