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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">litosphere</journal-id><journal-title-group><journal-title xml:lang="ru">Литосфера</journal-title><trans-title-group xml:lang="en"><trans-title>LITHOSPHERE (Russia)</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1681-9004</issn><issn pub-type="epub">2500-302X</issn><publisher><publisher-name>A.N. Zavaritsky Institute of Geology and Geochemistry</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.24930/1681-9004-2024-24-2-254-263</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-2059</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><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Articles</subject></subj-group></article-categories><title-group><article-title>Отрицательное термическое расширение β-Rb2SO4</article-title><trans-title-group xml:lang="en"><trans-title>Negative thermal expansion of β-Rb2SO4</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>Шаблинский</surname><given-names>А. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Shablinskii</surname><given-names>A. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>199034, г. Санкт-Петербург, наб. Макарова, 2</p></bio><bio xml:lang="en"><p>Andrey P. Shablinskii</p><p>2 Makarova emb., 199034 Saint Petersburg</p></bio><email xlink:type="simple">shablinskii.andrey@mail.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>Демина</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Demina</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>199034, г. Санкт-Петербург, наб. Макарова, 2</p><p>199034, г. Санкт-Петербург, Университетская наб., 7/9</p></bio><bio xml:lang="en"><p>Sofya V. Demina</p><p>2 Makarova emb., 199034 Saint Petersburg</p><p>7/9 Universitetskaya emb., 199034 Saint Petersburg</p></bio><email xlink:type="simple">demina.sofiya@bk.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>Бубнова</surname><given-names>Р. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Bubnova</surname><given-names>R. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>199034, г. Санкт-Петербург, наб. Макарова, 2</p></bio><bio xml:lang="en"><p>Rimma S. Bubnova</p><p>2 Makarova emb., 199034 Saint Petersburg</p></bio><email xlink:type="simple">rimma_bubnova@mail.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>Филатов</surname><given-names>С. К.</given-names></name><name name-style="western" xml:lang="en"><surname>Filatov</surname><given-names>S. K.</given-names></name></name-alternatives><bio xml:lang="ru"><p>199034, г. Санкт-Петербург, Университетская наб., 7/9</p></bio><bio xml:lang="en"><p>Stanislav K. Filatov</p><p>7/9 Universitetskaya emb., 199034 Saint Petersburg</p></bio><email xlink:type="simple">ilatov.stanislav@gmail.com</email><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт химии силикатов им. И.В. Гребенщикова, РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Silicate Chemistry, RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт химии силикатов им. И.В. Гребенщикова, РАН; Санкт-Петербургский государственный университет, Институт наук о Земле</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of Silicate Chemistry, RAS; Saint Petersburg State University, Institut des Géosciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>Санкт-Петербургский государственный университет, Институт наук о Земле</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Saint Petersburg State University, Institut des Géosciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>03</day><month>05</month><year>2024</year></pub-date><volume>24</volume><issue>2</issue><fpage>254</fpage><lpage>263</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Шаблинский А.П., Демина С.В., Бубнова Р.С., Филатов С.К., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Шаблинский А.П., Демина С.В., Бубнова Р.С., Филатов С.К.</copyright-holder><copyright-holder xml:lang="en">Shablinskii A.P., Demina S.V., Bubnova R.S., Filatov S.K.</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://www.lithosphere.ru/jour/article/view/2059">https://www.lithosphere.ru/jour/article/view/2059</self-uri><abstract><p>Объект исследования. Низкотемпературная модификация сульфата β-Rb2SO4 (Pmcn). Цель. Низкотемпературное исследование термического расширения β-Rb2SO4 методом порошковой терморентгенографии в сопоставлении с кристаллической структурой, а также трактовка анизотропии термического расширения β-Rb2SO4. Методы. Порошковая рентгенография, порошковая терморентгенография. Результаты. Методом низкотемпературной порошковой терморентгенографии впервые изучено термическое расширение сульфата β-Rb2SO4 в сопоставлении с кристаллической структурой. Фазовый состав подтверждался методом порошковой рентгеновской дифракции. Термическое расширение β-Rb2SO4 практически изотропно. В интервале температур от –177 до –140°C сульфат испытывает отрицательное термическое расширение. Дальнейшее повышение температуры ведет к изменению термического расширения – оно становится положительным. Предложено рассматривать кристаллическую структуру сульфата β-Rb2SO4 как смешанный каркас [RbSO4]–1, который, в свою очередь, состоит из фундаментальных строительных единиц (микроблоков) Rb(SO4)6. В интервале температур от комнатной до –100°С максимальное расширение сульфата β-Rb2SO4 происходит вдоль оси a. Минимальное термическое расширение наблюдается вдоль оси c, вдоль направления простирания колонн, состоящих из микроблоков (αa = 65.4(3)∙10–6°C–1, αb = 59.7(2)∙10–6°C–1, αc = 58.6(2)∙10–6°C–1 при 25°C). В интервале температур –177…–140°C термическое расширение отрицательно по всем трем направлениям (αa = –10.3(3)∙10–6°C–1, αb = –8.6(2)∙10–6°C–1, αc = –9.7(2)∙10–6°C–1 при –170°C). Выводы. Впер вые изучено термическое расширение сульфата β-Rb2SO4 в низкотемпературном интервале (–177…–25°C), дана его структурная трактовка, проведено сопоставление с термическим расширением изоструктурного β-K2SO4.</p></abstract><trans-abstract xml:lang="en"><p>Research subject. The low-temperature modification of β-Rb2SO4 sulfate (Pmcn). Aim. Low-temperature study of the thermal expansion of β-Rb2SO4 by high-temperature powder X-ray diffraction in comparison with the crystal structure, as well as interpretation of the anisotropy of β-Rb2SO4 thermal expansion. Materials and Method. Powder X-ray diffraction and high-temperature powder X-ray diffraction. Results. The thermal expansion of β-Rb2SO4 sulfate was studied for the first time using low-temperature powder thermal X-ray diffraction in comparison with the crystal structure. The phase composition was confirmed by powder X-ray diffraction. The thermal expansion of β-Rb2SO4 is practically isotropic. Across the temperature range from –177 to –140°C, the sulfate experiences negative thermal expansion. A further increase in temperature leads to a change in its thermal expansion, which becomes positive. It is proposed to consider the crystal structure of β-Rb2SO4 sulfate as a mixed framework of [RbSO4]–1, which, in turn, consists of fundamental building units (microblocks) of Rb(SO4)6. Across the temperature range from room temperature to –100°C, the maximum expansion of β-Rb2SO4 sulfate occurs along the a axis. The minimum thermal expansion is observed along the c-axis, along the columns consisting of microblocks (αa = 65.4(3)∙10–6°C–1, αb = 59.7(2)∙10–6°C–1, αc = 58.6(2)∙10–6°C–1 at +25°C). In the temperature range from –177 to –140°C, thermal expansion is negative in all three directions (αa = –10.3(3)∙10–6°C–1, αb = –8.6(2)∙10–6°C–1, αc = –9.7(2)∙10–6°C–1 at –170°C). Conclusion. The thermal expansion of β-Rb2SO4 sulfate in the low-temperature range (from –177 to –25°C) was studied for the first time, its structural interpretation was performed. A comparison was given with the thermal expansion of isostructural β-K2SO4.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>сульфат рубидия</kwd><kwd>отрицательное термическое расширение</kwd><kwd>порошковая терморентгенография</kwd></kwd-group><kwd-group xml:lang="en"><kwd>rubidium sulfate</kwd><kwd>negative thermal expansion</kwd><kwd>high temperature powder X-ray diffraction</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Рентгеновские эксперименты выполнены с использованием оборудования ресурсного центра СПБГУ “Рентгено-дифракционные методы исследования”. Работа в части проведения рентгеновских экспериментов, интерпретации рентгеновских данных, обобщения полученных результатов поддержана Российским научным фондом (РНФ) (№ 23-77-10066).</funding-statement><funding-statement xml:lang="en">X-ray diffraction experiments were carried out using the equipment of the resource center of St. Petersburg State University “X-ray diffraction research methods”. The work regarding the conduct of X-ray experiments, interpretation of X-ray data, generalization of the results obtained was supported by the Russian Science Foundation (RSF) (No. 23-77-10066).</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">Бубнова Р.С., Фирсова В.А., Волков С.Н., Филатов С.К. (2018) RietveldToTensor: программа для обработки порошковых рентгендифракционных данных, полученных в переменных условиях. Физика и химия стекла, 44(1), 48-60.</mixed-citation><mixed-citation xml:lang="en">Aksenov S.M., Deyneko D.V. (2022) Crystal chemistry and design of new materials with mineral-related structures: the structure-properties relationship. 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