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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">boolt</journal-id><journal-title-group><journal-title xml:lang="ru">Бюллетень Государственного Никитского ботанического сада</journal-title><trans-title-group xml:lang="en"><trans-title>Bulletin of the State Nikitsky Botanical Gardens</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0513-1634</issn><publisher><publisher-name>Federal State Funded Institution of Science “The Labour Red Banner Order Nikitsky Botanical Gardens – National scientific Center of the RAS”</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.36305/0513-1634-2022-142-129-140</article-id><article-id custom-type="elpub" pub-id-type="custom">boolt-586</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>АГРОЭКОЛОГИЯ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>AGROECOLOGY</subject></subj-group></article-categories><title-group><article-title>Сезонная динамика минерального состава грунтовых вод на территории палеовулкана</article-title><trans-title-group xml:lang="en"><trans-title>SEASONAL DYNAMICS OF GROUNDWATER MINERAL COMPOSITION AT THE TERRITORY OF THE CRIMEAN PALEOVOLCANO</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>Голубкина</surname><given-names>Н. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Golubkina</surname><given-names>Nadezhda</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.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>Лапченко</surname><given-names>В. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Lapchenko</surname><given-names>Vladimir</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Лапченко</surname><given-names>Е. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Lapchenko</surname><given-names>Helene</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Зуев</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Zuev</surname><given-names>Alexander</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Карузо</surname><given-names>Дж. .</given-names></name><name name-style="western" xml:lang="en"><surname>Caruso</surname><given-names>Gianluca</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-3"/></contrib></contrib-group><aff xml:lang="en" id="aff-1"><institution>Federal Scientific Vegetable Center</institution><country>Russian Federation</country></aff><aff xml:lang="en" id="aff-2"><institution>Т.I. Vyazemsky Karadag Scientific Station- Nature Reserve RAS - Branch of A. O. Kovalevsky Institute of Biology of the Southern Seas of RAS</institution><country>Russian Federation</country></aff><aff xml:lang="en" id="aff-3"><institution>University of Naples Federico II</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2022</year></pub-date><pub-date pub-type="epub"><day>11</day><month>05</month><year>2022</year></pub-date><volume>0</volume><issue>142</issue><fpage>129</fpage><lpage>140</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Голубкина Н.А., Лапченко В.А., Лапченко Е.В., Зуев А.В., Карузо Д..., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Голубкина Н.А., Лапченко В.А., Лапченко Е.В., Зуев А.В., Карузо Д...</copyright-holder><copyright-holder xml:lang="en">Golubkina N., Lapchenko V., Lapchenko H., Zuev A., Caruso G.</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://boolt.elpub.ru/jour/article/view/586">https://boolt.elpub.ru/jour/article/view/586</self-uri><abstract><p>Проведена оценка сезонной динамики концентраций 25 элементов в подземных водах Карадага. Были зарегистрированы повышенные уровни B, Li и Se, а также отрицательные корреляции между минерализацией воды и скоростью потока источников, и расстоянием от берега моря (r = -0,840 и r = -0,945), а также высокие сезонные колебания уровней P и K (78-130% и 80-118% соответственно). Положительные корреляции были обнаружены между Ca, Mg, Sr (r = 0,82-0,96); Li, B, Na (r = 0,72-0,90); Li, Na, минерализация (r = 0,80-0,90) и Se, Na (r = 0,551). Самые высокие концентрации P, K, Si, Na были зарегистрированы весной, B, Zn, Fe, Se, F осенью; Са, Se, F, Cl, I зимой и Sr весной и осенью. Ca, K, Mg, Na, B, Fe, Li, минерализация и жесткость воды родниковой воды биостанции продемонстрировали высокие сезонные колебания и превышение предельно допустимых концентраций.</p></abstract><trans-abstract xml:lang="en"><p>Seasonal dynamics of 25 elements concentrations in Karadag groundwater was evaluated. Increased levels of B, Li and Se were recorded, along with negative correlations between water mineralization and both flow rate of springs and the distance from the seashore (r = -0.840 and r = -0.945), as well as high seasonal variations of P and K levels (78-130% and 80-118% respectively). Positive correlations were found between Ca, Mg, Sr (r = 0.82-0.96); Li, B, Na (r = 0.72-0.90); Li, Na, mineralization (r = 0.80-0.90) and Se, Na (r = 0.551). The highest concentrations of P, K, Si, Na were registered in spring, B, Zn, Fe, Se, F in autumn; Са, Se, F, Cl, I in winter, and Sr in spring and autumn. Ca, K, Mg, Na, B, Fe, Li, mineralization and water hardness of Bio-station well water demonstrated high seasonal variations and maximum permissible concentrations excess.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>подземные воды</kwd><kwd>минеральный состав</kwd><kwd>сезонные колебания</kwd><kwd>палеовулкан</kwd></kwd-group><kwd-group xml:lang="en"><kwd>groundwater</kwd><kwd>mineral composition</kwd><kwd>seasonal variations</kwd><kwd>paleovolcano</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">Baillie C-K., Kaufholdt, D., Meinen R., Hu B., Rennenberg H., Hänsch R., Bloem E. Surviving Volcanic Environments-Interaction of Soil Mineral Content and Plant Element Composition // Front. Environ. 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