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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">10.19047/0136-1694-2023-116-43-75</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-744</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>Влияния внесения биоугля на теплофизические свойства дерново-подзолистой почвы и составляющие энергетического баланса яровой пшеницы в Ленинградской области при различных условиях почвенного увлажнения</article-title><trans-title-group xml:lang="en"><trans-title>Influence of the biochar application on the thermal properties of soddy-podzolic soil and on the energy balance fluxes of spring wheat in the Leningrad region under various soil moisture conditions</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author" corresp="yes"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0002-9368-6229</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Доброхотов</surname><given-names>А. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Dobrokhotov</surname><given-names>A. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>научный сотрудник</p></bio><email xlink:type="simple">dobralexey@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/0000-0001-7990-8211</contrib-id><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Козырева</surname><given-names>Л. В.</given-names></name><name name-style="western" xml:lang="en"><surname>Kozyreva</surname><given-names>L. V.</given-names></name></name-alternatives><bio xml:lang="ru"><p>ведущий инженер</p></bio><email xlink:type="simple">4ludak@gmail.com</email><xref ref-type="aff" rid="aff-2"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Агрофизический научно-исследовательский институт,&#13;
Почвенный институт имени В.В. Докучаева</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Agrophysical Research Institute&#13;
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>Агрофизический научно-исследовательский институт</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Agrophysical Research Institute</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2023</year></pub-date><pub-date pub-type="epub"><day>25</day><month>09</month><year>2023</year></pub-date><volume>0</volume><issue>116</issue><fpage>43</fpage><lpage>75</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Доброхотов А.В., Козырева Л.В., 2023</copyright-statement><copyright-year>2023</copyright-year><copyright-holder xml:lang="ru">Доброхотов А.В., Козырева Л.В.</copyright-holder><copyright-holder xml:lang="en">Dobrokhotov A.V., Kozyreva L.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://bulletin.esoil.ru/jour/article/view/744">https://bulletin.esoil.ru/jour/article/view/744</self-uri><abstract><p>В статье приведены результаты полевого эксперимента по оценке влияния предпосевного внесения биоугля на теплофизические свойства пахотного горизонта дерново-подзолистой супесчаной почвы, составляющие энергетического баланса, температуру подстилающей поверхности и температуру листьев яровой пшеницы сорта “Дарья” при различных условиях почвенного увлажнения в 2022 г. Эксперимент проводился на территории Меньковской опытной станции Агрофизического научно-исследовательского института, расположенной в Гатчинском районе Ленинградской области. Эксперимент включал опытный участок с внесением биоугля в дозе 21.9 т га-1 и контрольный участок. Условия почвенного увлажнения и влагообеспеченность пшеницы характеризовались объемной влажностью почвы и суммарным испарением. По результатам полевых экспериментов было обнаружено значимое влияние (p &lt; 0.05) внесения биоугля на теплофизические свойства почвы, однако в условиях различного увлажнения влияние было разнонаправленное. При влажности почвы в абсолютно сухом состоянии внесение биоугля уменьшило на 29.7% теплопроводность, уменьшило на 18.5% объемную теплоемкость, уменьшило на 13.7% температуропроводность, уменьшило на 24.3% тепловую инерцию. При значениях влажности почвы, соответствующей наименьшей влагоемкости, внесение биоугля увеличило на 9.4% теплопроводность, уменьшило на 2.6% объемную теплоемкость, увеличило на 12.3% температуропроводность, увеличило на 3.2% тепловую инерцию. Внесение биоугля значимо (p &lt; 0.05) за счет увеличения температуры подстилающей поверхности (на 6.4%) увеличило турбулентный поток тепла на 35.5%. Вследствие снижения испарения с поверхности почвы внесение биоугля уменьшило на 17.0% скрытый поток тепла и на 13.9% суммарное испарение. Температура листьев характеризует транспирацию растительности, которая может повышаться при внесении биоугля на легких почвах из-за увеличения влагоемкости. В нашем эксперименте внесение биоугля не оказало значимых изменений на температуру листьев растений. Результаты эксперимента подтверждаются многочисленными выводами как зарубежных, так и отечественных исследователей.</p></abstract><trans-abstract xml:lang="en"><p>The article presents the results of a field experiment to assess the effect of pre-sowing application of the biochar on the thermal properties of the arable horizon of soddy-podzolic sandy loam soil, on the energy balance components, on the crop surface temperature and on the leaves temperature of spring wheat (variety “Daria”) under various conditions of soil moisture in 2022. The experiment took place at the Menkovo Experimental Station of the Agrophysical Research Institute, located in the Gatchinsky District of the Leningrad Region. The experiment included the plot with the biochar application at the dose of 21.9 t ha-1 and the control plot. The soil thermal properties were measured by the heat pulse method. The components of the energy balance were determined using agrometeorological measurements, radiation balance measurements, crop surface temperature, and phenological measurements. The crop surface temperature was measured by a non-contact method using pyrometers. The soil moisture conditions and available water for wheat were characterized by volumetric soil moisture and evapotranspiration. The volumetric soil moisture was measured using a capacitive soil moisture sensor. The evapotranspiration was determined using the residual term of the energy balance equation through the latent heat flux. According to the results of field experiments, a significant effect (p &lt; 0.05) of the biochar application on the soil thermal properties was found, however, under different moisture conditions, the effect was multidirectional. At zero soil moisture, the biochar application reduced thermal conductivity by 29.7%, reduced volumetric heat capacity by 18.5%, reduced diffusivity by 13.7%, and reduced thermal inertia by 24.3%. Under the conditions of field capacity, the biochar application increased thermal conductivity by 9.4%, reduced volumetric heat capacity by 2.6%, increased diffusivity by 12.3%, and increased thermal inertia by 3.2%. The biochar application significantly (p &lt; 0.05) increased the turbulent heat flux – by 35.5%, which is due to an increase in the crop surface temperature (by 6.4%). Resulting from the decrease in soil evaporation, the biochar application reduced the latent heat flux by 17.0%, and the evapotranspiration by 13.9%. Leaf temperature is related to transpiration. Transpiration can increase when biochar is applied on light-textured soils due to an increase in soil water capacity. The biochar application did not result in significant changes of leaf temperature. The study results are confirmed by numerous articles of both foreign and Russian researchers.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>биоуголь</kwd><kwd>дерново-подзолистая супесчаная почва</kwd><kwd>теплофизические свойства почвы</kwd><kwd>составляющие энергетического баланса</kwd><kwd>температура подстилающей поверхности</kwd><kwd>температура листьев</kwd><kwd>суммарное испарение.</kwd></kwd-group><kwd-group xml:lang="en"><kwd>biochar</kwd><kwd>soddy-podzolic sandy loam soil</kwd><kwd>soil thermal properties</kwd><kwd>energy balance components</kwd><kwd>crop surface temperature</kwd><kwd>leaf temperature</kwd><kwd>evapotranspiration</kwd></kwd-group><funding-group><funding-statement xml:lang="ru">Авторы выражают благодарность Чикишеву Дмитрию Владимировичу и Балашову Евгению Владимировичу за содействие в проведении исследований, Моисееву Кириллу Геннадьевичу за предоставление материалов исследований гранулометрического состава почвы на сельскохозяйственных полях Меньковской опытной станции Агрофизического научно-исследовательского института.</funding-statement><funding-statement xml:lang="en">The authors would like to thank Dmitry Vladimirovich Chikishev and Evgeny Vladimirovich Balashov for their assistance in conducting the research, Kirill Gennadyevich Moiseev for providing the materials on particle size distribution of soil on agricultural fields of Menkovo experimental station of Agrophysical Research Institute.</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">Моисеев К.Г., Зинчук Е.Г. 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