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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">10.19047/0136-1694-2025-125-111-137</article-id><article-id custom-type="elpub" pub-id-type="custom">esoil-934</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>Почвенные условия биоценозов Quercus pubescens Willd. Южного берега Крыма</article-title><trans-title-group xml:lang="en"><trans-title>Soil conditions of biocenoses Quercus pubescens Willd. of the Southern coast of Crimea</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>Коба</surname><given-names>В. П.</given-names></name><name name-style="western" xml:lang="en"><surname>Koba</surname><given-names>V. P.</given-names></name></name-alternatives><bio xml:lang="ru"><p>298648, Республика Крым, Ялта, пгт Никита, Никитский спуск, 52</p></bio><bio xml:lang="en"><p>52 Nikitsky descent, Nikita urban settlement, Yalta 298648, Republic of Crimea</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Новицкий</surname><given-names>М. Л.</given-names></name><name name-style="western" xml:lang="en"><surname>Novitsky</surname><given-names>M. L.</given-names></name></name-alternatives><bio xml:lang="ru"><p>Новицкий Максим Леонидович</p><p>298648, Республика Крым, Ялта, пгт Никита, Никитский спуск, 52</p></bio><bio xml:lang="en"><p>52 Nikitsky descent, Nikita urban settlement, Yalta 298648, Republic of Crimea</p></bio><email xlink:type="simple">maxim.novickiy@bk.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>Пшеничников</surname><given-names>Н. А.</given-names></name><name name-style="western" xml:lang="en"><surname>Pshenichnikov</surname><given-names>N. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>298648, Республика Крым, Ялта, пгт Никита, Никитский спуск, 52</p></bio><bio xml:lang="en"><p>52 Nikitsky descent, Nikita urban settlement, Yalta 298648, Republic of Crimea</p></bio><xref ref-type="aff" rid="aff-1"/></contrib><contrib contrib-type="author" corresp="yes"><name-alternatives><name name-style="eastern" xml:lang="ru"><surname>Нагорняк</surname><given-names>А. A.</given-names></name><name name-style="western" xml:lang="en"><surname>Nagornyak</surname><given-names>A. A.</given-names></name></name-alternatives><bio xml:lang="ru"><p>298648, Республика Крым, Ялта, пгт Никита, Никитский спуск, 52</p></bio><bio xml:lang="en"><p>52 Nikitsky descent, Nikita urban settlement, Yalta 298648, Republic of Crimea</p></bio><xref ref-type="aff" rid="aff-1"/></contrib></contrib-group><aff-alternatives id="aff-1"><aff xml:lang="ru"><institution>Никитский ботанический сад – Национальный научный центр РАН</institution><country>Россия</country></aff><aff xml:lang="en"><institution>Nikitsky Botanical Garden – National Scientific Center of the Russian Academy of Sciences</institution><country>Russian Federation</country></aff></aff-alternatives><pub-date pub-type="collection"><year>2025</year></pub-date><pub-date pub-type="epub"><day>09</day><month>11</month><year>2025</year></pub-date><volume>0</volume><issue>125</issue><fpage>111</fpage><lpage>137</lpage><permissions><copyright-statement>Copyright &amp;#x00A9; Коба В.П., Новицкий М.Л., Пшеничников Н.А., Нагорняк А.A., 2025</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="ru">Коба В.П., Новицкий М.Л., Пшеничников Н.А., Нагорняк А.A.</copyright-holder><copyright-holder xml:lang="en">Koba V.P., Novitsky M.L., Pshenichnikov N.A., Nagornyak A.A.</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/934">https://bulletin.esoil.ru/jour/article/view/934</self-uri><abstract><p>Исследования проводили в биоценозах Q. pubescens Южного берега Крыма. В западной, центральной и восточной частях исследуемого района было заложено 6 пробных площадей. Основная часть почв представлена коричневыми слабомощными на элюводелювии известняков и глинистых сланцев, на “Мыс Мартьян” – коричневыми красноцветными (terra rossa), сформировавшимися на мощном слое выщелоченных продуктов выветривания верхнеюрских известняков. В почвах изучали структуру и состав фитоценоза, таксационные характеристики насаждений, особенности почвенных условий. Выявлено, что наиболее жесткие условия по характеристике качества почвенной среды в настоящее время складываются в западной части произрастания Q. pubescens на Южном берегу Крыма. В насаждениях Ласпи и Кастрополя самый низкий уровень концентрации гумуса и содержания влаги в почве. В центральной части массива лесов Q. pubescens, при некотором улучшении почвенных условий, общая специфика изменения качества почвенной среды весьма близка к насаждениям западных территорий. Установлено, что рост и развитие древостоев Q. pubescens мыса Ай-Тодор в значительной степени определяются сезонной динамикой увлажненности почвы. Сравнительно высокое содержание влаги в почве в первые месяцы вегетации положительно влияет на рост Q. pubescens; резкое ее снижение во второй половине лета до значений, близких к показателям биоценозов западной части, оказывает стрессовое действие на состояние древостоев на мысе Ай-Тодор. В восточной части Южного берега Крыма на почвенные условия в биоценозах Q. pubescens значительное действие оказывает подстилающий грунт. Габрро-диабаз лакколитов Аю-Даг и Кастель влияет на кислотность почвы, особенности формирования и накопления гумуса. Показано, что плотные слои габрро-диабаза повышают влагообеспечение древостоев Q. pubescens в экотопах г. Аю-Даг и Кастель. Сделан вывод, что тотальная вырубка в прошлом коренных древостоев Q. pubescens Южного берега Крыма определила глубокую деградацию структуры и состава растительных сообществ, формирование на данных территориях низкопродуктивных порослевых насаждений. Одной из причин деструктивных явлений в развитии биоценозов Q. pubescens является изменение водного баланса почвенной среды. Возможности роста порослевых насаждений Q. pubescens Южного берега Крыма в настоящее время обеспечиваются мощной корневой системой материнского древостоя, которая продолжает еще функционировать.</p></abstract><trans-abstract xml:lang="en"><p>The study was conducted in the biocenoses of Quercus pubescens on the Southern Coast of Crimea. Six sample plots were established in the western, central, and eastern parts of the study area. The soils are predominantly brown, weakly developed on eluvium-deluvium of limestones and clay shales, while at “Cape Martyan” they are brown reddish-brown soils (Terra Rossa) formed on a thick layer of leached weathering products of Upper Jurassic limestones. The study examined the structure and composition of the phytocenosis, taxation characteristics of the stands, and specific soil conditions. It was revealed that the most stringent conditions for the characteristics of the quality of the soil environment are currently developing in the western part of Q. pubescens growth on the Southern Coast of Crimea. The soil under Laspi and Kastropol plantings have the lowest humus concentration and moisture content. In the central part of the Q. pubescens forest, with some improvement in soil conditions, the general specificity of changes in the quality of the soil environment is very close to the plantings of the western territories. It was found that the growth and development of Q. pubescens stands on Cape Ai-Todor are largely determined by the seasonal dynamics of soil moisture. The relatively high moisture content in the soil during the first months of vegetation has a positive effect on the growth of Q. pubescens; and its sharp decrease in the second half of summer to values, close to the indicators of the biocenoses of the western part, shows a stressful effect on the condition of the forest stands on Cape Ai-Todor. In the eastern part of Q. pubescens habitat on the Southern Coast of Crimea, the underlying bedrock has a significant effect on soil conditions. Gabbro-diabase of the Ayu-Dag and Kastel laccoliths affects soil acidity, features of humus formation and accumulation. It is shown that dense gabbro-diabase layers increase moisture supply of Q. pubescens stands in the Ayu-Dag and Kastel ecotopes. It is concluded that the total cutting of primary Q. pubescens stands on the Southern Coast of Crimea in the past determined the deep degradation of the structure and composition of plant communities, the formation of low-productivity coppice plantations in these areas. One of the causes of destructive phenomena in the development of Q. pubescens biocenoses is a change in the water balance of the soil environment. The growth potential of Q. pubescens coppice stands on the Southern Coast of Crimea is currently provided by the powerful root system of the parent tree stand, which continues to function.</p></trans-abstract><kwd-group xml:lang="ru"><kwd>terra rossa</kwd><kwd>коричневые почвы</kwd><kwd>биоценоз</kwd><kwd>древостой</kwd><kwd>почва</kwd><kwd>гранулометрический состав</kwd><kwd>гумус</kwd><kwd>влажность</kwd></kwd-group><kwd-group xml:lang="en"><kwd>terra rossa</kwd><kwd>brown soils</kwd><kwd>biocenosis</kwd><kwd>forest stand</kwd><kwd>soil</kwd><kwd>granulometric composition</kwd><kwd>humus</kwd><kwd>humidity</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">Алексеев В.А. Лесные экосистемы и атмосферное загрязнение. 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