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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-3577</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>Статьи</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Article</subject></subj-group></article-categories><title-group><article-title>Соотношение транспортирующей способности потока и стока наносов как условие формирования русел рек разных типов</article-title><trans-title-group xml:lang="en"><trans-title>Relation of carrying capacity of river and sediment load as the main factor of different types river channels formation</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>Кондратьев</surname><given-names>А. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Kondratyev</surname><given-names>A. N.</given-names></name></name-alternatives><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Государственный гидрологический институт</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>1999</year></pub-date><pub-date pub-type="epub"><day>15</day><month>01</month><year>2024</year></pub-date><volume>0</volume><issue>3</issue><fpage>14</fpage><lpage>18</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Кондратьев А.Н., 2024</copyright-statement><copyright-year>2024</copyright-year><copyright-holder xml:lang="ru">Кондратьев А.Н.</copyright-holder><copyright-holder xml:lang="en">Kondratyev A.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/3577">https://geomorphology.igras.ru/jour/article/view/3577</self-uri><abstract><p>Multichanneled river bed appears when sediment load from the upper basin exceeds carrying capacity of the river in the site. Meanders appear on the converse condition. If the sediment load equals carrying capacity in the straight channel the latter continues straight (bandy-ridged).</p></abstract><trans-abstract xml:lang="en"><p>Multichanneled river bed appears when sediment load from the upper basin exceeds carrying capacity of the river in the site. Meanders appear on the converse condition. If the sediment load equals carrying capacity in the straight channel the latter continues straight (bandy-ridged).</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>
