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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">esoil</journal-id><journal-title-group><journal-title xml:lang="ru">Бюллетень Почвенного института имени В.В. Докучаева</journal-title><trans-title-group xml:lang="en"><trans-title>Dokuchaev Soil Bulletin</trans-title></trans-title-group></journal-title-group><issn pub-type="ppub">0136-1694</issn><issn pub-type="epub">2312-4202</issn><publisher><publisher-name>V.V. Dokuchaev Soil Science Institute</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="doi">10.19047/0136-1694-2020-104-158-198</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-621</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></article-categories><title-group><article-title>Цифровое картографирование степени эродированности почв с использованием моделей фактор - свойство и фактор - процесс - свойство (юг Среднерусской возвышенности)</article-title><trans-title-group xml:lang="en"><trans-title>Digital mapping of erosion degree of soils using the factor - property and factor - process - property models (the south of the Central Russian upland)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-5256-4348</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Смирнова</surname><given-names>М. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Smirnova</surname><given-names>M. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119017, Москва, Пыжевский пер, 7, стр. 2; 119991, Москва, Ленинские горы, 1</p></bio><bio xml:lang="en"><p>7 Bld. 2 Pyzhevskiy per., Moscow 119017; Leninskie Gori, Moscow 119234</p></bio><email xlink:type="simple">summerija@yandex.ru</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-3995-9203</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Жидкин</surname><given-names>А. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Zhidkin</surname><given-names>A. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119017, Москва, Пыжевский пер, 7, стр. 2</p></bio><bio xml:lang="en"><p>7 Bld. 2 Pyzhevskiy per., Moscow 119017</p></bio><email xlink:type="simple">gidkin@mail.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-0377-3124</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Лозбенев</surname><given-names>Н. И.</given-names></name><name name-style="western" xml:lang="en"><surname>Lozbenev</surname><given-names>N. I.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119017, Москва, Пыжевский пер, 7, стр. 2</p></bio><bio xml:lang="en"><p>7 Bld. 2 Pyzhevskiy per., Moscow 119017</p></bio><email xlink:type="simple">nikolay.lozbenev@yandex.ru</email><xref ref-type="aff" rid="aff-2"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Заздравных</surname><given-names>Е. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Zazdravnykh</surname><given-names>E. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>308027, Белгород, ул. Щорса, д. 8</p></bio><bio xml:lang="en"><p>8 Shchorsa Str., Belgorod 308027</p></bio><email xlink:type="simple">genn-86@yandex.ru</email><xref ref-type="aff" rid="aff-3"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-0103-0300</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Козлов</surname><given-names>Д. Н.</given-names></name><name name-style="western" xml:lang="en"><surname>Kozlov</surname><given-names>D. N.</given-names></name></name-alternatives><bio xml:lang="ru"><p>119017, Москва, Пыжевский пер, 7, стр. 2</p></bio><bio xml:lang="en"><p>7 Bld. 2 Pyzhevskiy per., Moscow 119017</p></bio><email xlink:type="simple">daniilkozlov@gmail.com</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>ФИЦ Почвенный институт им. В.В. Докучаева; МГУ им. М.В. Ломоносова</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Federal Research Centre V.V. Dokuchaev Soil Science Institute; Lomonosov Moscow State University</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>ФИЦ Почвенный институт им. В.В. Докучаева</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Federal Research Centre V.V. Dokuchaev Soil Science Institute</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-3"><aff xml:lang="ru"><institution>ЦАС Белгородский</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Agrochemical Service Center Belgorodskiy</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2020</year></pub-date><pub-date pub-type="epub"><day>03</day><month>12</month><year>2020</year></pub-date><volume>0</volume><issue>104</issue><fpage>158</fpage><lpage>198</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Смирнова М.А., Жидкин А.П., Лозбенев Н.И., Заздравных Е.А., Козлов Д.Н., 2020</copyright-statement><copyright-year>2020</copyright-year><copyright-holder xml:lang="ru">Смирнова М.А., Жидкин А.П., Лозбенев Н.И., Заздравных Е.А., Козлов Д.Н.</copyright-holder><copyright-holder xml:lang="en">Smirnova M.A., Zhidkin A.P., Lozbenev N.I., Zazdravnykh E.A., Kozlov D.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://bulletin.esoil.ru/jour/article/view/621">https://bulletin.esoil.ru/jour/article/view/621</self-uri><abstract><p>Деградация почв в результате водной эрозии представляет серьезную угрозу продовольственной и экологической безопасности, вследствие чего вопросы изучения и картографирования эрозии почв не теряют своей актуальности. В работе приведены результаты крупномасштабного            цифрового        картографирования     степени эродированности почвенного покрова пашни Прохоровского района Белгородской области (85 тыс га), выполненного на основании подходов, связывающих факторы эрозионно-аккумулятивных процессов и степень эродированности почв напрямую (модель фактор - свойство), и посредством имитационной эрозионной модели WaTEM/SEDEM (модель фактор - процесс - свойство). Включение процессной составляющей в алгоритм цифрового почвенного картографирования позволило учесть не только пространственные, но и временные особенности протекания эрозионных процессов. Выявлено, что распашка земель Прохоровского района в первую очередь проводилась на землях, слабо подверженных эрозии, с темпами эрозии почти в два раза ниже, чем на более молодых пашнях. В результате этого карты эродированности почв, построенные на основе модели фактор - процесс - свойство с учетом и без учета длительности распашки в значительной степени соответствуют друг другу. Карты доминантных почвенных категорий (пиксел карты соответствует одной категории почв - неэродированной и слабоэродированной, средне-, сильноэродированной), построенные с использованием моделей фактор - свойство и фактор - процесс -свойство, обладают высокой степенью соответствия друг другу (идентичность предсказания для 90% пикселей), в то время как карты комбинаций почв (пиксел карты содержит информацию о долевом участии почв разной степени эродированности) различаются в большей мере (идентичность менее чем для 60% пикселей). Площади зональных, эрозионно-зональных и слабоэродированных комбинаций почв отличаются в 1.5-2 раза в сторону большей степени эродированности почв на картах, построенных с использованием модели фактор -процесс - свойство.</p></abstract><trans-abstract xml:lang="en"><p>Soil degradation resulting from water erosion poses a serious threat to food and environmental security, therefore the research of soil erosion features and soil erosion mapping do not lose their relevance. The paper presents the results of large-scale digital mapping of the erosion degree of the arable soils in the Prokhorovsky district of the Belgorod region (85 thousand hectares), based on two approaches: (1) linking the factors of erosion-accumulative processes and the erosion degree of soil directly (factor -property model), and (2) due to imitation erosion model WaTEM/SEDEM (factor - process - property model). The inclusion of the process component into the digital soil mapping algorithm allows taking into account not only the spatial but also the temporal soil erosion features. It was revealed that the agricultural development of the Prokhorovsky district was primarily carried out on lands that are weakly prone to erosion, with the rate of erosion almost two times lower than on younger arable lands. As a result, the soil erosion maps, based on the factor - process - property model, with and without taking into account the duration of agricultural use, largely correspond to each other. Dominant soil categories (the map pixel corresponds to one soil taxa - noneroded and slightly eroded, medium, highly eroded), mapping by factor -property and factor - process - property models, have a high degree of correspondence to each other (prediction identity for 90% of pixels), while the soil combinations (the map pixel has information on the proportion of soils with different erosion degrees of soil) more significant (identity for less than 60% of pixels). The areas of zonal, erosion-zonal, and weakly eroded soil combinations differ 1.5-2 times, in the direction of a greater degree of soil erosion on the factor - process - property map.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>эрозионное моделирование</kwd><kwd>черноземы</kwd><kwd>Белгородская область</kwd><kwd>WATEM/SEDEM</kwd><kwd>структура почвенного покрова</kwd></kwd-group><kwd-group xml:lang="en"><kwd>erosion modeling</kwd><kwd>Chernozems</kwd><kwd>Belgorod region</kwd><kwd>WATEM/SEDEM</kwd><kwd>soil cover pattern</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Работа выполнена при финансовой поддержке РФФИ (проект № 18-3520011) и в рамках темы госзадания № 0591-2020-0029</funding-statement><funding-statement xml:lang="en">The studies were carried out with the financial support of the Russian Foundation for Basic Research (RFBR) (scientific project No. 18-35-20011) and within the framework of the theme of state assignment No. 0591-20200029</funding-statement></funding-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Белеванцев В.Г., Чендев Ю.Г. 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