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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">10.17073/0368-0797-2017-2-145-150</article-id><article-id custom-type="elpub" pub-id-type="custom">blackmet-1024</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>ФИЗИКО-ХИМИЧЕСКИЕ ОСНОВЫ МЕТАЛЛУРГИЧЕСКИХ ПРОЦЕССОВ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>PHYSICO-CHEMICAL BASICS OF METALLURGICAL PROCESSES</subject></subj-group></article-categories><title-group><article-title>ФИЗИКО-ХИМИЧЕСКАЯ АТТЕСТАЦИЯ КАРБИДА КРЕМНИЯ – ПРОДУКТА ВОССТАНОВЛЕНИЯ ТЕХНОГЕННОГО МИКРОКРЕМНЕЗЕМА БУРОУГОЛЬНЫМ ПОЛУКОКСОМ</article-title><trans-title-group xml:lang="en"><trans-title>PHYSICAL-CHEMICAL ASSESSMENT OF SILICON CARBIDE – PRODUCT OF TECHNOGENIC SILICA RECOVERY BY FUME LIGNITE SEMI-COKE</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>Аникин</surname><given-names>А. Е.</given-names></name><name name-style="western" xml:lang="en"><surname>Anikin</surname><given-names>A. E.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кандидат технических наук, доцент кафедры теплоэнергетики и экологии</p></bio><bio xml:lang="en"><p>Cand. Sci. (Eng.), Assist. Professor of the Chair “Thermal Power and Ecology”</p></bio><email xlink:type="simple">kafcmet@sibsiu.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>Галевский</surname><given-names>Г. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Galevskii</surname><given-names>G. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Доктор технических наук, профессор, директор института металлургии и материаловедения, заведующий кафедрой металлургии цветных металлов и химической технологии</p></bio><bio xml:lang="en"><p>Dr. Sci. (Eng.), Professor, Head of the Chair “Non-ferrous Metallurgy and Chemical Engineering”, Director of the Institute of Metallurgy and Materials</p></bio><email xlink:type="simple">kafcmet@sibsiu.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>Руднева</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Rudneva</surname><given-names>V. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Доктор технических наук, профессор кафедры металлургии цветных металлов и химической технологии</p></bio><bio xml:lang="en"><p>Dr. Sci. (Eng.), Professor of the Chair “Non-ferrous Metallurgy and Chemical Engineering</p></bio><email xlink:type="simple">kafcmet@sibsiu.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Сибирский государственный индустриальный университет</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Siberian State Industrial University</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2017</year></pub-date><pub-date pub-type="epub"><day>01</day><month>03</month><year>2017</year></pub-date><volume>60</volume><issue>2</issue><fpage>145</fpage><lpage>150</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Аникин А.Е., Галевский Г.В., Руднева В.В., 2017</copyright-statement><copyright-year>2017</copyright-year><copyright-holder xml:lang="ru">Аникин А.Е., Галевский Г.В., Руднева В.В.</copyright-holder><copyright-holder xml:lang="en">Anikin A.E., Galevskii G.V., Rudneva V.V.</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/1024">https://fermet.misis.ru/jour/article/view/1024</self-uri><abstract><p>Проведена физико-химическая аттестация карбида кремния, полученного из высокодисперсной шихты двух видов, состоящей из микрокремнезема, образующегося при производстве кремния и высококремнистого ферросилиция, и полукокса из бурого угля Березовского месторождения Канско-Ачинского бассейна. Микрокремнезем обоих видов содержит 93,41 – 95,33 % и 91,72 – 93,63 % SiO2 ; 1,96 – 3,28 % и 0,56 – 1,18 % Ссвоб. ; 0,30 – 0,34 % и 0,18 – 0,20 % Siсвоб. ; 1,25 – 1,45 и 1,38 – 2,32 % (CaO + Fe2O3 + MnO). Микрокремнезем имеет удельную поверхность 21 000 – 24 000 м2/кг, склонен к агрегированию с образованием шаровидных агрегатов размером 200 – 800 нм. Агрегаты составлены шарообразными частицами размерного диапазона от 30 до 100 нм. Буроугольный полукокс содержит 94,05 % углерода; 9,2 % золы; 0,2 % серы; 0,007 % фосфора и имеет удельную поверхность 264 000 кг/м2. Исследованы фазовый и химический составы карбида кремния, его удельная поверхность, размер и форма карбидных частиц. Установлено, что в обоих случаях преобладающей фазой является карбид кремния кубической структуры (β-SiC), а сопутствующей – стекловидная фаза, образованная силикатами кальция, магния и железа. При карбидизации шихты, содержащей микрокремнезем производства ферросилиция, карбиду кремния сопутствует α-железо. При температуре синтеза 1923 и 1973 К и продолжительности синтеза 50 и 90 мин происходит полиморфное превращение β-SiC в α-SiCII . Содержание карбида кремния в продуктах карбидизации составляет 82,52 – 84,90 %. Установлены целесообразность и оптимальные условия химического обогащения карбида кремния: воздействие соляной кислотой концентрации не менее 35 % при температуре 353 К, отношении Т:Ж = 1:2, длительности 3 ч. Определены показатели химического обогащения: содержание карбида кремния в продуктах обогащения 90,42 – 91,10 %, удаление примесей оксидов металлов и железа на 87 – 95 %. Карбид кремния представляет собой микропорошок с частицами неправильной формы размерного диапазона 0,2 – 1,0 мкм с удельной поверхностью 8000 – 9000 м2/кг.</p></abstract><trans-abstract xml:lang="en"><p>The paper describes the conducted physical-chemical certification of silicone carbide, obtained from fine-grained charge of two kinds, which contains microsilica formed at the production of silicon and high-silicon ferrosilicium, as well as semicoke from brown coal of Beresovskii deposit of Kansk-Achinsk basin. Microsilca of both kinds contains 93.41 – 95.33 % and 91.72 – 93.00 %, 63 % of SiO2 ; 1.96 – 3.28 % and 0.56 – 1.18 % of Ссвоб. ; 0.30 – 0.34 % and 0.18 – 0.20 % of Siсвоб. ; 1.25 – 1.45 % and 1.38 – 2.32 % of (CaO + Fe2O3 + MnO). Microsilica has a specific surface of 21 000 – 24 000 m2/kg and is inclined to aggregation with the formation of spherical units with the size of 200 – 800 nm. The units consist of spherical particles with a dimensional diapason from 30 to 100 nm. Brown-coal semicoke contains 94.05 % of carbon; 9.2 % of ash; 0.2 % of sulfur; 0.007 % of phosphorus and has a specific surface of 264 000 kg/m2. Phase and chemical compositions of silicone carbide, its specific surface, the size and the form of carbide particles have been studied. It has been established that in both cases predominate phase is silicon carbide of a cubical structure (β-SiC), but an accompanied one is a glassy phase, formed with lime silicate, magnesium and iron. At carburizing of charge, containing microsilca of the production of ferrosilicium, α-iron accompanies to silicon carbide. At the synthesis temperature of 1923 and 1973 K and the duration of 50 and 90 minutes polymorthic transformation of β-SiC into α-SiCII occurs. The content of silicon carbide in the products of carbonization is 82,52 – 84,90 %. The authors of the work have established the viability and optimal conditions of chemical enrichment of silicon carbide: influence of hydrochloric acid with the concentration of not less than 35 % at the temperature of 353 K, ratio of Т:Ж = 1:2, durability of 3 hours. The indexes of chemical enrichment have been defined: the content of silicon carbide in the products of enrichment is 90.42 – 91.10 %, removal of impurities of metal and iron oxides of 87 – 95 %. Silicon carbide appears as micropowder with the particles of wrong form with the dimensional range of 0.2 – 1.0 um with the specific surface of 8000 – 9000 m2/kg.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>карбид кремния</kwd><kwd>микропорошок</kwd><kwd>микрокремнезем</kwd><kwd>буроугольный полукокс</kwd><kwd>карбидизация</kwd><kwd>химическое обогащение</kwd><kwd>фазовый и химический составы</kwd><kwd>размер и морфология частиц</kwd></kwd-group><kwd-group xml:lang="en"><kwd>silicon carbide</kwd><kwd>micropowder</kwd><kwd>microsilica</kwd><kwd>brown-coal semicoke</kwd><kwd>carbonization</kwd><kwd>chemical enrichment</kwd><kwd>phase and chemical compositions</kwd><kwd>size and morphology of a particle</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Министерство образования и науки Российской Федерации (№ 11.1531.2014/К)</funding-statement><funding-statement xml:lang="en">Russian Ministry of Education and Science (no. 11.1531.2014/K)</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">Гаршин А.П., Шумячер В.М., Пушкарев О.И. 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