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<article 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" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Priroda</journal-id><journal-title-group><journal-title xml:lang="en">Priroda</journal-title><trans-title-group xml:lang="ru"><trans-title>Природа</trans-title></trans-title-group></journal-title-group><issn publication-format="print">0032-874X</issn><publisher><publisher-name xml:lang="en">Akademizdatcenter Nauka</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">627936</article-id><article-id pub-id-type="doi">10.7868/S0032874X20120029</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Articles</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Статьи</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">Mixites and petersites: New Data on the Structure of Agardite-(Ce)</article-title><trans-title-group xml:lang="ru"><trans-title>Микситы и петерситы: новые данные о структуре агардита-(Се)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Rastsvetaeva</surname><given-names>R. K</given-names></name><name xml:lang="ru"><surname>Расцветаева</surname><given-names>Р. К</given-names></name></name-alternatives><email>rast.crys@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Aksenov</surname><given-names>S. M</given-names></name><name xml:lang="ru"><surname>Аксёнов</surname><given-names>С. М</given-names></name></name-alternatives><email>aks.crys@gmail.com</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Shubnikov Institute of Crystallography, RAS</institution></aff><aff><institution xml:lang="ru">Институт кристаллографии имени А.В.Шубникова РАН</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2020-12-11" publication-format="electronic"><day>11</day><month>12</month><year>2020</year></pub-date><issue>12</issue><issue-title xml:lang="en">NO12 (2020)</issue-title><issue-title xml:lang="ru">№12 (2020)</issue-title><fpage>11</fpage><lpage>18</lpage><history><date date-type="received" iso-8601-date="2024-03-02"><day>02</day><month>03</month><year>2024</year></date></history><permissions><copyright-statement xml:lang="ru">Copyright ©; 2020, Издательство «Наука»</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Издательство «Наука»</copyright-holder></permissions><self-uri xlink:href="https://journals.eco-vector.com/0032-874X/article/view/627936">https://journals.eco-vector.com/0032-874X/article/view/627936</self-uri><abstract xml:lang="en"><p>Arsenates and phosphates are rare although challenging minerals of the mixite group. Their general formula is ACu6(TO4)3–x(TO3OH)x(OH)6·3H2O, where A = REE, Ca, Pb, Bi3+, Al; T = As5+, P5+; x = 0–1, hexagonal cell parameters a ≈ 13.5 Å, c ≈ 6 Å, V ≈ 900 Å3, and space group P63/m or P63. There are two subgroups in accordance with chemical composition in T-sites: mixite (T = As) and petersite (T = P). Agardit-(Ce) CeCu6(AsO4)3(OH)6·3H2O from Clara Mine, Schwarzwald, Germany, has been investigated. Unit-cell parameters of agaradite-(Ce) are: a = 13.598(6) Å, c = 5.954(3) Å; V = 953.5(2) Å3; space group P63/m. The structure has been specified and refined to final R = 3.87% for 786 I &gt; 3σ(I). For the first time in the structure of minerals of mixite group hydrogen atoms have been localized and hydrogen bonding has been characterized.</p></abstract><trans-abstract xml:lang="ru"><p>К редким, но очень интересным минералам относятся арсенаты и фосфаты группы миксита с общей формулой ACu6(TO4)3–x(TO3OH)x(OH)6·3H2O (где A = REE, Ca, Pb, Bi3+, Al; T = As5+, P5+; x = 0–1), параметрами гексагональной ячейки a ≈ 13.5 Å, c ≈ 6 Å, V ≈ 900 Å3 и с пространственной группой P63/m или P63. С учетом состава в T-позициях выделяются две подгруппы: миксита (T = As) и петерсита (T = P). К первой относится и изученный нами агардит-(Се) — CeCu6(AsO4)3(OH)6·3H2O, который найден в Шварцвальде, на руднике Клара (Германия). Параметры ячейки агардита-(Се): a = 13.598(6) Å, c = 5.954(3) Å; V = 953.5(2) Å3; пространственная группа P63/m, структура уточнена до R = 3.87% с использованием 786 I &gt; 3σ(I). В этой структуре впервые для минералов группы миксита локализованы атомы водорода и исследована система водородных связей.</p></trans-abstract><kwd-group xml:lang="en"><kwd>mixite group</kwd><kwd>agardite-(Ce)</kwd><kwd>crystal structure</kwd><kwd>hydrogen bonding</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>группа миксита</kwd><kwd>агардит-(Ce)</kwd><kwd>кристаллическая структура</kwd><kwd>водородные связи</kwd></kwd-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Walenta K., Theye T. Agardit-(Ce) von der Grube Clara im mittleren Schwarzwald. Aufschluss. 2004; 55: 17–23.</mixed-citation></ref><ref id="B2"><label>2.</label><mixed-citation>Miletich R., Zemann J., Nowak M. Reversible hydration in synthetic mixite, BiCu6(OH)6(AsO4)3·nH2O (n&lt;3): Hydration kinetics and crystal chemistry. 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