<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Journal Publishing DTD v1.3 20210610//EN" "JATS-journalpublishing1-3.dtd">
<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-3144</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>Морфология русел рек равнинной части Алтайского края</article-title><trans-title-group xml:lang="en"><trans-title>Channel morphology of plain rivers of the Altai Territory</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>Павлов</surname><given-names>И. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Pavlov</surname><given-names>L. N.</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>1994</year></pub-date><pub-date pub-type="epub"><day>02</day><month>03</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><fpage>78</fpage><lpage>85</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Павлов И.Н., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Павлов И.Н.</copyright-holder><copyright-holder xml:lang="en">Pavlov l.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/3144">https://geomorphology.igras.ru/jour/article/view/3144</self-uri><abstract><p>To study channel morphology of freely meandering rivers on the plains of the Altai Territory a modified technique has been applied, which involved determination of prevailing radii of meander curvature within hydrologically uniform segments of channel. It appeared that the prevailing radius values change systematically along the river and depend on regional conditions, primarily on the river discharge and drainage basin configuration. Those conditions influence also relationship between meander parameters.</p></abstract><trans-abstract xml:lang="en"><p>To study channel morphology of freely meandering rivers on the plains of the Altai Territory a modified technique has been applied, which involved determination of prevailing radii of meander curvature within hydrologically uniform segments of channel. It appeared that the prevailing radius values change systematically along the river and depend on regional conditions, primarily on the river discharge and drainage basin configuration. Those conditions influence also relationship between meander parameters.</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>
