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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-3048</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>Article</subject></subj-group></article-categories><title-group><article-title>Овражная эрозия на пахотных землях Европы</article-title><trans-title-group xml:lang="en"><trans-title>Gully erosion on arable lands in Europe</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>Дедков</surname><given-names>А. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Dedkov</surname><given-names>A. P.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Рысин</surname><given-names>И. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Rysin</surname><given-names>I. I.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Чернышева</surname><given-names>Т. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Chernysheva T</surname><given-names>T. N.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Казанский университет</institution><country>Россия</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Удмуртский университет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1993</year></pub-date><pub-date pub-type="epub"><day>02</day><month>02</month><year>2023</year></pub-date><volume>0</volume><issue>2</issue><issue-title>Геоморфология</issue-title><fpage>3</fpage><lpage>13</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Дедков А.П., Рысин И.И., Чернышева Т.Н., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Дедков А.П., Рысин И.И., Чернышева Т.Н.</copyright-holder><copyright-holder xml:lang="en">Dedkov A.P., Rysin I.I., Chernysheva T T.N.</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/3048">https://geomorphology.igras.ru/jour/article/view/3048</self-uri><abstract><p>Three large regions of active gully erosion are known in Europe, those are south-eastern, central and southern ones. The main controlling factors are high degree of the land cultivation, a considerable runoff unevenly distributed, and high erodibility of loess and clayey rocks in the regions. Erosion first appears on arable lands, though many cultivated elevations in various parts of Europe lack gullies. That is mostly due to the fact that length and steepness of slopes there are insufficient for linear erosion to initiate. The gully erosion shows zonal pattern which depends on zonal features of drainage density, runoff irregularities and loess distribution.</p></abstract><trans-abstract xml:lang="en"><p>Three large regions of active gully erosion are known in Europe, those are south-eastern, central and southern ones. The main controlling factors are high degree of the land cultivation, a considerable runoff unevenly distributed, and high erodibility of loess and clayey rocks in the regions. Erosion first appears on arable lands, though many cultivated elevations in various parts of Europe lack gullies. That is mostly due to the fact that length and steepness of slopes there are insufficient for linear erosion to initiate. The gully erosion shows zonal pattern which depends on zonal features of drainage density, runoff irregularities and loess distribution.</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>
