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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">blackmet</journal-id><journal-title-group><journal-title xml:lang="ru">Известия высших учебных заведений. Черная Металлургия</journal-title><trans-title-group xml:lang="en"><trans-title>Izvestiya. Ferrous Metallurgy</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0368-0797</issn><issn pub-type="epub">2410-2091</issn><publisher><publisher-name>National University of Science and Technology "MISIS"</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.17073/0368-0797-2014-6-12-15</article-id><article-id custom-type="elpub" pub-id-type="custom">blackmet-287</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>МЕТАЛЛУРГИЧЕСКИЕ ТЕХНОЛОГИИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>METALLURGICAL TECHNOLOGIES</subject></subj-group></article-categories><title-group><article-title>СВЯЗЬ СТРУКТУРЫ И ТЕРМОДИНАМИЧЕСКОЙ АКТИВНОСТИ САЖИСТОГО УГЛЕРОДА</article-title><trans-title-group xml:lang="en"><trans-title>THE CONNECTION BETWEEN THE STRUCTURE AND THERMODYNAMIC ACTIVITY OF SOOT CARBON</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>Амдур</surname><given-names>А. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Amdur</surname><given-names>A. M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>д.т.н., профессор</p></bio><bio xml:lang="en"><p>Dr. Eng., Professor</p></bio><email xlink:type="simple">engineer-ektb@rambler.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>Лхамсурэн</surname><given-names>М.</given-names></name><name name-style="western" xml:lang="en"><surname>Lkhamsuren</surname><given-names>M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>аспирант</p></bio><bio xml:lang="en"><p>Postgraduent</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Павлов</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Pavlov</surname><given-names>V. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>д.х.н, профессор</p></bio><bio xml:lang="en"><p>Dr. Chem., Professor</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Барнасан</surname><given-names>П.</given-names></name><name name-style="western" xml:lang="en"><surname>Barnasan</surname><given-names>P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>д.т.н., академик</p></bio><bio xml:lang="en"><p>Dr. Eng., academician</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Уральский государственный горный университет (Екатеринбург, Россия)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Ural State Mining University (Ekaterinburg, Russia)</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт химии и химической технологии АН Монголии (Улан-Батор, Монголия)</institution><country>Монголия</country></aff><aff xml:lang="en"><institution>Institute of Chemistry and Chemical Technology, Mongolian Academy of Sciences (Ulan Bator, Mongolia)</institution><country>Mongolia</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2014</year></pub-date><pub-date pub-type="epub"><day>25</day><month>03</month><year>2015</year></pub-date><volume>57</volume><issue>6</issue><fpage>12</fpage><lpage>15</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Амдур А.М., Лхамсурэн М., Павлов В.В., Барнасан П., 2015</copyright-statement><copyright-year>2015</copyright-year><copyright-holder xml:lang="ru">Амдур А.М., Лхамсурэн М., Павлов В.В., Барнасан П.</copyright-holder><copyright-holder xml:lang="en">Amdur A.M., Lkhamsuren M., Pavlov V.V., Barnasan P.</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://fermet.misis.ru/jour/article/view/287">https://fermet.misis.ru/jour/article/view/287</self-uri><abstract><p>Экспериментально с помощью сканирующего электронного микроскопа показано, что частицы сажистого углерода, полученного по реакции Будуара, имеют сложную ажурную структуру, включающую глобулярные аморфные и графитизированные кристаллические элементы, соединенные перемычками, размеры которых находятся в нанометровом диапазоне. Следствием высокодисперсной и аморфной структуры сажистого углерода является повышение энергии Гиббса и высокая кинетическая активность.</p></abstract><trans-abstract xml:lang="en"><p>Using a scanning electron microscope it has been shown that the particles of soot carbon produced by the Boudoir reaction, have a complicated open-work structure including globular amorphous parts and graphitized crystalline elements connected by crosspieses with the size of nanometric range. The soot carbon is characterized by increased Gibbs energy and high kinetic activity because of its dispersed and amorphous structure.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>частицы сажистого углерода</kwd><kwd>аморфная структура</kwd><kwd>энергия Гиббса</kwd><kwd>активность</kwd></kwd-group><kwd-group xml:lang="en"><kwd>particles black carbon</kwd><kwd>amorphous structure</kwd><kwd>Gibbs’s energy</kwd><kwd>activity</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа  выполнена  при  финансовой  поддержке  Российского  Фонда фундаментальных исследований и Научно-технологического  Фонда Монголии.</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">Есин О.А., Гельд П.В. Физическая химия пирометаллургических процессов. 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