Patterns of soil cover organization within the northern part of the Kondinskaya lowland (Western Siberia) | Vestnik Tomskogo gosudarstvennogo universiteta. Biologiya - Tomsk State University Journal of Biology. 2020. № 49. DOI: 10.17223/19988591/49/1

Patterns of soil cover organization within the northern part of the Kondinskaya lowland (Western Siberia)

The paper presents the results of the studies devoted to the morphological features and properties of soils representing different geomorphological conditions within the elevated relief forms of the Kondinskaya lowland, with the example of the Kondinskie Lakes Natural Park area. The northern part of the Kondinskaya lowland is characterized by a contrasting and diverse relief, which is generally not typical of the middle taiga zone of Western Siberia. Soil-morphological and -geomorphological methods formed the structural framework of this research. The results showed that Folic Albic Podzols (Geoabruptic) formed on the flat tops of ridges are characterized by a moderate thickness of the E horizon, the largest number of rock fragments, as well as by bedding with loams that have signs of paleocryogenic deformations. Albic Podzols of terraced slopes have more developed E and Bs horizons with large wedge like tongues having depth of about one meter. This group of soils is distinguished by the most diverse structure of the upper part of the profile due to the variability of morphological elements related to biogenic pedoturbations. Albic Lamellic Arenosols occupying steep slopes of the ridges are less developed, and erosional processes often interrupt soil development within this geomorphic position. Albic Gleyic Podzols (Turbic) formed under the steep slopes of high ridges develop over buried Podzols, and often contain charcoal-enriched interlayers in the bottom and middle parts of the profile. Formation of a complex profile, with series of burials, is possibly associated with the activation of erosional processes related to fires and ancient human activity. Study results showed that there is a strong relationship between the lithology on the one hand, and the intensity of podzolization and variability of soil morphological elements related to biogenic pedoturbations on the other hand. The paper contains 5 Figures, 1 Table and 51 References. The Authors declare no conflict of interest.

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Keywords

Albic Podzols, middle taiga, Kondinskie Lakes Natural Park, Western Siberia, buried soils, morphological elements, binomial deposits, подзолы иллювиально-железистые, средняя тайга, Природный Парк Кондинские озера, Западная Сибирь, погребенные почвы, морфологические элементы, двучленные отложения

Authors

Name	Organization	E-mail
Kurasova Alina O.	Tomsk State University	kurasovalina@gmail.com
Konstantinov Alexandr O.	Tyumen State University	konstantinov.alexandr72@gmail.com
Kulizhskiy Sergey P.	Tomsk State University	kulizhskiy@yandex.ru
Konstantinova Elizaveta Yu.	Southern Federal University	konstantliza@gmail.ru
Khoroshavin Vitaliy Yu.	Tyumen State University	purriver@mail.ru
Loyko Sergey V.	Tomsk State University; Tomsk Oil and Gas Research and Design Institute	s.loyko@yandex.ru

Всего: 6

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