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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">10.19047/0136-1694-2023-115-129-159</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-759</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>Спутниковая оценка агрономически важных свойств пахотных почв с учетом состояния их поверхности</article-title><trans-title-group xml:lang="en"><trans-title>Satellite based assessment of agronomically important properties of agricultural soils with consideration of their surface state</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-7743-8607</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Прудникова</surname><given-names>Е. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Prudnikova</surname><given-names>E. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Елена Юрьевна Прудникова</p><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">kiryan4ik@mail.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/0000-0002-8739-5441</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Савин</surname><given-names>И. Ю.</given-names></name><name name-style="western" xml:lang="en"><surname>Savin</surname><given-names>I. Yu.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Игорь Юрьевич Савин</p><p>119017, Москва, Пыжевский пер, 7, стр. 2; 117198, Москва, ул. Миклухо-Маклая, 6</p></bio><bio xml:lang="en"><p>7 Bld. 2 Pyzhevskiy per., Moscow 119017; 8/2 Miklukho-Maklaya Str., Moscow 117198</p></bio><email xlink:type="simple">savin_iyu@esoil.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/0000-0001-6325-4604</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Грубина</surname><given-names>П. Г.</given-names></name><name name-style="western" xml:lang="en"><surname>Grubina</surname><given-names>P. G.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Прасковья Георгиевна Грубина</p><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">grubina_pg@esoil.ru</email><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><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-2"><aff xml:lang="ru"><institution>ФИЦ “Почвенный институт им. В.В. Докучаева”; Российский университет дружбы народов</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Federal Research Centre “V.V. Dokuchaev Soil Science Institute”; Peoples' Friendship University of Russia</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>04</day><month>08</month><year>2023</year></pub-date><volume>0</volume><issue>115</issue><fpage>129</fpage><lpage>159</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Прудникова Е.Ю., Савин И.Ю., Грубина П.Г., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Прудникова Е.Ю., Савин И.Ю., Грубина П.Г.</copyright-holder><copyright-holder xml:lang="en">Prudnikova E.Y., Savin I.Y., Grubina P.G.</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/759">https://bulletin.esoil.ru/jour/article/view/759</self-uri><abstract><p>Спутниковые данные достаточно давно используются для оценки различных свойств пахотных почв. В то же время существуют определенные сложности, связанные с тем, что ряд агрономически важных свойств почв не оказывает непосредственного влияния на спектральную отражательную способность их поверхности, что осложняет дистанционную оценку таких свойств. Кроме того, для получения воспроизводимых моделей необходимо учитывать состояние открытой поверхности почв во время съемки. Целью исследования было провести демонстрацию метода детектирования агрономически важных свойств пахотных почв по спутниковым данным Landsat 8-9 OLI с привлечением информации о состоянии их открытой поверхности на примере тестового поля в Серебряно-Прудском районе Московской области. В зависимости от свойства почвы R2cv моделей, построенных по спутниковым данным Landsat 8-9 OLI, варьировал от 0.57 до 0.91. Наилучшие модели R2cv &gt; 0.8 были получены для органического вещества и сильно скоррелированных с ним свойств, таких как содержание обменных катионов кальция и магния, содержание общего азота, рН водной и солевой вытяжек. Привлечение информации о состоянии открытой поверхности пахотных почв для большинства свойств позволило получить модели более высокого качества и предсказательной способности вне зависимости от срока съемки. На основе полученных моделей в рамках демонстрации метода были построены карты пространственного варьирования агрономически важных свойств пахотных почв. Полученные модели могут быть использованы для дистанционного мониторинга анализируемых свойств пахотных почв тестового поля. В то же время для таких свойств, как содержание обменного калия и соединений фосфора необходим поиск подходов, учитывающих их высокую пространственную вариабельность, а также требуется предварительная оценка информативности сроков съемки, в которые открытая поверхность почвы не трансформирована.</p></abstract><trans-abstract xml:lang="en"><p>Satellite data have been used for a long time to assess various properties of arable soils. At the same time, there are certain difficulties associated with the fact that a number of agronomically important soil properties do not directly affect spectral reflectance of their surface, which complicates the remote assessment of such properties. In addition, to obtain reproducible models, it is necessary to take into account the state of the open soil surface during the survey. The aim of the study was to demonstrate a method for detecting agronomically important properties of arable soils based on Landsat 8-9 OLI satellite data and including information about the state of their open surface using the example of a test field in the Serebryano-Prudsky district of the Moscow region. Depending on the soil property, R2cv of the models developed based on Landsat 8-9 OLI satellite data varied from 0.57 to 0.91. The best models with R2cv&gt;0.8 were obtained for organic matter and properties higly correlated with it such as the content of exchangeable calcium and magnesium cations, the content of total nitrogen, pH of water and salt extracts. The involvement of information on the state of the open surface of arable soils for most properties made it possible to obtain models of higher quality and predictive ability, regardless of the survey period. Based on the models obtained, maps of the spatial variation of agronomically important properties of arable soils were constructed as part of the demonstration of the method. The resulting models can be used for remote monitoring of the analyzed properties of arable soils of the test field. At the same time, for such properties as the content of exchangeable potassium and phosphorus compounds, it is necessary to search for the approaches that will take into account their high variability, as well as to perform a prior assessment of the informativity of the survey periods in which the open soil surface is not transformed.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>дистанционные методы</kwd><kwd>пахотные почвы</kwd><kwd>агрономически важные свойства</kwd><kwd>Landsat 8-9 OLI</kwd><kwd>состояние открытой поверхности почв</kwd></kwd-group><kwd-group xml:lang="en"><kwd>remote methods</kwd><kwd>arable soils</kwd><kwd>agronomically important properties</kwd><kwd>Landsat 8-9 OLI</kwd><kwd>state of open soil surface</kwd></kwd-group></article-meta></front><back><ref-list><title>References</title><ref id="cit1"><label>1</label><citation-alternatives><mixed-citation xml:lang="ru">Виндекер Г.В., Прудникова Е.Ю., Савин И.Ю. 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