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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">Ice and Snow</journal-id><journal-title-group><journal-title xml:lang="en">Ice and Snow</journal-title><trans-title-group xml:lang="ru"><trans-title>Лед и снег</trans-title></trans-title-group></journal-title-group><issn publication-format="print">2076-6734</issn><issn publication-format="electronic">2412-3765</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">688414</article-id><article-id pub-id-type="doi">10.31857/S2076673425020124</article-id><article-id pub-id-type="edn">FOALPV</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Applied studies</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Прикладные исследования</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">Analysis of ice cuttings collected during drilling of the snow-firn layer at Vostok station</article-title><trans-title-group xml:lang="ru"><trans-title>Анализ ледяного шлама, полученного при бурении снежно-фирновой толщи на станции Восток</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Vasilev</surname><given-names>D. A.</given-names></name><name xml:lang="ru"><surname>Васильев</surname><given-names>Д. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vasilev_da@pers.spmi.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Rakitin</surname><given-names>I. V.</given-names></name><name xml:lang="ru"><surname>Ракитин</surname><given-names>И. В.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vasilev_da@pers.spmi.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Ignatev</surname><given-names>S. A.</given-names></name><name xml:lang="ru"><surname>Игнатьев</surname><given-names>С. А.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vasilev_da@pers.spmi.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Bolshunov</surname><given-names>A. V.</given-names></name><name xml:lang="ru"><surname>Большунов</surname><given-names>А. В.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vasilev_da@pers.spmi.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Ozhigin</surname><given-names>A. Yu.</given-names></name><name xml:lang="ru"><surname>Ожигин</surname><given-names>А. Ю.</given-names></name></name-alternatives><address><country country="RU">Russian Federation</country></address><email>Vasilev_da@pers.spmi.ru</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Saint Petersburg Mining University</institution></aff><aff><institution xml:lang="ru">Санкт-Петербургский горный университет</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2025-09-04" publication-format="electronic"><day>04</day><month>09</month><year>2025</year></pub-date><volume>65</volume><issue>2</issue><issue-title xml:lang="en"/><issue-title xml:lang="ru"/><fpage>357</fpage><lpage>372</lpage><history><date date-type="received" iso-8601-date="2025-07-28"><day>28</day><month>07</month><year>2025</year></date><date date-type="accepted" iso-8601-date="2025-07-28"><day>28</day><month>07</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2025, Vasilev D.A., Rakitin I.V., Ignatev S.A., Bolshunov A.V., Ozhigin A.Y.</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2025, Васильев Д.А., Ракитин И.В., Игнатьев С.А., Большунов А.В., Ожигин А.Ю.</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="en">Vasilev D.A., Rakitin I.V., Ignatev S.A., Bolshunov A.V., Ozhigin A.Y.</copyright-holder><copyright-holder xml:lang="ru">Васильев Д.А., Ракитин И.В., Игнатьев С.А., Большунов А.В., Ожигин А.Ю.</copyright-holder><license><ali:license_ref xmlns:ali="http://www.niso.org/schemas/ali/1.0/">http://creativecommons.org/licenses/by/4.0</ali:license_ref></license></permissions><self-uri xlink:href="https://journals.eco-vector.com/2076-6734/article/view/688414">https://journals.eco-vector.com/2076-6734/article/view/688414</self-uri><abstract xml:lang="en"><p>The size and shape of the ice cuttings influence the choice of drilling regimes, as well as the design of drilling heads, augers, chip chambers, and internal drilling channels. To collect ice chips, two boreholes, VK-22 (30 m) and VK-23 (40 m), were drilled at Vostok station. Sieving was used to analyze the particle size distribution of the ice cuttings at full depth in both boreholes. The shape of the ice particles was examined microscopically at drilling depths of 5, 10, 15, 20, 25, 30, and 35 m of VK-23. The density of the snow-firn layer and the bulk density of ice cuttings were measured. The ice cuttings became finer-grained as the borehole depth increased. The prevailing fraction changes from 1.6–3 mm to 0.4–0.63 mm, the average particle diameter reduces from 1.55 mm to 0.06 mm, and the <italic>D</italic>10, <italic>D</italic>50, and <italic>D</italic>90 values decrease more than twice. The shape analysis revealed that the ice chips are dominated by equant and elongated particles, with medium shape projections described by parameters <italic>FF</italic> = 0.74 and <italic>ER</italic> = 0.67. A visual comparison of microscopic images shows that the thickness of the ice cuttings decreases as the depth of the well increases.</p></abstract><trans-abstract xml:lang="ru"><p>Установлены и описаны зависимости изменения размера и формы ледяного шлама снежно-фирновой толщи района станции Восток с учётом плотности массива и механической скорости бурения. Предложена классификация формы частиц ледяного шлама и её аппроксимация к эллипсоиду. Рассмотрена практическая значимость полученных данных при разработке техники и технологий бурения верхних горизонтов ледников.</p></trans-abstract><kwd-group xml:lang="en"><kwd>Antarctic</kwd><kwd>ice drilling</kwd><kwd>snow-firn layer</kwd><kwd>ice cuttings</kwd><kwd>size distribution</kwd><kwd>shape characteristics</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>Антарктида</kwd><kwd>бурение во льду</kwd><kwd>снежно-фирновый слой</kwd><kwd>ледяной шлам</kwd><kwd>гранулометрический анализ</kwd><kwd>характеристики формы</kwd></kwd-group><funding-group><funding-statement xml:lang="en">The research was performed at the expense of the subsidy for the state assignment in the field of scientific activity for 2024 № FSRW-2024-0003.</funding-statement><funding-statement xml:lang="ru">Исследование выполнено с помощью субсидии на выполнение государственного задания в сфере научной деятельности на 2024 г. № FSRW-2024-0003.</funding-statement></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><citation-alternatives><mixed-citation xml:lang="en">Bolshunov A.V., Vasilev D.A., Dmitriev A.N., Ignatev S.A., Kadochnikov V.G., Krikun N.S., Serbin D.V., Shadrin V.S. 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