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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">litosphere</journal-id><journal-title-group><journal-title xml:lang="ru">Литосфера</journal-title><trans-title-group xml:lang="en"><trans-title>LITHOSPHERE (Russia)</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">1681-9004</issn><issn pub-type="epub">2500-302X</issn><publisher><publisher-name>A.N. Zavaritsky Institute of Geology and Geochemistry</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.24930/1681-9004-2018-18-6-928-941</article-id><article-id custom-type="elpub" pub-id-type="custom">litosphere-262</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Articles</subject></subj-group></article-categories><title-group><article-title>Элементный состав грунтовых вод и спелеотемы “лунное молокоˮ в карстовой пещере Прощальная (Дальний Восток)</article-title><trans-title-group xml:lang="en"><trans-title>Element composition of ground water and speleothem “moon milkˮ in a karst cave Proshchal’naya (Far East)</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>Кондратьева</surname><given-names>Л. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Kondratyeva</surname><given-names>Lubov’ M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>г. Хабаровск, ул. Ким Ю Чена, 65, 680000</p></bio><bio xml:lang="en"><p>65 Kim-Yu-Chen st., Khabarovsk 680000</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Полевская</surname><given-names>О. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Polevskaya</surname><given-names>Oksana S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>г. Хабаровск, ул. Ким Ю Чена, 65, 680000</p></bio><bio xml:lang="en"><p>65 Kim-Yu-Chen st., Khabarovsk 680000</p></bio><email xlink:type="simple">oksasha.polevskaya@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>Голубева</surname><given-names>Е. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Golubeva</surname><given-names>Evgeniya M.</given-names></name></name-alternatives><bio xml:lang="ru"><p>г. Хабаровск, ул. Ким Ю Чена, 65, 680000</p></bio><bio xml:lang="en"><p>65 Kim-Yu-Chen st., Khabarovsk 680000</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Штарева</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Shtareva</surname><given-names>Anna V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>г. Хабаровск, ул. Ким Ю Чена, 65, 680000</p></bio><bio xml:lang="en"><p>65 Kim-Yu-Chen st., Khabarovsk 680000</p></bio><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Коновалова</surname><given-names>Н. С.</given-names></name><name name-style="western" xml:lang="en"><surname>Konovalova</surname><given-names>Natal’ya S.</given-names></name></name-alternatives><bio xml:lang="ru"><p>г. Хабаровск, ул. Ким Ю Чена, 65, 680000</p></bio><bio xml:lang="en"><p>65 Kim-Yu-Chen st., Khabarovsk 680000</p></bio><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Институт водных и экологических проблем ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Institute of water and ecological problems, Far East Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Институт тектоники и геофизики им. Ю.А. Косыгина ДВО РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Yu.A.. Kosygin Institute of tectonics and geophysics, Far East Branch of RAS</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2018</year></pub-date><pub-date pub-type="epub"><day>28</day><month>12</month><year>2018</year></pub-date><volume>0</volume><issue>6</issue><fpage>928</fpage><lpage>941</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Кондратьева Л.М., Полевская О.С., Голубева Е.М., Штарева А.В., Коновалова Н.С., 2018</copyright-statement><copyright-year>2018</copyright-year><copyright-holder xml:lang="ru">Кондратьева Л.М., Полевская О.С., Голубева Е.М., Штарева А.В., Коновалова Н.С.</copyright-holder><copyright-holder xml:lang="en">Kondratyeva L.M., Polevskaya O.S., Golubeva E.M., Shtareva A.V., Konovalova N.S.</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.lithosphere.ru/jour/article/view/262">https://www.lithosphere.ru/jour/article/view/262</self-uri><abstract><p>Объект исследования. Целью работы являлся сравнительный анализ элементного состава грунтовых вод (капельной, трещинной), воды из внутреннего водотока, в карстовой пещере Прощальная (Хабаровский край) и поверхностных вод ближайшей реки Сагды-Селанка. Большой интерес представляло исследование спелиотемы (натечного образования) “лунное молоко” (moonmilk) в пещере Прощальная. Материалы и методы. Натечное образование “лунное молоко” исследовалось с помощью сканирующей электронной микроскопии (EVO-40HV, CarlZeiss, Германия) и кремний-дрейфового рентгеновского детектора X-MAX 80 мм2 . Методом ICP-MS проведен сравнительный анализ элементного состава грунтовых вод (капельной, трещинной), воды из внутреннего водотока в пещере Прощальная и поверхностных вод р. Сагды-Селанка. Результаты. Максимальные концентрации кальция, железа и марганца были установлены в весенний период в капельной воде, а магния – в проточных водах (внутренний водоток пещеры и р. Сагды-Селанка). Определено, что визуально пластичная и гомогенная масса спелеотемы “лунное молоко” гетерогенна и содержит различные микроструктуры. Трубчатые микроструктуры представлены более богатым элементным составом (C, O, Ca, Fe, Mn, Si, Al и S) по сравнению с булавовидными образованиями (C, O, Ca и Na). Связующей матрицей в составе “лунного молока” были сетчатые структуры, подобные мицелию актиномицетов и бактериальным пленкам. Выводы. Результаты проведенных исследований в условиях муссонного климата могут быть интересны при изучении карстовых процессов в других климатических зонах.</p></abstract><trans-abstract xml:lang="en"><p>Object of research. The aim of this work was the comparative analysis of element composition of groundwater (drip, fracture), water from the interior of the watercourse in a karst cave Proshchal’naya (Khabarovsk Territory) and the surface water of the nearest river Sagdy-Selanka. The great interest was the study of speleothem (dropstones) “moon milk” in the cave Proshchal’naya. Materials and methods. Speleothem “moon milk” was investigated with a scanning electron microscope (EVO-40HV, CarlZeiss, Germany) and silicon-drift x-ray detector X-MAX 80 мм2 . By ICP-MS method a comparative analysis of element composition of groundwater (drip, fracture), water from an internal stream in the cave Proshchal’naya and surface water of the river Sagdy-Selenka were carried out. Results. Maximum concentrations of calcium, iron and manganese was installed in the spring, between drip and fracture water and magnesium – in flowing waters (inland watercourse caves and Sagdy-Selanka R.). It was determined that visually plastic and homogeneous mass of speleothem “moon milk” is heterogeneous and contains various microstructures. Tubular microstructures were represented by richer elemental compo sition (C, O, Ca, Fe, Mn, Si, Al, and S) compared with club-shaped formations (C, O, Ca, and Na). The binding matrix in the composition of the “moon milk” were reticular structures similar to actinomycente mycelium and bacterial films. Findings. The results of studies conducted in a monsoon climate may be interesting for researchers which study karst processes in other climatic zones.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>карст</kwd><kwd>капельная вода</kwd><kwd>трещинная вода</kwd><kwd>натечное образование “лунное молоко”</kwd></kwd-group><kwd-group xml:lang="en"><kwd>karst</kwd><kwd>drip water</kwd><kwd>water of fracturing</kwd><kwd>dropstones</kwd><kwd>“moonmilk”</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">Абдрахманов Р.Ф., Попов В.Г. 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