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Особенности почв степных кластеров Хакасского заповедника Т. А. Марон, С. П. Кулижский, А. В. Родикова

By: Марон, Татьяна АлексеевнаContributor(s): Кулижский, Сергей Павлинович | Родикова, Анна ВикторовнаMaterial type: ArticleArticleContent type: Текст Media type: электронный Other title: Features of steppe cluster soils Khakassky Nature Reserve [Parallel title]Subject(s): Хакасский, государственный природный заповедник | почвы степей | полевые исследованияGenre/Form: статьи в сборниках Online resources: Click here to access online In: Почва как связующее звено функционирования природных и антропогенно-преобразованных экосистем [Электронный ресурс] : материалы V Международной научной конференции, посвященной 90-летию кафедры почвоведения и оценки земельных ресурсов ИГУ, Иркутск, 23–29 августа 2021 года С. 451-455Abstract: The soils of the steppe areas of the Khakassky Nature Reserve (“Lake Shira”, “Lake Bele”, “Kamyzyaksky steppe and Lake Ulug-Kol”) are considered. They include, as a key element, the water area of non-flowing mineralized lakes and the adjacent landscapes with variegated soil cover. The subordinate position determines the conditions for the additional inflow of moisture and substances, the features of humidification-drying, freezing-thawing. In the contact zones of territorial and aquatic complexes, active exodynamic processes occur: waterlogging, salinization, and others. The research results demonstrate a number of features of the morphology and composition of soils, which is determined by a whole complex of local factors of soil formation, such as, for example, the composition of soil-forming rocks, stratified material, proximity to lakes, and others. Among the features of the profiles, both natural and anthropogenic manifestations are noted: surface cracks, cryoturbation, salt accumulation, violations of various genesis.
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The soils of the steppe areas of the Khakassky Nature Reserve (“Lake Shira”, “Lake Bele”, “Kamyzyaksky steppe and Lake Ulug-Kol”) are considered. They include, as a key element, the water area of non-flowing mineralized lakes and the adjacent landscapes with variegated soil cover. The subordinate position determines the conditions for the additional inflow of moisture and substances, the features of humidification-drying, freezing-thawing. In the contact zones of territorial and aquatic complexes, active exodynamic processes occur: waterlogging, salinization, and others. The research results demonstrate a number of features of the morphology and composition of soils, which is determined by a whole complex of local factors of soil formation, such as, for example, the composition of soil-forming rocks, stratified material, proximity to lakes, and others. Among the features of the profiles, both natural and anthropogenic manifestations are noted: surface cracks, cryoturbation, salt accumulation, violations of various genesis.

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