Diversity of soils in the Dnipro River valley (based on the example of the Dnipro-Orilsky Nature Reserve)

The study established the classification position of the soils of the Dnipro River valley (within the Dnipro-Orilsky Nature Reserve) according to the international WRB classification. The pits were laid along three transects that passed through the most significant relief gradients within the study...

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Main Authors: Yakovenko Volodymyr, Kunakh Olga, Tutova Hanna, Zhukov Olexander
Format: Article
Language:English
Published: Sciendo 2023-07-01
Series:Folia Oecologica
Subjects:
Online Access:https://doi.org/10.2478/foecol-2023-0011
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author Yakovenko Volodymyr
Kunakh Olga
Tutova Hanna
Zhukov Olexander
author_facet Yakovenko Volodymyr
Kunakh Olga
Tutova Hanna
Zhukov Olexander
author_sort Yakovenko Volodymyr
collection DOAJ
description The study established the classification position of the soils of the Dnipro River valley (within the Dnipro-Orilsky Nature Reserve) according to the international WRB classification. The pits were laid along three transects that passed through the most significant relief gradients within the study area. The study of the morphological structure of 20 soil profiles showed that the soil cover is closely related to the geo-morphological structure of the river valley. The morphological characteristics of typical profiles of these soils reflect their structure, properties and genesis and determine the classification position of the soils according to the WRB. Multidimensional scaling allowed us to perform soil ordination in the space of two dimensions. Dimension 1 differentiates soils by the gradient of relief height and/or moisture level. Dimension 2 differentiated hydromorphic soils. The properties of Quaternary sediments were found to determine the position of soils at both levels of classification (reference groups, main and additional classifiers). The distribution of each of the reference groups is clearly related to the geomorphology of the valley. Arenosols and Cambisols form the soil cover of the floodplain terrace, while Fluvisols and Gleysols are found mainly in the floodplain.
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spelling doaj.art-4e0b1f19fa054b2fa3e9f34ecf17c4ca2023-08-01T05:16:35ZengSciendoFolia Oecologica1338-70142023-07-0150211913310.2478/foecol-2023-0011Diversity of soils in the Dnipro River valley (based on the example of the Dnipro-Orilsky Nature Reserve)Yakovenko Volodymyr0Kunakh Olga1Tutova Hanna2Zhukov Olexander31Oles Gonchar Dnipro National University, Gagarin av., 72, Dnipro, 49000, Ukraine1Oles Gonchar Dnipro National University, Gagarin av., 72, Dnipro, 49000, Ukraine2Bogdan Khmelnitsky Melitopol State Pedagogical University, Hetmanska st., 20, Melitopol, 72318, Ukraine2Bogdan Khmelnitsky Melitopol State Pedagogical University, Hetmanska st., 20, Melitopol, 72318, UkraineThe study established the classification position of the soils of the Dnipro River valley (within the Dnipro-Orilsky Nature Reserve) according to the international WRB classification. The pits were laid along three transects that passed through the most significant relief gradients within the study area. The study of the morphological structure of 20 soil profiles showed that the soil cover is closely related to the geo-morphological structure of the river valley. The morphological characteristics of typical profiles of these soils reflect their structure, properties and genesis and determine the classification position of the soils according to the WRB. Multidimensional scaling allowed us to perform soil ordination in the space of two dimensions. Dimension 1 differentiates soils by the gradient of relief height and/or moisture level. Dimension 2 differentiated hydromorphic soils. The properties of Quaternary sediments were found to determine the position of soils at both levels of classification (reference groups, main and additional classifiers). The distribution of each of the reference groups is clearly related to the geomorphology of the valley. Arenosols and Cambisols form the soil cover of the floodplain terrace, while Fluvisols and Gleysols are found mainly in the floodplain.https://doi.org/10.2478/foecol-2023-0011floodplainlandscape managementmultidimensional scalingnature conservationsoil covertransition matrix
spellingShingle Yakovenko Volodymyr
Kunakh Olga
Tutova Hanna
Zhukov Olexander
Diversity of soils in the Dnipro River valley (based on the example of the Dnipro-Orilsky Nature Reserve)
Folia Oecologica
floodplain
landscape management
multidimensional scaling
nature conservation
soil cover
transition matrix
title Diversity of soils in the Dnipro River valley (based on the example of the Dnipro-Orilsky Nature Reserve)
title_full Diversity of soils in the Dnipro River valley (based on the example of the Dnipro-Orilsky Nature Reserve)
title_fullStr Diversity of soils in the Dnipro River valley (based on the example of the Dnipro-Orilsky Nature Reserve)
title_full_unstemmed Diversity of soils in the Dnipro River valley (based on the example of the Dnipro-Orilsky Nature Reserve)
title_short Diversity of soils in the Dnipro River valley (based on the example of the Dnipro-Orilsky Nature Reserve)
title_sort diversity of soils in the dnipro river valley based on the example of the dnipro orilsky nature reserve
topic floodplain
landscape management
multidimensional scaling
nature conservation
soil cover
transition matrix
url https://doi.org/10.2478/foecol-2023-0011
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