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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">resar</journal-id><journal-title-group><journal-title xml:lang="ru">Природные ресурсы Арктики и Субарктики</journal-title><trans-title-group xml:lang="en"><trans-title>Arctic and Subarctic Natural Resources</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2618-9712</issn><issn pub-type="epub">2686-9683</issn><publisher><publisher-name>Академия наук Республики Саха (Якутия)</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.31242/2618-9712-2024-29-4-562-573</article-id><article-id custom-type="elpub" pub-id-type="custom">resar-596</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>Биологические науки. Экология</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Biological sciences. Ecology</subject></subj-group></article-categories><title-group><article-title>Влияние крупных лесных пожаров на мерзлотные палевые почвы Лено-Вилюйского водораздела</article-title><trans-title-group xml:lang="en"><trans-title>The impact of large forest fires on frozen pale soils in the Lena-Vilyui watershed</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-1289-5433</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Десяткин</surname><given-names>Р. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Desyatkin</surname><given-names>R. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Десяткин Роман Васильевич, доктор биологических наук, главный научный сотрудник</p><p>ResearcherID: K-5281-2018, Scopus Author ID: 6507832825</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Desyatkin Roman Vasilievich, Dr. Sci. (Biol.), Chief Researcher</p><p>ResearcherID: K-5281-2018, Scopus Author ID: 6507832825</p><p>Yakutsk</p></bio><email xlink:type="simple">rvdes@ibpc.ysn.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-8501-6807</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Иванова</surname><given-names>А. З.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanova</surname><given-names>A. Z.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Иванова Александра Зуевна, младший научный сотрудник, 89248654037</p><p>ResearcherID: J-6741-2018, Scopus Author ID: 57216969934</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Ivanova Alexandra Zuevna, Junior Researcher</p><p>ResearcherID: J-6741-2018, Scopus Author ID: 57216969934</p><p>Yakutsk</p></bio><email xlink:type="simple">madalexia@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-9597-999X</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Десяткин</surname><given-names>А. Р.</given-names></name><name name-style="western" xml:lang="en"><surname>Desyatkin</surname><given-names>A. R.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Десяткин Алексей Романович, научный сотрудник, PhD</p><p>ResearcherID: G-1918-2016, Scopus Author ID: 160215-000377</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Desyatkin Alexey Romanovich, PhD, Researcher</p><p>ResearcherID: G-1918-2016, Scopus Author ID: 160215-000377</p><p>Yakutsk</p></bio><email xlink:type="simple">desyatkinar@rambler.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-0160-2295</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Николаева</surname><given-names>М. Х.</given-names></name><name name-style="western" xml:lang="en"><surname>Nikolaeva</surname><given-names>M. Ch.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Николаева Майя Христофоровна, младший научный сотрудник</p><p>ResearcherID: N-6732-2019, Scopus Author ID: 34875605400</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Nikolaeva Maya Christophorovna, Junior Researcher</p><p>ResearcherID: N-6732-2019, Scopus Author ID: 34875605400</p><p>Yakutsk</p></bio><email xlink:type="simple">mayan34@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-0463-3123</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Филиппов</surname><given-names>Н. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Filippov</surname><given-names>N. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Филиппов Николай Васильевич, инженер-исследователь</p><p>ResearcherID: J-6803-2018, Scopus Author ID: 57202088215</p><p>г. Якутск</p></bio><bio xml:lang="en"><p>Filippov Nikolai Vasilievich, Research Engineer</p><p>ResearcherID: J-6803- 2018, Scopus Author ID: 57202088215</p><p>Yakutsk</p></bio><email xlink:type="simple">finiva88@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт биологических проблем криолитозоны СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute for Biological Problems of Cryolithozone, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт биологических проблем криолитозоны СО РАН; Институт мерзлотоведения им. П.И. Мельникова СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute for Biological Problems of Cryolithozone, Siberian Branch of the Russian Academy of Sciences; Melnikov Permafrost Institute, Siberian Branch of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>26</day><month>12</month><year>2024</year></pub-date><volume>29</volume><issue>4</issue><fpage>562</fpage><lpage>573</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Десяткин Р.В., Иванова А.З., Десяткин А.Р., Николаева М.Х., Филиппов Н.В., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Десяткин Р.В., Иванова А.З., Десяткин А.Р., Николаева М.Х., Филиппов Н.В.</copyright-holder><copyright-holder xml:lang="en">Desyatkin R.V., Ivanova A.Z., Desyatkin A.R., Nikolaeva M.C., Filippov N.V.</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://resar.elpub.ru/jour/article/view/596">https://resar.elpub.ru/jour/article/view/596</self-uri><abstract><p>В результате катастрофических пожаров 2021 г. в Центральной Якутии полностью выгорели леса на огромных территориях – погиб древостой, деградировали лесная подстилка и верхние органогенные горизонты почвы. Резко изменился водно-температурный режим мерзлотных почв, развивающихся в условиях близкого залегания многолетнемерзлой толщи к дневной поверхности. Цель работы – изучение влияния пожара на морфологические и физико-химические свойства палевых почв в первые годы после пожара после гибели древостоя, выгорания подстилки и органогенного слоя почвы. Объект исследования – мерзлотные палевые слабоосолоделые суглинистые почвы в лиственничных лесах Лено-Вилюйского водораздела. Дана подробная информация о растительности, морфогенетическом строении почвенных профилей, проведена параметризация полевой влажности, содержания гумуса, потерь при прокаливании, реакции почвенной среды, суммы обменных оснований и гранулометрического состава почв. Выявлено, что поступление на поверхность продуктов горения в виде золы вызывает подщелачивание с параллельным значительным уменьшением содержания органического углерода в поверхностных слоях. Почвы контрольного участка и гари сильно различаются по морфологическому строению: на гари сформирован пирогенный слой небольшой мощности со слабым экранирующим эффектом, активизировались процессы перемешивания грунта, из-за чего нарушаются горизонтально-направленные естественные границы почвенных горизонтов. Уничтожение теплоизолирующего слоя в виде напочвенного покрова и органогенных отложений способствует сильному нагреву почвы, начинается повышение температуры почвенной массы, увеличение глубины сезонного протаивания. Таяние верхних слоев многолетней мерзлоты и освобождение ранее консервированной влаги приводит к насыщению почвы влагой, что при промерзании почв в зимний период активизирует криотурбацию. В почвах, не тронутых пожарами, мерзлотное перемешивание почвенного профиля выражено слабо. Временное переувлажнение почв на плохо дренируемых грунтах в первые годы после пожаров повышает валеж древесного яруса из-за снижения механического сцепления корней деревьев с грунтом.</p></abstract><trans-abstract xml:lang="en"><p>The catastrophic wildfires that occurred in Central Yakutia in 2021 resulted in extensive forest destruction, leading to the complete incineration of significant forested areas. This devastation has caused the loss of tree stands and the degradation of forest litter, as well as the upper organic layers of the soil. Consequently, there has been a substantial alteration in the water-temperature regime of permafrost soils, which are formed under permafrost conditions. The objective of this study is to investigate the impact of these fires on the morphological, physical, and chemical characteristics of pale soils during the initial years following the fire event, specifically after the destruction of the tree stand and the combustion of the litter and organic soil layers. This research primarily focuses on pale, slightly solodized soils located within the larch forests of the Lena-Vilyui watershed. This research presents comprehensive insights into vegetation and the morphogenetic characteristics of soil profiles, alongside the parameterization of various soil properties, including field moisture, humus content, loss on ignition, , reactions of the soil environment, exchangeable base quantities, and granulometric composition. The findings indicate that the deposition of combustion byproducts, specifically in the form of ash, results in soil alkalization, which is associated with a marked decrease in organic carbon levels within the surface strata. Notably, the morphological characteristics of soils in the control area exhibit significant differences compared to those in the burned region; a thin pyrogenic layer with minimal screening effects has developed in the burned region, soil mixing processes have become more pronounced, and the natural horizontal boundaries of soil horizons have been disrupted. The degradation of heat-insulating ground cover and organic matter contributes to substantial soil heating, leading to elevated soil mass temperatures and an extended seasonal thaw. The thawing of upper permafrost layers and the release of previously sequestered moisture result in soil saturation, which, upon winter freeze, triggers cryoturbation. In contrast, soils that have not experienced fire exhibit only a weak expression of permafrost mixing within the soil profile. Furthermore, the temporary waterlogging of poorly drained soils in the initial years post-fire exacerbates tree.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>лесные пожары</kwd><kwd>гарь</kwd><kwd>палевая почва</kwd><kwd>многолетняя мерзлота</kwd><kwd>лиственничник</kwd><kwd>деградация</kwd><kwd>Центральная Якутия</kwd></kwd-group><kwd-group xml:lang="en"><kwd>forest fire</kwd><kwd>burnt forest</kwd><kwd>pale soil</kwd><kwd>permafrost</kwd><kwd>larch</kwd><kwd>degradation</kwd><kwd>Central Yakutia</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках государственного задания Министерства науки и высшего образования РФ (проект № 0297-2021-0026, ЕГИСУ НИОКТР № АААА-А21-121012190036-6).</funding-statement><funding-statement xml:lang="en">This study was conducted within the framework of the state assignment of the Ministry of Science and Higher Education of the Russian Federation (project No. 0297-2021-0026, reg. 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