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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-3403</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>Эрозионно-аккумулятивные процессы на поймах равнинных рек (на примере бассейна Дона)</article-title><trans-title-group xml:lang="en"><trans-title>Riverine forests and processes of erosion and alluviation</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>Шаталов</surname><given-names>В. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Shatalov</surname><given-names>V. G.</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>Воронежская лесотехническая академия</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1997</year></pub-date><pub-date pub-type="epub"><day>24</day><month>11</month><year>2023</year></pub-date><volume>0</volume><issue>1</issue><fpage>87</fpage><lpage>90</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Шаталов В.Г., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Шаталов В.Г.</copyright-holder><copyright-holder xml:lang="en">Shatalov V.G.</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/3403">https://geomorphology.igras.ru/jour/article/view/3403</self-uri><abstract><p>Forests growing on the plain rivers floodplains deeply influence erosion and sedimentation. They control erosion and protect the banks. The riverine forests impact on the erosion and alluviation processes is discussed with reference to various types of banks: concave, eroded, convex bulit-up, and rectilinear ones. The paper discusses different tree species, as well as differences in the age and density of growth. Consideration of all those data would permit to choose right species, as well as correct system of planting, and thus to regulate and control erosion and alluviation in each individual case.</p></abstract><trans-abstract xml:lang="en"><p>Forests growing on the plain rivers floodplains deeply influence erosion and sedimentation. They control erosion and protect the banks. The riverine forests impact on the erosion and alluviation processes is discussed with reference to various types of banks: concave, eroded, convex bulit-up, and rectilinear ones. The paper discusses different tree species, as well as differences in the age and density of growth. Consideration of all those data would permit to choose right species, as well as correct system of planting, and thus to regulate and control erosion and alluviation in each individual case.</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>
