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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-3358</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>Дискуссии</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Discussions</subject></subj-group></article-categories><title-group><article-title>О цикличности эрозионно-аккумулятивных процессов в сельскохозяйственной зоне Русской равнины</article-title><trans-title-group xml:lang="en"><trans-title>On the cyclicity of erosion and sedimentation processes in the agricultural zone of the Russian Plain</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>Голосов</surname><given-names>В. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Golosov</surname><given-names>V. N.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Московский государственный университет имени М.В. Ломоносова, географический факультет</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1996</year></pub-date><pub-date pub-type="epub"><day>26</day><month>10</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>43</fpage><lpage>51</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Голосов В.Н., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Голосов В.Н.</copyright-holder><copyright-holder xml:lang="en">Golosov V.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/3358">https://geomorphology.igras.ru/jour/article/view/3358</self-uri><abstract><p>A recent trend in the erosion-accumulation processes is analysed using various approaches, such as quantitative analysis of spatial-temporal variations in the main factors of erosion; natural stationary observations of the soil erosion on slopes, some indirect methods of estimation of erosion and sedimentation rates. The best results might be obtained using all the methods simultaneously. Most promising seems to be estimation of the processes rate based on radioisotopes. A few examples are given of the erosion and sedimentation trends throughout the last 100 to 150 years in different natural zones of the Russian Plain.</p></abstract><trans-abstract xml:lang="en"><p>A recent trend in the erosion-accumulation processes is analysed using various approaches, such as quantitative analysis of spatial-temporal variations in the main factors of erosion; natural stationary observations of the soil erosion on slopes, some indirect methods of estimation of erosion and sedimentation rates. The best results might be obtained using all the methods simultaneously. Most promising seems to be estimation of the processes rate based on radioisotopes. A few examples are given of the erosion and sedimentation trends throughout the last 100 to 150 years in different natural zones of the Russian Plain.</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>
