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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="en"><front><journal-meta><journal-id journal-id-type="publisher-id">gscience</journal-id><journal-title-group><journal-title xml:lang="en">Mining Science and Technology (Russia)</journal-title><trans-title-group xml:lang="ru"><trans-title>Горные науки и технологии</trans-title></trans-title-group></journal-title-group><issn pub-type="epub">2500-0632</issn><publisher><publisher-name>The National University of Science and Technology MISiIS (NUST MISIS)</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.17073/2500-0632-2021-3-181-191</article-id><article-id custom-type="elpub" pub-id-type="custom">gscience-289</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="en"><subject>SAFETY IN MINING AND PROCESSING INDUSTRY AND ENVIRONMENTAL PROTECTION</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="ru"><subject>ТЕХНОЛОГИЧЕСКАЯ БЕЗОПАСНОСТЬ В МИНЕРАЛЬНО-СЫРЬЕВОМ КОМПЛЕКСЕ И ОХРАНА ОКРУЖАЮЩЕЙ СРЕДЫ</subject></subj-group></article-categories><title-group><article-title>Chemical reactions and conditions of mineral formation at tailings storage facilities of the Russian Far East</article-title><trans-title-group xml:lang="ru"><trans-title>Химические реакции и условия минералообразования на хвостохранилищах Дальнего Востока России</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-8288-0993</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Зверева</surname><given-names>В. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Zvereva</surname><given-names>V. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Валентина Павловна Зверева – доктор геолого-минералогических наук, главный научный сотрудник, Лаборатория геохимии гипергенных процессов</p><p>Scopus ID 14628094500</p><p>ResearcherID D-6017-2014</p><p>г. Владивосток</p></bio><bio xml:lang="en"><p>Valentina P. Zvereva – Dr. Sci. (Geol. and Min.), Chief Researcher, Laboratory of Hypergene Processes Geochemistry</p><p>Scopus ID 14628094500</p><p>ResearcherID D-6017-2014</p><p>Vladivostok</p></bio><email xlink:type="simple">zvereva@fegi.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-6122-2980</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Фролов</surname><given-names>К. Р.</given-names></name><name name-style="western" xml:lang="en"><surname>Frolov</surname><given-names>K. R.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Константин Русланович Фролов – кандидат химических наук, старший преподаватель, Базовая кафедра химических и ресурсосберегающих технологий</p><p>Scopus ID 55570105700</p><p>ResearcherID Q-1471-2016</p><p>г. Владивосток</p></bio><bio xml:lang="en"><p>Konstantin R. Frolov – Cand. Sci. (Chem.), Associate Professor, Department of Petroleum Technology and Petrochemicals</p><p>Scopus ID 55570105700</p><p>ResearcherID Q-1471-2016</p><p>Vladivostok</p><p> </p></bio><email xlink:type="simple">frolov.kr@dvfu.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-6439-0736</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Лысенко</surname><given-names>А. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Lysenko</surname><given-names>A. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Анастасия Игоревна Лысенко – кандидат химических наук, научный сотрудник, Лаборатория геохимии гипергенных процессов</p><p>Scopus ID 55569808000</p><p>г. Владивосток</p></bio><bio xml:lang="en"><p>Anastasiya I. Lysenko – Cand. Sci. (Chem.), Researcher, Laboratory of Hypergene Processes Geochemistry</p><p>Scopus ID 55569808000</p><p>Vladivostok</p></bio><email xlink:type="simple">zvereva@fegi.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Дальневосточный геологический институт ДВО РАН<country>Россия</country></aff><aff xml:lang="en">Far East Geological Institute, Far Eastern Branch of the Russian Academy of Sciences<country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru">Дальневосточный федеральный университет<country>Россия</country></aff><aff xml:lang="en">Far Eastern Federal University<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2021</year></pub-date><pub-date pub-type="epub"><day>13</day><month>10</month><year>2021</year></pub-date><volume>6</volume><issue>3</issue><fpage>181</fpage><lpage>191</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Zvereva V.P., Frolov K.R., Lysenko A.I., 2021</copyright-statement><copyright-year>2021</copyright-year><copyright-holder xml:lang="ru">Зверева В.П., Фролов К.Р., Лысенко А.И.</copyright-holder><copyright-holder xml:lang="en">Zvereva V.P., Frolov K.R., Lysenko A.I.</copyright-holder><license 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://mst.misis.ru/jour/article/view/289">https://mst.misis.ru/jour/article/view/289</self-uri><abstract><p>Cassiterite-sulfide and polymetallic deposits of the Far Eastern Region (FER) were mined by both openpit and underground methods. This resulted in the emerging numerous mine workings and tailings storage facilities (TSFs) (abandoned without reclamation in latest decades) and the formation of mining technogenic mineralogical systems. Sulfide component of minerals in the mining technogenic system is subjected to hypergenic and technogenic processes (oxidation and hydrolysis reactions). As a result, highly concentrated technogenic solutions are formed, from which minerals of various classes precipitate. In this connection the purpose of this study was formulated as follows: to show the possibility of crystallization of technogenic minerals from micropore technogenic solutions. In achieving this goal the following tasks were solved: to demonstrate the possible reactions of oxidation and hydrolysis of technogenic minerals at the tailings storage facilities; to identify Eh-pH parameters of their precipitation from highly concentrated solutions; to determine their possible associations. The studies involved field observations and computations with the use of “Selector” software package. The study findings allow demonstrating possible chemical reactions and physico-chemical conditions of mineral formation for the following elements: Fe, Cu, Pb, Zn, Sb, Mg, Al, and Ca, including the following classes of minerals: oxides and hydroxides, sulfates, carbonates, arsenates and silicates. The paper presented for the first time the crystallization reactions of secondary minerals (37 ones) and their physico-chemical conditions. It was found that secondary minerals: jarosite, pitticite, siderite, tenorite, poznyakite, antlerite and ktenasite crystallize in the interval of positive temperatures, while scorodite, chalcantite, broshantite, cerussite, starkeyite, epsomite and rostite originate in cryogenic conditions (below 0 oC). All other minerals, the possibility of precipitation of which was shown in the paper, crystallized in the whole considered temperature interval, from −25 oС to +45 oС. Field studies and modeling data on formation of technogenic waters (solutions) and crystallization of secondary minerals on the surface of and inside tailings at the tailings storage facilities of the Far East showed high intensity of technogenic processes. Since the tailings storage facilities were not reclaimed, the process of environmental pollution, including the hydrosphere, would last for many decades.</p></abstract><trans-abstract xml:lang="ru"><p>Касситерит-сульфидные и полиметаллические месторождения дальневосточного региона отрабатывались как открытым, так и подземным способами, что привело к появлению многочисленных горных выработок и хвостохранилищ (в период перестройки брошены без рекультивации), а также к формированию горнопромышленных техногенных систем. Сульфидная составляющая полезных ископаемых в горнопромышленной техногенной системе подвергается гипергенным и техногенным процессам (реакциям окисления и гидролиза). В результате формируются высококонцентрированные техногенные воды, из которых выпадают минералы из различных классов. В связи с этим сформулирована цель данной работы – показать возможность кристаллизации техногенных минералов из микропоровых растворов техногенных вод. При достижении данной цели решались следующие задачи: показать возможные реакции окисления и гидролиза техногенного минералообразования на хвостохранилищах; выявить Eh-pH параметры их выпадения из высококонцентрированных растворов; определить их возможные ассоциации. Исследования проведены с помощью натурных наблюдений и программного комплекса «Селектор». Полученные результаты позволяют продемонстрировать возможные химические реакции и физико-химические условия формирования минералов: Fe, Cu, Pb, Zn, Sb, Mg, Al и Ca из различных классов: оксидов и гидроксидов, сульфатов, карбонатов, арсенатов и силикатов. В статье впервые показаны реакции кристаллизации вторичных минералов (37 наименований) и их физико-химические условия. Установлено, что в интервале положительных температур кристаллизуются вторичные минералы: ярозит, питтицит, сидерит, тенорит, познякит, антлерит и ктенасит, а в криогенных условиях: скородит, халькантит, брошантит, церуссит, старкеит, эпсомит и ростит. Все остальные минералы, возможность выпадения которых показана в статье, кристаллизуются во всем рассматриваемом интервале – от –25 до +45 ºС. Натурные наблюдения и полученные при моделировании данные по формированию техногенных вод и кристаллизации вторичных минералов на поверхности и в толще хвостов обогащения на хвостохранилищах Дальнего Востока позволили показать высокую активность техногенных процессов. Так как хвостохранилища не рекультивированы, то процесс загрязнения окружающей среды, включая гидросферу, продлится на многие десятилетия.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>горное дело</kwd><kwd>полезные ископаемые</kwd><kwd>обогащение</kwd><kwd>отходы</kwd><kwd>хвостохранилище</kwd><kwd>техногенные минералы</kwd><kwd>гипергенные минералы</kwd><kwd>сульфиды</kwd><kwd>ассоциация (associare)</kwd><kwd>парагенезис</kwd><kwd>шламовые и дренажные воды</kwd></kwd-group><kwd-group xml:lang="en"><kwd>mining</kwd><kwd>minerals</kwd><kwd>beneficiation</kwd><kwd>wastes</kwd><kwd>tailings storage facility</kwd><kwd>technogenic minerals</kwd><kwd>hypergene minerals</kwd><kwd>sulfides</kwd><kwd>association</kwd><kwd>paragenesis</kwd><kwd>slime and drainage waters</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">Булавко Н. В. 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