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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">esoil</journal-id><journal-title-group><journal-title xml:lang="ru">Бюллетень Почвенного института имени В.В. Докучаева</journal-title><trans-title-group xml:lang="en"><trans-title>Dokuchaev Soil Bulletin</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0136-1694</issn><issn pub-type="epub">2312-4202</issn><publisher><publisher-name>V.V. Dokuchaev Soil Science Institute</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.19047/0136-1694-2019-97-52-90</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-341</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></article-categories><title-group><article-title>КОМБИНАЦИЯ ЗАСОЛЕННЫХ ПОЧВ СЕВЕРНОГО СКЛОНА ВОЗВЫШЕННОСТИ ЕРГЕНИ ПОСЛЕ ПРЕКРАЩЕНИЯ ОРОШЕНИЯ</article-title><trans-title-group xml:lang="en"><trans-title>COMBINATION OF SALINE SOILS OF THE NORTHERN SLOPE OF THE ERGENI UPLAND AFTER IRRIGATION CESSATION</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5151-5109</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Хитров</surname><given-names>Н. Б.</given-names></name><name name-style="western" xml:lang="en"><surname>Khitrov</surname><given-names>N. B.</given-names></name></name-alternatives><bio xml:lang="ru"><p>зав. отделом генезиса и мелиорации засоленных и солонцовых почв</p><p>119017, Москва, Пыжевский пер, 7, стр. 2.</p></bio><bio xml:lang="en"><p>119017, Moscow, Pizhevskiy per., 7, build. 2.</p></bio><email xlink:type="simple">khitrovnb@gmail.com</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>Горохова</surname><given-names>И. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Gorokhova</surname><given-names>I. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>с.н.с. отдела генезиса и мелиорации засоленнйх и солонцовых почв</p><p>119017, Москва, Пыжевский пер, 7, стр. 2.</p></bio><bio xml:lang="en"><p>119017, Moscow, Pizhevskiy per., 7, build. 2.</p></bio><email xlink:type="simple">g-irina14@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>Кравченко</surname><given-names>Е. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Kravchenko</surname><given-names>E. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>инженер отдела генезиса и мелиорации засоленных и солонцовых почв</p><p>119017, Москва, Пыжевский пер, 7, стр. 2.</p></bio><bio xml:lang="en"><p>119017, Moscow, Pizhevskiy per., 7, build. 2.</p></bio><email xlink:type="simple">krav4enko_elena@mail.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru">Почвенный институт им. В.В. Докучаева<country>Россия</country></aff><aff xml:lang="en">V.V. Dokuchaev Soil Science Institute<country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>18</day><month>06</month><year>2019</year></pub-date><volume>0</volume><issue>97</issue><fpage>52</fpage><lpage>90</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Хитров Н.Б., Горохова И.Н., Кравченко Е.И., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Хитров Н.Б., Горохова И.Н., Кравченко Е.И.</copyright-holder><copyright-holder xml:lang="en">Khitrov N.B., Gorokhova I.N., Kravchenko E.I.</copyright-holder><license 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://bulletin.esoil.ru/jour/article/view/341">https://bulletin.esoil.ru/jour/article/view/341</self-uri><abstract><p>Исследован почвенный покров и засоленность почв на поле с чередующимися более темными и более светлыми широкими полосами, заметными на космическом снимке, в пределах орошаемого участка Червленое Светлоярской оросительной системы (юг Волгоградской обл.). Поле орошалось до середины 1990-х годов и было подвержено вторичному засолению, с тех пор используется в богаре. Почвенная комбинация представляет собой бывший степной светло-каштановый солонцовый комплекс, преобразованный в ходе планировки поверхности и орошения в агроземы аккумулятивно-карбонатные сегрегационные солончаковатые (Sodic Endoprotosalic Cambisol (Loamic, Aric, Protocalcic, Ochric, Bathygypsic) and Cambic Calcisols (Loamic, Aric)) и глубокосолончаковатые, и агросветлогумусовую аккумулятивно-карбонатную стратифицированную почву. Светлые полосы на поле маркируют сильнокарбонатные (12–13 % CaCO3) с поверхности почвы (Calcaric Cambisol (Loamic, Aric)) среди других почв, имеющих с поверхности в 5–10 раз меньше карбонатов. Все почвы засоленные, но содержание солей меняется в пространстве волнообразно несогласно с изображением на снимке. Обсуждаются двумерные распределения содержания карбонатов и солей в почвенной комбинации. Отмечается наличие остаточных признаков вторичного засоления в виде хлоридов кальция и магния через два десятилетия после прекращения орошения и снижения уровня грунтовых вод глубже 7 м.</p></abstract><trans-abstract xml:lang="en"><p>The soil cover and soil salinity of the field were studied and the results are given in the article, the explored fileld is located within the Chervlenoye irrigated area belonging to Svetloyarskaya irrigation system (south of the Volgograd region). It was characterized by alternating dark and light wide strips visible on the satellite image. The field was irrigated until the mid-1990s and was subject to secondary salinization, since that time it has been used in dry-farming system. The soil combination is performed by steppe light chestnut solonetzic complex that was transformed due to the surface leveling and irrigation into agrozem accumulative-carbonate segregation saline (Sodic Endoprotosalic Cambisol (Loamic, Aric, Protocalcic, Ochric, Bathygypsic) and Cambic Calcisols (Loamic, Aric)) and deep saline, and agro-light-humus accumulative-carbonate stratified soil. The bright bands on the field mark soils rich in carbonates on the surface (12–13 % CaCO3) (Calcaric Cambisol (Loamic, Aric)) among the other soils that contain less carbonates on the surface by 5–10 times. All the soils are saline, but the salt content varies in space in a wave-like manner, wich disagrees with the satellite image. Two-dimensional distributions of carbonates and salts in the soil combination are discussed. The residual signs of secondary salinization are revealed in the form of calcium and magnesium chlorides two decades after the cessation of irrigation and drawdown of the groundwater curve deeper than 7 m.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>карбонаты</kwd><kwd>засоленные почвы</kwd><kwd>водная вытяжка</kwd><kwd>ионоселективные электроды</kwd><kwd>активности ионов</kwd></kwd-group><kwd-group xml:lang="en"><kwd>carbonates</kwd><kwd>saline soils</kwd><kwd>water extraction</kwd><kwd>ion-selective electrodes</kwd><kwd>ions activity</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">Барановская В.А, Азовцев В.И. Влияние орошения на миграцию карбонатов в почвах Поволжья // Почвоведение. 1981. № 10. 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