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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">soil</journal-id><journal-title-group><journal-title xml:lang="ru">Почвоведение и агрохимия</journal-title><trans-title-group xml:lang="en"><trans-title>Soil Science and Agrochemistry</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0130-8475</issn><publisher><publisher-name>Институт почвоведения и агрохимии</publisher-name></publisher></journal-meta><article-meta><article-id custom-type="elpub" pub-id-type="custom">soil-273</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>1. ПОЧВЕННЫЕ РЕСУРСЫ И ИХ РАЦИОНАЛЬНОЕ ИСПОЛЬЗОВАНИЕ</subject></subj-group><subj-group subj-group-type="section-heading" xml:lang="en"><subject>1. SOIL RESOURCES AND THEIR RATIONAL USE</subject></subj-group></article-categories><title-group><article-title>КОЭФФИЦИЕНТЫ УСТОЙЧИВОСТИ ПОЧВ БЕЛАРУСИ К ВОДНОЙ ЭРОЗИИ</article-title><trans-title-group xml:lang="en"><trans-title>COEFFICIENTS OF RESISTANCE OF SOD-PODZOLIC  SOILS OF BELARUS TO EROSION</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>Афанасьев</surname><given-names>Н. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Afanas’Ev</surname><given-names>N. I.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Юхновец</surname><given-names>Ан. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Yuhnovets</surname><given-names>AN. V.</given-names></name></name-alternatives><email xlink:type="simple">noemail@neicon.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff xml:lang="ru" id="aff-1"><institution>Институт почвоведения и агрохимии, г. Минск, Беларусь</institution><country>Russian Federation</country></aff><pub-date pub-type="collection"><year>2010</year></pub-date><pub-date pub-type="epub"><day>30</day><month>12</month><year>2010</year></pub-date><volume>0</volume><issue>2</issue><fpage>49</fpage><lpage>54</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Афанасьев Н.И., Юхновец А.В., 2010</copyright-statement><copyright-year>2010</copyright-year><copyright-holder xml:lang="ru">Афанасьев Н.И., Юхновец А.В.</copyright-holder><copyright-holder xml:lang="en">Afanas’Ev N.I., Yuhnovets A.V.</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://soil.belal.by/jour/article/view/273">https://soil.belal.by/jour/article/view/273</self-uri><abstract><p>Расчетным способом определены коэффициенты эрозионной устойчивости для 10 почв Беларуси. Для этой цели использованы данные гранулометрического и валового химического состава. Коэффициенты по гранулометрическому составу изменялись 0,5 до 5,8, а по соотношению полуторных оксидов от 6,4 до 19,0. Устойчивость почв к эрозии определяется величиной коэффициента, который зависит от содержания песка. Табл. 2. Библиогр. 8.</p></abstract><trans-abstract xml:lang="en"><p>Coefficients of erodibility of sod-podzolic soils of Belarus to erosion were determined by two methods: relation in soils sand to summary of silt and clay; SiO2:R2O3. Fluctuation of these coefficients was from 0,5 to 5,8 and 6,4 to 19, accordingly. Both methods can use for orientation evaluate of erosion stability of soils. 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