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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-2858</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>О роли капельно-дождевой эрозии в процессах денудации рельефа</article-title><trans-title-group xml:lang="en"><trans-title>On the splash erosion importance in the denudation process</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>Бредихин</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Bredikhin</surname><given-names>A. V.</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>1989</year></pub-date><pub-date pub-type="epub"><day>13</day><month>12</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>51</fpage><lpage>59</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Бредихин А.В., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Бредихин А.В.</copyright-holder><copyright-holder xml:lang="en">Bredikhin A.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/2858">https://geomorphology.igras.ru/jour/article/view/2858</self-uri><abstract><p>The raindrop impact is one of less studied exogenous processes. All the related phenomena are known by the term «xsplash erosion». Two processes can be distinguished: splash of soil particles and creep induced by raindrops impact. Some factors are discussed which control the splash erosion (rainfall regime, vegetation and burrowing animals, slope of surface and soil characteristics: particles size, moisture content etc.). Data on splash erosion rate are given. The process should be considered as an individual type of denudation of the Earth surface which combines features of both slope and erosional process.</p></abstract><trans-abstract xml:lang="en"><p>The raindrop impact is one of less studied exogenous processes. All the related phenomena are known by the term «xsplash erosion». Two processes can be distinguished: splash of soil particles and creep induced by raindrops impact. Some factors are discussed which control the splash erosion (rainfall regime, vegetation and burrowing animals, slope of surface and soil characteristics: particles size, moisture content etc.). Data on splash erosion rate are given. The process should be considered as an individual type of denudation of the Earth surface which combines features of both slope and erosional process.</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>
