Soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the Central Russian province

Aim. The aim of the research was to identify the influence of the climate factor on the soil processes in sandy podzols in the forest‐steppe of the Central Russian province.Material and Methods. Traditional methods (soil survey method, profile method, microbiological methods, etc.) and the latest me...

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Main Authors: N. P. Nevedrov, E. P. Protsenko, I. P. Balabina, M. Yu. Fomina, G. I. Popova
Format: Article
Language:Russian
Published: Kamerton 2022-04-01
Series:Юг России: экология, развитие
Subjects:
Online Access:https://ecodag.elpub.ru/ugro/article/view/2410
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author N. P. Nevedrov
E. P. Protsenko
I. P. Balabina
M. Yu. Fomina
G. I. Popova
author_facet N. P. Nevedrov
E. P. Protsenko
I. P. Balabina
M. Yu. Fomina
G. I. Popova
author_sort N. P. Nevedrov
collection DOAJ
description Aim. The aim of the research was to identify the influence of the climate factor on the soil processes in sandy podzols in the forest‐steppe of the Central Russian province.Material and Methods. Traditional methods (soil survey method, profile method, microbiological methods, etc.) and the latest methods (direct measurements [in situ] of soil CO2 emission) of investigation were used.Results. It has been established that soil formation processes in azonal Al‐Fe‐humus sandy soils are reflexive to variations in climatic parameters of the forest‐steppe zone. In warmer and arid conditions of the forest‐steppe (southern part), sandy sod‐podzols are formed, in colder and humid conditions of the forest‐steppe (northern part) – sandy podzols. The soddy‐podzols of the southern part of the forest‐steppe can be characterized by a more humous soil profile, the content of which is 19.2% higher than in the sandy podzols. More over sod‐podzols have greater availability of mineral nutrition elements for plants and a higher microbiological activity (the number of bacteria is 12.7 times higher, micromycetes – 10.5 times, actinomycetes – 4.5 times) than sandy podzols. In summer, the rate of CO2 emission in Al‐Fe‐humus sandy soils in the northern part of the forest‐steppe zone reached 9.1 g CO2 m2/day, in the southern part – 12.5 g CO2 m2/day.Conclusion. Further climate changes, which have an arid trend in the forest‐steppe zone, can possibly lead to transformation of sandy podzols into sandy sod‐podzols.
format Article
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institution Kabale University
issn 1992-1098
2413-0958
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publishDate 2022-04-01
publisher Kamerton
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series Юг России: экология, развитие
spelling doaj-art-4f6827fa33904db2bfc897c607c49aa32025-08-20T03:43:41ZrusKamertonЮг России: экология, развитие1992-10982413-09582022-04-01171809010.18470/1992-1098-2022-1-80-901223Soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the Central Russian provinceN. P. Nevedrov0E. P. Protsenko1I. P. Balabina2M. Yu. Fomina3G. I. Popova4Kursk State UniversityKursk State UniversityKursk State UniversityKursk State UniversityKursk State UniversityAim. The aim of the research was to identify the influence of the climate factor on the soil processes in sandy podzols in the forest‐steppe of the Central Russian province.Material and Methods. Traditional methods (soil survey method, profile method, microbiological methods, etc.) and the latest methods (direct measurements [in situ] of soil CO2 emission) of investigation were used.Results. It has been established that soil formation processes in azonal Al‐Fe‐humus sandy soils are reflexive to variations in climatic parameters of the forest‐steppe zone. In warmer and arid conditions of the forest‐steppe (southern part), sandy sod‐podzols are formed, in colder and humid conditions of the forest‐steppe (northern part) – sandy podzols. The soddy‐podzols of the southern part of the forest‐steppe can be characterized by a more humous soil profile, the content of which is 19.2% higher than in the sandy podzols. More over sod‐podzols have greater availability of mineral nutrition elements for plants and a higher microbiological activity (the number of bacteria is 12.7 times higher, micromycetes – 10.5 times, actinomycetes – 4.5 times) than sandy podzols. In summer, the rate of CO2 emission in Al‐Fe‐humus sandy soils in the northern part of the forest‐steppe zone reached 9.1 g CO2 m2/day, in the southern part – 12.5 g CO2 m2/day.Conclusion. Further climate changes, which have an arid trend in the forest‐steppe zone, can possibly lead to transformation of sandy podzols into sandy sod‐podzols.https://ecodag.elpub.ru/ugro/article/view/2410sod‐podzolal‐fe‐humus soilsco<sub>2</sub> emissionmicrobiological activityclimatic changes
spellingShingle N. P. Nevedrov
E. P. Protsenko
I. P. Balabina
M. Yu. Fomina
G. I. Popova
Soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the Central Russian province
Юг России: экология, развитие
sod‐podzol
al‐fe‐humus soils
co<sub>2</sub> emission
microbiological activity
climatic changes
title Soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the Central Russian province
title_full Soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the Central Russian province
title_fullStr Soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the Central Russian province
title_full_unstemmed Soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the Central Russian province
title_short Soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the Central Russian province
title_sort soil processes in sandy podzols under conditions of variations in climatic parameters of the forest steppe of the central russian province
topic sod‐podzol
al‐fe‐humus soils
co<sub>2</sub> emission
microbiological activity
climatic changes
url https://ecodag.elpub.ru/ugro/article/view/2410
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