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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-1827</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>Изучение процесса формирования береговой зоны водохранилищ на модели</article-title><trans-title-group xml:lang="en"><trans-title>Studies of formation of reservoir shore zone using experimental model</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>Виноградова</surname><given-names>Н. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Vinogradova</surname><given-names>N. N.</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>Самойлова</surname><given-names>А. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Samoilova</surname><given-names>A. A.</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>1977</year></pub-date><pub-date pub-type="epub"><day>06</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>55</fpage><lpage>60</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Виноградова Н.Н., Самойлова А.А., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Виноградова Н.Н., Самойлова А.А.</copyright-holder><copyright-holder xml:lang="en">Vinogradova N.N., Samoilova A.A.</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/1827">https://geomorphology.igras.ru/jour/article/view/1827</self-uri><abstract><p>Some data are given on special features of reservoir coast development obtained by laboratory experiments. The technique allows to study stages of the coast development which are difficult to trace at the natural basins. Some data have been obtained on dimensions of shore platform under a certain wave regime. Volumes and mean rates of erosion and accumulation have been estimated.</p></abstract><trans-abstract xml:lang="en"><p>Some data are given on special features of reservoir coast development obtained by laboratory experiments. The technique allows to study stages of the coast development which are difficult to trace at the natural basins. Some data have been obtained on dimensions of shore platform under a certain wave regime. Volumes and mean rates of erosion and accumulation have been estimated.</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>
