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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">geomorf</journal-id><journal-title-group><journal-title xml:lang="ru">Геоморфология и палеогеография</journal-title><trans-title-group xml:lang="en"><trans-title>Geomorfologiya i Paleogeografiya</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">2949-1789</issn><issn pub-type="epub">2949-1797</issn><publisher><publisher-name></publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">geomorf-1654</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>Геоморфология и народное хозяйство</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Geomorphology and economy</subject></subj-group></article-categories><title-group><article-title>Геоморфологические условия процесса подтопления на территории г. Волгограда</article-title><trans-title-group xml:lang="en"><trans-title>Geomorphic conditions of waterlogging process in the city of Volgograd</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>Севостьянов</surname><given-names>В. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Sevostyanov</surname><given-names>V. V.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>ВолгоградНИПИнефть</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>1990</year></pub-date><pub-date pub-type="epub"><day>16</day><month>05</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>40</fpage><lpage>44</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Севостьянов В.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Севостьянов В.В.</copyright-holder><copyright-holder xml:lang="en">Sevostyanov V.V.</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://geomorphology.igras.ru/jour/article/view/1654">https://geomorphology.igras.ru/jour/article/view/1654</self-uri><abstract><p>The significance of topography in the waterlogging process is analysed with reference to the Volgograd territory at the right bank of the Volga. Special features of the water logging process are described which result from natural and artificial factors and also from their joint impact. Certain clusters of waterlogged sites are outlined.</p></abstract><trans-abstract xml:lang="en"><p>The significance of topography in the waterlogging process is analysed with reference to the Volgograd territory at the right bank of the Volga. Special features of the water logging process are described which result from natural and artificial factors and also from their joint impact. Certain clusters of waterlogged sites are outlined.</p></trans-abstract></article-meta></front><back><ref-list><title>References</title></ref-list><fn-group><fn fn-type="conflict"><p>The authors declare that there are no conflicts of interest present.</p></fn></fn-group></back></article>
