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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-2242</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>Методика научных исследований</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>Scientific Research Methods</subject></subj-group></article-categories><title-group><article-title>Метод расчета интенсивности поверхностного смыва с пахотных склонов в ЦЧО</article-title><trans-title-group xml:lang="en"><trans-title>Technique of surface wash intensity calculation for arable slopes in the Central Chernozem Region</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>Иванов</surname><given-names>В. Д.</given-names></name><name name-style="western" xml:lang="en"><surname>Ivanov</surname><given-names>V. D.</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>Воронежский сельскохозяйственный институт</institution><country>Россия</country></aff></aff-alternatives><pub-date pub-type="collection"><year>1980</year></pub-date><pub-date pub-type="epub"><day>07</day><month>09</month><year>2022</year></pub-date><volume>0</volume><issue>4</issue><issue-title>Геоморфология</issue-title><fpage>61</fpage><lpage>66</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Иванов В.Д., 2022</copyright-statement><copyright-year>2022</copyright-year><copyright-holder xml:lang="ru">Иванов В.Д.</copyright-holder><copyright-holder xml:lang="en">Ivanov V.D.</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/2242">https://geomorphology.igras.ru/jour/article/view/2242</self-uri><abstract><p>Приводится формула расчета интенсивности современного смыва почв со склонов за время весеннего половодья, представляющая собой произведение показателя удельного смыва почв, работы воды, стекающей по склону, и ряда коэффициентов, учитывающих Форму и экспозицию склона, механический состав, эрудированность, карбонат ость и солонцеватость почв, агрофон и выращиваемые культуры, защищенность почв от эрозии. По изменению мощности гумусового горизонта за известный период времени и по формуле определена интенсивность современной денудации на пахотных склонах ЦЧО в бассейне р. Дон, которая на восточном склоне Среднерусской возвышенности колеблется в пределах от 0,71 до 1,48 мм/год.</p></abstract><trans-abstract xml:lang="en"><p>A possibility is shown to define the intensity of presentday erosion processes on arable slopes by means of measurements of changes of humic horizon thickness during a certain time span; it is also possible to use a formula which is the product of specific soil wash and work of water flowing downslope. The formula includes also coefficients considering slope form and exposition, soil mecanical composition and degree of erosion, degree and type of soil salinization and soil protection against erosion. Present day erosion intensity is defined at arable slopes of the Central Chernozem Region, the value at the Middle Russian Upland appeared to be between 0,71 and 1,48 millimeters per year.</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>
