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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">nature</journal-id><journal-title-group><journal-title xml:lang="ru">Природопользование</journal-title><trans-title-group xml:lang="en"><trans-title>Nature Management</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2079-3928</issn><publisher><publisher-name>Институт природопользования НАН Беларуси</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">nature-102</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>ГЕОГРАФИЯ. ГЕОЭКОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>GEOGRAPHY. GEOECOLOGY</subject></subj-group></article-categories><title-group><article-title>Особенности химического состава атмосферных осадков в Минске в 2018–2022 гг.</article-title><trans-title-group xml:lang="en"><trans-title>Features of the chemical composition of atmospheric precipitation in Minsk in 2018–2022</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Какарека</surname><given-names>С. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kakareka</surname><given-names>S. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Сергей Витальевич Какарека, доктор технических наук, профессор, заведующий лабораторией</p><p>лаборатория трансграничного загрязнения</p><p>220076; (ул. Ф. Скорины, 10; Минск</p></bio><bio xml:lang="en"><p>Sergey V. Kakareka, D. Sc. (Technical), Professor, Head of Lab</p><p>Lab of Transboundary Pollution</p><p>220076; 10, F. Skoriny Str.; Minsk</p></bio><email xlink:type="simple">sk001@yandex.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>Кокош</surname><given-names>Ю. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Kokosh</surname><given-names>Yu. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Юлия Геннадьевна Кокош, кандидат географических наук, старший научный сотрудник</p><p>220076; ул. Ф. Скорины, 10; Минск</p></bio><bio xml:lang="en"><p>Yuliya G. Kokosh, Senior Researcher</p><p>220076; 10, F. Skoriny Str.; Minsk</p></bio><email xlink:type="simple">y-kokosh@mail.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>Кудревич</surname><given-names>М. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Kudrevich</surname><given-names>M. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Мария Александровна Кудревич, научный сотрудник</p><p>220076; (ул. Ф. Скорины, 10; Минск</p></bio><bio xml:lang="en"><p>Mariya A. Kudrevich, Researcher</p><p>220076; 10, F. Skoriny Str.; Minsk</p></bio><email xlink:type="simple">kudrevich.mary.1991@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт природопользования НАН Беларуси</institution></aff><aff xml:lang="en"><institution>Institute of Nature Management of the National Academy of Sciences of Belarus</institution></aff></aff-alternatives><pub-date pub-type="collection"><year>2024</year></pub-date><pub-date pub-type="epub"><day>02</day><month>11</month><year>2025</year></pub-date><volume>0</volume><issue>1</issue><fpage>41</fpage><lpage>53</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Какарека С.В., Кокош Ю.Г., Кудревич М.А., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Какарека С.В., Кокош Ю.Г., Кудревич М.А.</copyright-holder><copyright-holder xml:lang="en">Kakareka S.V., Kokosh Y.G., Kudrevich M.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://www.nature-journal.by/jour/article/view/102">https://www.nature-journal.by/jour/article/view/102</self-uri><abstract><p>   Охарактеризованы особенности химического состава атмосферных осадков на территории г. Минска за период с 2018 по 2022 гг. на основе анализа результатов мониторинга химического состава атмосферных осадков на экспериментальной площадке Института природопользования НАН Беларуси. Основное внимание уделено соединениям серы и азота – основным закисляющим и эвтрофирующим соединениям в атмосферных осадках. Установлено, что среднегодовые взвешенные содержания серы в атмосферных осадках за исследуемый период варьировали от 0,29 мг S/л (2018 г.) до 0,47 мг S/л (2021 г.), окисленного азота – от 0,21 мг N/л (2019 г.) до 0,43 мг N/л (2020 г.), восстановленного азота – от 0,20 мг N/л (2019 г.) до 0,89 мг N/л (2020 г.). Выполнено сопоставление данных наблюдений химического состава осадков в г. Минске с динамикой содержания серы и азота в осадках на станциях Совместной программы наблюдений и оценки переноса на большие расстояния загрязняющих воздух веществ в Европе (Программы ЕМЕП); основное внимание уделено станциям, расположенным в странах-соседях Беларуси. Наиболее заметное отклонение среднегодового содержания в атмосферных осадках в г. Минске от диапазона колебаний концентраций в рассматриваемый период на станциях ЕМЕП характерно для восстановленного азота в 2020 г. Величины сухих и влажных выпадений серы и азота по данным наблюдений близки расчетным значениям, полученным в рамках Программы ЕМЕП. Установлено, что модельные величины годовых влажных выпадений в целом близки расчетным по данным мониторинга на экспериментальной площадке. Максимальные уровни выпадений как серы, так и азота, согласно моделированию по Программе ЕМЕП, характерны для 2020 г.; для этого же года характерны пиковые уровни выпадений и по данным измерений на экспериментальной площадке. Выявлена сходимость рядов годового средневзвешенного содержания серы в осадках в г. Минске и на станциях фонового мониторинга Европейской территории России (ЕТР).</p></abstract><trans-abstract xml:lang="en"><p>   The features of the chemical composition of atmospheric precipitation on the territory of Minsk for the period from 2018 to 2022 are characterized based on an analysis of the results of monitoring the chemical composition of atmospheric precipitation at the experimental site of the Institute of Environmental Management of the National Academy of Sciences of Belarus. The main attention is paid to sulfur and nitrogen compounds – the major acidifying and eutrophicating compounds in atmospheric precipitation. It was established that the average annual suspended sulfur content in precipitation during the study period varied from 0.29 mg S/l (2018) to 0.47 mg S/l (2021), oxidized nitrogen – from 0.21 mg N /l (2019) to 0.43 mg N/l (2020), reduced nitrogen – from 0.20 mg N/l (2019) to 0.89 mg N/l (2020). A comparison was made of observation data on the chemical composition of precipitation in Minsk with the dynamics of sulfur and nitrogen content in precipitation at Co-operative Programme for Monitoring and Evaluation of the long-range transmissions of air pollutants in Europe (EMEP Program) stations; the main attention is paid to stations located in neighboring countries to Belarus. The most noticeable deviation of the average annual content in atmospheric precipitation in Minsk from the range of concentration fluctuations during the period under review at EMEP stations is typical for refurbished nitrogen in 2020. The comparison was made of the values of atmospheric deposition of sulfur and nitrogen based on observation data on the chemical composition of atmospheric precipitation in Minsk with the calculated values of dry and wet deposition of sulfur and nitrogen obtained within the framework of the EMEP Program. It has been established that the model values of annual wet deposition are generally close to those calculated from monitoring data at the experimental site. The maximum levels of the deposition of both sulfur and nitrogen, according to modeling by the EMEP Program, are typical for 2020; for the same year is characterized by peak levels of fallout and according to measurements at the experimental site. The convergence of series of annual weighted average sulfur content in precipitation in Minsk and at background monitoring stations in the European territory of Russian Federation (ETR) was revealed.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>атмосферные осадки</kwd><kwd>атмосферные выпадения</kwd><kwd>азот</kwd><kwd>сера</kwd><kwd>закисление</kwd><kwd>эвтрофирование</kwd></kwd-group><kwd-group xml:lang="en"><kwd>precipitation</kwd><kwd>atmospheric deposition</kwd><kwd>nitrogen</kwd><kwd>sulfur</kwd><kwd>acidification</kwd><kwd>eutrophication</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">Mehr, M. R. Influence of natural and urban emissions on rainwater chemistry at a southwestern Iran coastal site / M. R. Mehr, B. Keshsvarzi, A. Sorooshian // Sci. Total Environ. – 2019. – Vol. 668. – P. 1213–1221.</mixed-citation><mixed-citation xml:lang="en">Mehr M. 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