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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-2992</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>Дифференциация гидрологических процессов и смыва почвы в пределах городских территорий (на примере г. Курска)</article-title><trans-title-group xml:lang="en"><trans-title>Hydrological processes and soil loss differentiation within the limits of urban territories (a case study of Kursk)</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>Китаев</surname><given-names>Л. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Kitaev</surname><given-names>L. M.</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>Институт географии РАН</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1992</year></pub-date><pub-date pub-type="epub"><day>21</day><month>01</month><year>2023</year></pub-date><volume>0</volume><issue>3</issue><issue-title>Геоморфология</issue-title><fpage>63</fpage><lpage>70</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Китаев Л.М., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Китаев Л.М.</copyright-holder><copyright-holder xml:lang="en">Kitaev L.M.</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/2992">https://geomorphology.igras.ru/jour/article/view/2992</self-uri><abstract><p>Urban areas are subdivided into regions on the basis of spatial differentiation of hydrological processes and associated soil loss. The primary material for the quantitative (including statistic) analysis of the processes comes from experimental studies Io the city of Kursk. Principles of regionalisation and quantitative characteristics of runoff and soil loss within the regions permit physical model ling and forecast of runoff and erosion quantities within urban territories.</p></abstract><trans-abstract xml:lang="en"><p>Urban areas are subdivided into regions on the basis of spatial differentiation of hydrological processes and associated soil loss. The primary material for the quantitative (including statistic) analysis of the processes comes from experimental studies Io the city of Kursk. Principles of regionalisation and quantitative characteristics of runoff and soil loss within the regions permit physical model ling and forecast of runoff and erosion quantities within urban territories.</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>
