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    <journal-meta>
      <journal-id journal-id-type="issn">2411-3336</journal-id>
      <journal-id journal-id-type="eissn">2541-9404</journal-id>
      <journal-title-group>
        <journal-title xml:lang="ru">Записки Горного института</journal-title>
        <journal-title xml:lang="en">Journal of Mining Institute</journal-title>
      </journal-title-group>
      <publisher>
        <publisher-name xml:lang="ru">Санкт-Петербургский горный университет императрицы Екатерины ΙΙ</publisher-name>
        <publisher-name xml:lang="en">Empress Catherine II Saint Petersburg Mining University</publisher-name>
      </publisher>
    </journal-meta>
    <article-meta>
      <article-id custom-type="edn" pub-id-type="custom">UOUEJM</article-id>
      <article-id custom-type="pmi" pub-id-type="custom">pmi-16706</article-id>
      <article-id pub-id-type="uri">https://pmi.spmi.ru/pmi/article/view/16706</article-id>
      <article-categories>
        <subj-group subj-group-type="section-heading" xml:lang="ru">
          <subject>Геотехнология и инженерная геология</subject>
        </subj-group>
        <subj-group subj-group-type="section-heading" xml:lang="en">
          <subject>Geotechnical Engineering and Engineering Geology</subject>
        </subj-group>
      </article-categories>
      <title-group>
        <article-title xml:lang="en">Gold sorption on modified saponite</article-title>
        <trans-title-group xml:lang="ru">
          <trans-title>Сорбция золота на модифицированном сапоните</trans-title>
        </trans-title-group>
      </title-group>
      <contrib-group>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Chanturiya</surname>
            <given-names>Valentin A.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Чантурия</surname>
              <given-names>В. А.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Chanturiya</surname>
              <given-names>Valentin A.</given-names>
            </name>
          </name-alternatives>
          <email>vchan@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0002-4410-8182</contrib-id>
          <xref ref-type="aff" rid="aff1"/>
        </contrib>
        <aff-alternatives id="aff1">
          <aff>
            <institution xml:lang="ru">Институт проблем комплексного освоения недр им. академика Н.В.Мельникова РАН (Москва, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Institute of Comprehensive Exploitation of Mineral Resources, RAS (Moscow, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author">
          <name name-style="eastern">
            <surname>Minenko</surname>
            <given-names>Vladimir G.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Миненко</surname>
              <given-names>В. Г.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Minenko</surname>
              <given-names>Vladimir G.</given-names>
            </name>
          </name-alternatives>
          <email>vladi200@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0001-9117-4310</contrib-id>
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        </contrib>
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          <aff>
            <institution xml:lang="ru">Институт проблем комплексного освоения недр им. академика Н.В.Мельникова РАН (Москва, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Institute of Comprehensive Exploitation of Mineral Resources, RAS (Moscow, Russia)</institution>
          </aff>
        </aff-alternatives>
        <contrib contrib-type="author" corresp="yes">
          <name name-style="eastern">
            <surname>Samusev</surname>
            <given-names>Andrei L.</given-names>
          </name>
          <name-alternatives>
            <name name-style="eastern" xml:lang="ru">
              <surname>Самусев</surname>
              <given-names>А. Л.</given-names>
            </name>
            <name name-style="western" xml:lang="en">
              <surname>Samusev</surname>
              <given-names>Andrei L.</given-names>
            </name>
          </name-alternatives>
          <email>Andrey63vzm@mail.ru</email>
          <contrib-id contrib-id-type="orcid">0000-0001-7324-0353</contrib-id>
          <xref ref-type="aff" rid="aff3"/>
        </contrib>
        <aff-alternatives id="aff3">
          <aff>
            <institution xml:lang="ru">Институт проблем комплексного освоения недр им. академика Н.В.Мельникова РАН (Москва, Россия)</institution>
          </aff>
          <aff>
            <institution xml:lang="en">Institute of Comprehensive Exploitation of Mineral Resources, RAS (Moscow, Russia)</institution>
          </aff>
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      <pub-date pub-type="epub" iso-8601-date="2025-10-15">
        <day>15</day>
        <month>10</month>
        <year>2025</year>
      </pub-date>
      <pub-date date-type="collection">
        <year>2025</year>
      </pub-date>
      <volume>276</volume>
      <issue>2</issue>
      <fpage>49</fpage>
      <lpage>57</lpage>
      <history>
        <date date-type="received" iso-8601-date="2025-03-27">
          <day>27</day>
          <month>03</month>
          <year>2025</year>
        </date>
        <date date-type="accepted" iso-8601-date="2025-07-02">
          <day>02</day>
          <month>07</month>
          <year>2025</year>
        </date>
        <date date-type="rev-recd" iso-8601-date="2025-12-30">
          <day>30</day>
          <month>12</month>
          <year>2025</year>
        </date>
      </history>
      <permissions>
        <copyright-statement xml:lang="ru">© 2025 В. А. Чантурия, В. Г. Миненко, А. Л. Самусев</copyright-statement>
        <copyright-statement xml:lang="en">© 2025 Valentin A. Chanturiya, Vladimir G. Minenko, Andrei L. Samusev</copyright-statement>
        <copyright-year>2025</copyright-year>
        <copyright-holder xml:lang="ru">В. А. Чантурия, В. Г. Миненко, А. Л. Самусев</copyright-holder>
        <copyright-holder xml:lang="en">Valentin A. Chanturiya, Vladimir G. Minenko, Andrei L. Samusev</copyright-holder>
        <license license-type="open-access" xlink:href="http://creativecommons.org/licenses/by/4.0" xml:lang="ru">
          <license-p>Эта статья доступна по лицензии Creative Commons Attribution 4.0 International (CC BY 4.0)</license-p>
        </license>
        <license license-type="open-access" xlink:href="http://creativecommons.org/licenses/by/4.0" xml:lang="en">
          <license-p>This article is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0)</license-p>
        </license>
      </permissions>
      <self-uri xlink:type="simple" xlink:href="https://pmi.spmi.ru/pmi/article/view/16706">https://pmi.spmi.ru/pmi/article/view/16706</self-uri>
      <abstract xml:lang="ru">
        <p>Теоретически и экспериментально обоснован перспективный метод модификации сапонита (интеркаляция), обеспечивающий его высокую сорбционную емкость по отношению к золоту. Модификация сапонита, выделенного из оборотной воды хвостохранилища обогатительной фабрики, осуществляется путем перемешивания суспензии минерала и ацетона с поверхностно-активным веществом гексадецилтриметиламмония бромид (CTAB), четырехкратной промывкой этанолом и дистиллированной водой, сушкой. Механизм интеркаляции сапонитсодержащего продукта заключается во внедрении в межслоевое пространство положительно заряженных катионов органических соединений путем катионного обмена или адсорбции, что приводит к расширению слоев минерала, резкому смещению дзета-потенциала в положительную сторону. Появление полос в ИК-спектральном интервале 1460-1490 и 2850-2920 см–1, относящихся к деформационным и валентным колебаниям группы CH2 соответственно, подтверждает успешное внедрение молекул CTAB в структуру минерала. В результате исследований максимальной сорбционной емкости модифицированного сапонита установлено, что при исходной концентрации золота 22,6 мг/л полное извлечение достигается уже через 7,5 мин. Максимальная статическая обменная емкость модифицированного сапонита была достигнута после контакта с третьей порцией свежего золотосодержащего раствора и составила 100,5 мг/г. Изотермы сорбции золота соответствуют модели Ленгмюра, основанной на том, что на поверхности модифицированного сапонита образуется мономолекулярный сорбционный слой, и все активные места обладают равной энергией и энтальпией сорбции. При этом кинетические зависимости сорбции наилучшим образом описываются моделью псевдовторого порядка, предполагающей, что химическая реакция обмена лимитирует процесс сорбции. Установлено, что интеркаляция сапонита гексадецилтриметиламмонием бромида обеспечивает более эффективную сорбцию отрицательно заряженных комплексных ионов золота ([AuCl4]–). Рассчитанная равновесная статическая обменная емкость модифицированного сапонита составила 92-119 мг/г, экспериментально установленная – 102 мг/г.</p>
      </abstract>
      <abstract xml:lang="en">
        <p>A potential method for modifying saponite (intercalation) ensuring its high sorption capacity for gold was theoretically and experimentally substantiated. Saponite isolated from recycled water of processing plant tailings dam is modified by mixing a suspension of the mineral and acetone with the surfactant hexadecyltrimethylammonium bromide (CTAB) followed by four washings with ethanol and distilled water, and drying. The intercalation mechanism of saponite-containing product involves the introduction of positively charged cations of organic compounds into the interlayer space through cation exchange or adsorption, which leads to expansion of mineral layers and an abrupt shift in zeta potential toward the positive side. The appearance of bands in the IR spectral ranges of 1460-1490 and 2850-2920 cm–1 related to the deformation and stretching vibrations of the CH2 group, respectively, confirms the successful incorporation of CTAB molecules into the mineral structure. Studies of the maximum sorption capacity of modified saponite revealed that at initial gold concentration 22.6 mg/l, complete extraction is achieved after 7.5 min. The maximum static exchange capacity of modified saponite was achieved after contact with the third portion of fresh gold-bearing solution and amounted to 100.5 mg/g. Gold sorption isotherms correspond to the Langmuir model which presumes that a monomolecular sorption layer forms on the surface of the modified saponite, and all active sites have equal energy and enthalpy of sorption. The kinetic dependences of sorption are best described by a pseudo-second order model, which presumes that the chemical exchange reaction limits the sorption process. It was found that saponite intercalation with hexadecyltrimethylammonium bromide ensures a more efficient sorption of negatively charged gold complex ions ([AuCl4]–). The calculated equilibrium static exchange capacity of modified saponite was 92-119 mg/g, while the experimentally determined value was 102 mg/g.</p>
      </abstract>
      <kwd-group xml:lang="ru">
        <title>Ключевые слова</title>
        <kwd>органическая модификация</kwd>
        <kwd>сапонит</kwd>
        <kwd>золото</kwd>
        <kwd>сорбция</kwd>
        <kwd>статическая обменная емкость</kwd>
        <kwd>кинетика</kwd>
        <kwd>изотермы сорбции</kwd>
      </kwd-group>
      <kwd-group xml:lang="en">
        <title>Keywords</title>
        <kwd>organic modification</kwd>
        <kwd>saponite</kwd>
        <kwd>gold</kwd>
        <kwd>sorption</kwd>
        <kwd>static exchange capacity</kwd>
        <kwd>kinetics</kwd>
        <kwd>sorption isotherms</kwd>
      </kwd-group>
    </article-meta>
  </front>
  <body/>
  <back>
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