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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-1955</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>Связь типов русел с формами речных долин</article-title><trans-title-group xml:lang="en"><trans-title>Valley form control of river channel type</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>Снищенко</surname><given-names>Б. Ф.</given-names></name><name name-style="western" xml:lang="en"><surname>Snishchenko</surname><given-names>B. F.</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>Государственный гидрологический институт</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1979</year></pub-date><pub-date pub-type="epub"><day>19</day><month>06</month><year>2022</year></pub-date><volume>0</volume><issue>1</issue><issue-title>Геоморфология</issue-title><fpage>18</fpage><lpage>25</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Снищенко Б.Ф., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Снищенко Б.Ф.</copyright-holder><copyright-holder xml:lang="en">Snishchenko B.F.</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/1955">https://geomorphology.igras.ru/jour/article/view/1955</self-uri><abstract><p>На обширном материале исследований в натуре установлено, что необходимые условия перехода свободно меандрируюших русел к прямолинейным состоят в совместном уменьшении относительной ширины дна долины и увеличении меры использования потоком уклона долины. Приведены критериальные характеристики типов русла, которые могут применяться при прогнозировании типов русловых форм в зарегулированных реках и созданных искусственным путем.</p></abstract><trans-abstract xml:lang="en"><p>A great deal of nature studies reveal necessary conditions of transition of free meandering river channels into linear ones, the conditions are combined decrease in relative valley floor width and increase in degree of valley slope utilisation by the stream. Some criteria of channel type characteristics are given which may be applied to forecasting of channel forms developing in regulated rivers and artificial streams.</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>
