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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">geores</journal-id><journal-title-group><journal-title xml:lang="ru">Георесурсы</journal-title><trans-title-group xml:lang="en"><trans-title>Georesources</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1608-5043</issn><issn pub-type="epub">1608-5078</issn><publisher><publisher-name>Georesursy LLC</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.18599/grs.2026.3.12</article-id><article-id custom-type="elpub" pub-id-type="custom">geores-765</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>ПОТЕНЦИАЛ СЕВЕРА ЗАПАДНОЙ СИБИРИ: РЕСУРСЫ И ТЕХНОЛОГИИ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>THE POTENTIAL OF THE NORTH OF WESTERN SIBERIA: RESOURCES AND TECHNOLOGIES</subject></subj-group></article-categories><title-group><article-title>Интеграция результатов капилляриметрии и ЯМР-релаксометрии: от линейной калибровки к нелинейной 2D-интерпретации</article-title><trans-title-group xml:lang="en"><trans-title>Integration of Capillary and NMR Relaxometry Results: From Linear Calibration to Nonlinear 2D Interpretation</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0009-0001-4078-6656</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Хохолков</surname><given-names>А. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Khokholkov</surname><given-names>A. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Алексей Георгиевич Хохолков – кандидат физ.-мат. наук, старший инженер лаборатории петрофизических исследований керна Лабораторно-исследовательского центра</p><p>Тюмень</p></bio><bio xml:lang="en"><p>Alexey G. Khokholkov – Сand. Sci. (Physics and Mathematics), Senior Engineer of the Laboratory of Petrophysical Core Research</p><p>Tyumen</p></bio><email xlink:type="simple">agkhokholkov@novatek.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>Костеневич</surname><given-names>К. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kostenevich</surname><given-names>K. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Кристина Альбертовна Костеневич – начальник исследовательской группы литолого-минералогических исследований керна Лабораторно-исследовательского центра</p><p>Тюмень</p></bio><bio xml:lang="en"><p>Kristina A. Kostenevich – Head of the Research Group for Lithological and Mineralogical Core Studies of the Laboratory Research Center</p><p>Tyumen</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0009-0003-8496-1174</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Корытов</surname><given-names>В. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Korytov</surname><given-names>V. S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Виталий Сергеевич Корытов – заместитель директора Лабораторно- исследовательского центра</p><p>Тюмень</p></bio><bio xml:lang="en"><p>Vitaly S. Korytov – Deputy Director of the Laboratory Research Center</p><p>Tyumen</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ООО «НОВАТЭК НТЦ»</institution><country>Россия</country></aff><aff xml:lang="en"><institution>NOVATEK NTC LLC</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2026</year></pub-date><pub-date pub-type="epub"><day>08</day><month>10</month><year>2026</year></pub-date><volume>28</volume><issue>3</issue><fpage>67</fpage><lpage>81</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Хохолков А.Г., Костеневич К.А., Корытов В.С., 2026</copyright-statement><copyright-year>2026</copyright-year><copyright-holder xml:lang="ru">Хохолков А.Г., Костеневич К.А., Корытов В.С.</copyright-holder><copyright-holder xml:lang="en">Khokholkov A.G., Kostenevich K.A., Korytov V.S.</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.geors.ru/jour/article/view/765">https://www.geors.ru/jour/article/view/765</self-uri><abstract><p>Предложен подход к интерпретации распределений порометрических характеристик (по данным ЯМР-релаксометрии, капилляриметрии методом полупроницаемой мембраны и т.п.), основанный на нелинейном преобразовании (квантильном выравнивании) распределений. В отличие от классических линейных калибровок вида r = cT2 (где r – радиус поры, c – калибровочный коэффициент, T2 – время поперечной ЯМР-релаксации), предлагаемый метод учитывает геометрическую неоднородность порового пространства и позволяет достичь хорошей сопоставимости с экспериментом при восстановлении кривых капиллярного давления по результатам ЯМР. На коллекции из 751 образца керна показано, что имеется корреляция между параметрами нелинейного преобразования и литологическим строением пород. Предложена интерпретация зависимости r ~ T2 n , учитывающая связь между фрактальной размерностью поверхности поры ds и показателем степени n. На ограниченной выборке образцов на основе анализа изображений порового пространства методом box-counting дана оценка диапазонов значений ds для рассматриваемых типов пород. Показано, что кажущиеся значения ds , определенные по зависимости r(T2 ), согласуются с диапазонами, определенными методом box-counting. На примере простой модели машинного обучения (метод kNN) показано, что качество восстановления остаточной водонасыщенности Кво по данным ЯМР-релаксации с использованием рассматриваемого метода соответствует качеству восстановления Кво методом отсечек при обучении на той же выборке, при сопоставимой точности оценки водонасыщенности на остальных ступенях капиллярного давления.</p></abstract><trans-abstract xml:lang="en"><p>An approach to interpreting pore size distributions (derived from NMR relaxometry, mercury injection, and porous plate methods) based on a nonlinear transformation (quantile alignment, or quantile mapping) is proposed. Unlike conventional linear calibrations of the form r = cT2 (where r is the pore radius, c is the calibration coefficient, and T2 is the transverse NMR relaxation time), the proposed method accounts for the geometric heterogeneity of the pore space, enabling a closer match with experimental data when reconstructing capillary pressure curves from NMR results. Based on a dataset of 751 core samples, a correlation was established between the nonlinear transformation parameters and the lithological characteristics of the rocks. An interpretation of the r ~ T2 n relationship is proposed, accounting for the link between the pore surface fractal dimension ds and the exponent n. Based on a limited sample set, ranges of ds values for the considered rock types were estimated through pore-space image analysis using the box-counting method. It is shown that the apparent ds values derived from the r(T2 ) dependence are consistent with the ranges determined by the box‑counting method. Using a simple machine learning model (the k-nearest neighbors method) as an example, it is demonstrated that the quality of residual water saturation Swi recovery from NMR relaxometry data using the considered method corresponds to the quality of Swi recovery by the cut-off method when trained on the same dataset, with comparable accuracy of saturation estimation at other capillary pressure stages.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>ЯМР-релаксометрия</kwd><kwd>кривая капиллярного давления</kwd><kwd>квантильное выравнивание</kwd><kwd>преобразование распределений</kwd><kwd>метод ближайших соседей</kwd><kwd>фрактальная размерность</kwd></kwd-group><kwd-group xml:lang="en"><kwd>NMR relaxometry</kwd><kwd>capillary pressure curve</kwd><kwd>quantile alignment</kwd><kwd>distribution transformation</kwd><kwd>k-nearest neighbors method</kwd><kwd>fractal dimension</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">МакФи К., Рид Дж., Зубизаретта И. 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