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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-3078</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>Научные сообщения</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Short communications</subject></subj-group></article-categories><title-group><article-title>Динамика современных процессов сноса и аккумуляции на Курском опытном полигоне</article-title><trans-title-group xml:lang="en"><trans-title>Dynamics of the present-day processes of erosion and sedimentation on the Kursk experimental site</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>Фирсенкова</surname><given-names>В. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Firsenkova</surname><given-names>V. M.</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>Институт экологии РАН, г. Тольятти</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1993</year></pub-date><pub-date pub-type="epub"><day>03</day><month>02</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>99</fpage><lpage>106</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Фирсенкова В.М., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Фирсенкова В.М.</copyright-holder><copyright-holder xml:lang="en">Firsenkova V.M.</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/3078">https://geomorphology.igras.ru/jour/article/view/3078</self-uri><abstract><p>The paper summarizes long-term measurements of slope and gully erosion and sedimentation within elementary catchments in the Kursk region. Soil erosion and sedimentation dynamics on slopes and bottoms of elementary rills is traced on daily, seasonal, and yearly basis. The processes appeared to relate to spatial differentiation of the catchment surface, its morphology in the first place. Quantitative data are given on the erosion and sedimentation dynamics in the gully and on its elements. The gully growth and its elements development is concluded to be of cyclic character.</p></abstract><trans-abstract xml:lang="en"><p>The paper summarizes long-term measurements of slope and gully erosion and sedimentation within elementary catchments in the Kursk region. Soil erosion and sedimentation dynamics on slopes and bottoms of elementary rills is traced on daily, seasonal, and yearly basis. The processes appeared to relate to spatial differentiation of the catchment surface, its morphology in the first place. Quantitative data are given on the erosion and sedimentation dynamics in the gully and on its elements. The gully growth and its elements development is concluded to be of cyclic character.</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>
