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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">10.31242/2618-9712-2022-27-4-572-591</article-id><article-id custom-type="elpub" pub-id-type="custom">resar-79</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>Общая биология. Экология</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>General biology. Ecology</subject></subj-group></article-categories><title-group><article-title>Анализ гидрохимического режима наиболее крупных озер города Якутска</article-title><trans-title-group xml:lang="en"><trans-title>Analysis of the hydrochemical conditions of the largest lakes in Yakutsk</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-1556-9182</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Легостаева</surname><given-names>Я. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Legostaeva</surname><given-names>Y. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>ЛЕГОСТАЕВА Яна Борисовна, ведущий научный сотрудник</p><p>677980, г. Якутск, пр. Ленина, 41</p></bio><bio xml:lang="en"><p>LEGOSTAEVA, Yana Borisovna, Leading Researcher</p><p>39 Lenina pr., Yakutsk 677980</p></bio><email xlink:type="simple">ylego@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/0000-0003-2216-3866</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Руфова</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Rufova</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>РУФОВА Алена Афанасьевна, младший научный сотрудник</p><p>677980, г. Якутск, пр. Ленина, 33</p></bio><bio xml:lang="en"><p>RUFOVA, Alena Afanasievna, Junior Researcher</p><p>33 Lenina pr., Yakutsk 677980</p></bio><email xlink:type="simple">alenaruf@inbox.ru</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт геологии алмаза и благородных металлов СО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Diamond and Precious Metal Geology Institute, 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>Академия наук РС (Я)</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Academy of Sciences of the Republic of Sakha (Yakutia)</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>09</day><month>09</month><year>2022</year></pub-date><volume>27</volume><issue>4</issue><fpage>572</fpage><lpage>591</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Легостаева Я.Б., Руфова А.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Легостаева Я.Б., Руфова А.А.</copyright-holder><copyright-holder xml:lang="en">Legostaeva Y.B., Rufova A.A.</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/79">https://resar.elpub.ru/jour/article/view/79</self-uri><abstract><p>Проведен ретроспективный анализ гидрохимического режима наиболее крупных озер г. Якутск (Белое, Хатынг-Юрях, Ытык-Кюель, Сергелях, Сайсары) на основе созданной базы данных, охватывающей период с 1985 по 2021 г. Изучаемые озера преимущественно гидрокарбонатно-натриевые с повышенной минерализацией и умеренно-жесткой водой. В суммарный объем катионов основной вклад вносят Na+ и Ca2+, анионов – HCO3 – и Cl– . Прослеживается снижение минерализации с невысокой достоверностью аппроксимации. Вариации значений жесткости воды напрямую зависят от содержания катионов Ca2+ и Mg2+ и гидрокарбонатов. Среднее содержание взвешенных веществ значительно выше существующих ПДКкб, изменение концентраций в каждом озере носит индивидуальный характер, наиболее высокая обнаружена в озерах Белое, Сайсары и Хатынг-Юрях. Наиболее значимыми факторами в формировании гидрохимического режима являются минерализация и жесткость воды. Установленные закономерности характерны в целом для всей выборки, что отражает специфику формирования гидрохимического режима городских озер. Микроэлементный состав характеризуется повышением концентраций Zn и Cu.</p></abstract><trans-abstract xml:lang="en"><p>A retrospective analysis of the hydrochemical conditions of the largest lakes in Yakutsk (Beloe, Khatyng-Yuryakh, Ytyk-Kuel, Sergelyakh, Saysary) was carried out in accordance with a registered database covering the period from 1985 to 2021. The studied lakes are mainly sodium bicarbonate with increased mineralization and moderately hard water. The main contribution to the total volume of cations is made by Na+ and Ca2+ , HCO3 – and Cl– anions. They also demonstrate a decrease in mineralization with a low value of approximation reliability. The variation of water hardness values directly depends on the content of Ca2+ and Mg2+ cations and hydrocarbonates. The average value of suspended materials in the lakes is significantly higher than the existing Maximum Concentration Limit (MCL). The change in their content in each lake is individual, however the highest was found in Beloe, Saysary and Khatyng-Yuryah lakes. Mineralization and hardness of water are the most significant factors in the formation of the hydrochemical conditions. The established mechanisms are characteristic of the whole sample, which reflects the nature of the formation of the hydrochemical conditions of urban lakes. The trace element composition is characterized by an increase in Zn and Cu concentrations.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>антропогенное воздействие</kwd><kwd>озерные экосистемы</kwd><kwd>городские озера</kwd><kwd>ретроспективный анализ</kwd></kwd-group><kwd-group xml:lang="en"><kwd>anthropogenic impact</kwd><kwd>lake ecosystems</kwd><kwd>urban lakes</kwd><kwd>retrospective analysis</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена в рамках Государственного задания АН РС (Я) «Анализ экологической обстановки регионов Якутии, выявление неблагоприятных зон и факторов, отрицательно влияющих на экологическую безопасность» и Государственного задания ИГАБМ СО РАН (FUEM-2019-0003).</funding-statement><funding-statement xml:lang="en">This study was carried out within the framework of the State Assignment to the Academy of Sciences of the Republic of Sakha (Yakutia) on the project “Analysis of the ecological situation in Yakutia, identification of unfavorable zones and factors negatively affecting environmental safety” and the State Assignment to the Diamond and Precious Metal Geology Institute SB RAS (project number FUEM-2019-0003).</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">Noori R. et al. 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