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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">10.19047/0136-1694-2019-98-5-36</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-325</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>ПОЧВЕННО-АГРОЭКОЛОГИЧЕСКАЯ ОЦЕНКА ПАХОТНОПРИГОДНОСТИ ЗЕМЕЛЬ ВАЛДАЙСКОЙ ВОЗВЫШЕННОСТИ ПО МАТЕРИАЛАМ ГЕНЕРАЛЬНОГО МЕЖЕВАНИЯ</article-title><trans-title-group xml:lang="en"><trans-title>SOIL-AGRO-ECOLOGICAL ASSESSMENT OF THE ARABLE LAND OF THE VALDAI UPLAND BASED ON THE GENERAL SURVEY</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-4113-6396</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Шилов</surname><given-names>П. М.</given-names></name><name name-style="western" xml:lang="en"><surname>Shilov</surname><given-names>P. M.</given-names></name></name-alternatives><bio xml:lang="ru"/><email xlink:type="simple">pavelshilovv@gmail.com</email><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-0103-0300</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"/><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>Почвенный институт имени В.В. Докучаева</institution><country>Россия</country></aff><aff xml:lang="en"><institution>V.V. Dokuchaev Soil Science Institute</institution><country>Russian Federation</country></aff></aff-alternatives><aff-alternatives id="aff-2"><aff xml:lang="ru"><institution>Почвенный институт им. В.В. Докучаева</institution><country>Russian Federation</country></aff><aff xml:lang="en"><institution>V.V. Dokuchaev Soil Science Institute</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2019</year></pub-date><pub-date pub-type="epub"><day>23</day><month>09</month><year>2019</year></pub-date><volume>0</volume><issue>98</issue><fpage>5</fpage><lpage>36</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Шилов П.М., Козлов Д.Н., 2019</copyright-statement><copyright-year>2019</copyright-year><copyright-holder xml:lang="ru">Шилов П.М., Козлов Д.Н.</copyright-holder><copyright-holder xml:lang="en">Shilov P.M., 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/325">https://bulletin.esoil.ru/jour/article/view/325</self-uri><abstract><p>Предложен методический подход к цифровому картографированию ареала пахотнопригодных земель в зависимости от их почвенно-агроэкологических и позиционных условий. Подход апробирован для модельного участка Валдайской возвышенности площадью 160 тыс. га. Мелкоочаговое земледельческое освоение слаборасчлененных моренных равнин ограничено широким распространением избыточно увлажненных почв. Средствами канонического дискриминантного анализа рассчитана мера топографически обусловленной продолжительности переувлажнения почв на основе сопоставления морфологической диагностики их водного режима и стокоформирующих свойств рельефа по элементам сетки 30 × 30 м. Определен диапазон дренируемости для реконструированного по материалам Генерального межевания ареала пашни конца XVIII века, что позволило оценить потенциальный ареал пахотнопригодных земель в этот период. Площадь пашни, равновесная благоприятным условиям транспортной доступности и дренируемости почв, составила 12 %. В то же самое время ее фактическая площадь, реконструированная по материалам Генерального межевания, составила 5 %. В условиях натурального хозяйства XVIII в. больше половины потенциально пригодных земель модельного региона оказались неосвоенными.</p></abstract><trans-abstract xml:lang="en"><p>A methodical approach to the digital mapping of the arable lands area depending on their soil-agroecological and positional conditions is proposed. The approach was tested on a model plot located on the Valdai Upland with an area of 160 thousand ha. Small-scale agricultural development of the poorly dissected moraine plains is limited by the wide distribution of overmoistened soils. Using the traditional discriminant analysis, a measure of the topographically determined duration of soil overmoistening was calculated based on a comparison of the morphological diagnostics of water regime and topography runoff properties according to the grid elements of 30 × 30 m. The drainability range was determined for the arable lands of XVIII century, reconstructed according to the materials of the General Survey. This allowed us to determine the potential area of the arable lands for this period. The area of arable lands, which is characterized by favorable conditions of transport accessibility and soil drainability, was 12 %. At the same time, reconstructed area contained 5 %. In the subsistence economy of the XVIII century more than a half of the potential arable lands of the model region turned out to be undeveloped.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>цифровая почвенная картография</kwd><kwd>Центрально-Лесной заповедник</kwd><kwd>природа и общество</kwd></kwd-group><kwd-group xml:lang="en"><kwd>digital soil mapping</kwd><kwd>Central Forest Reserve</kwd><kwd>nature and society</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Авторы благодарят А.А. Голубинского за помощь в вы-явлении и подготовке к копированию материалов Генерально-го межевания в РГАДА, проф. Н.В. Козлову за ценные кон-сультации в области общественных и экономических отноше-ний в России XVIII в. 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