Genetic Characteristics of Brown Forest Soils on the Middle Urals

Samofalova Iraida

doi:doi:10.11648/j.ajep.s.2015040301.33

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Genetic Characteristics of Brown Forest Soils on the Middle Urals

Samofalova Iraida

Published in American Journal of Environmental Protection (Volume 4, Issue 3-1)

Received: 5 March 2015 Accepted: 8 March 2015 Published: 25 June 2015

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Abstract

Feature of mountain soil formation is that the soils on the mountain slopes are formed in different bioclimatic and orogeomorfological conditions. The purpose of research is to study genetic properties of the brown forest soils in the Middle Urals. Features of the morphological structure: truncated profile (35-75 cm), weakly expressed in the differentiation of the soil profile into individual Horizons, detritus (20-65%), loamy fine earth, the signs of podzolization in the soil profile is not found. Feature granulometric size distribution of the soil - a gradual increase in weight on the profile into Sandy Loam to Silty Clay and Clay, the dominant factions are either big Silt or Sand. Soils are characterized by a very acidic environment and high hydrolytic acidity. The soils are enriched in organic matter and humus profile characterized by prolixity. Group composition humus shows mobility, high degree of humification of organic substances to fulvic acids. Gross composition shows that the processes of soil formation on Mount, North Basegi aren’t leading to a distinctly different profile. Coefficients of geochemical accumulation, subsurface weathering, eluviation, oxidation calculated and helped define the features of the gross composition of soils. Character of distribution in profile and correlation of forms of iron help to diagnose physical processes of weathering and soil formation (burozemic pedogenesis et al.); signs Podzolization not revealed. Weathering and soil formation processes that occur with varying intensity, creating a diversity of soil cover and the spatial heterogeneity of soils, even within the same type. Thus, in the mountains of the Middle Urals brown forest soils form a number of subtypes: raw organic (900 m) - ferruginized (655 m) - metamorphosed (590 m) - clay-illuvial (577 m) - eluvial (565 m) - clay-illuvial (315 m).

Published in	American Journal of Environmental Protection (Volume 4, Issue 3-1) This article belongs to the Special Issue Applied Ecology: Problems, Innovations
DOI	10.11648/j.ajep.s.2015040301.33
Page(s)	148-156
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2015. Published by Science Publishing Group

Keywords

Brown Forest Soils, Properties, Genetic Horizons, Soil Profile, Soil Formation, Weathering Processes

References

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Samofalova Iraida. (2015). Genetic Characteristics of Brown Forest Soils on the Middle Urals. American Journal of Environmental Protection, 4(3-1), 148-156. https://doi.org/10.11648/j.ajep.s.2015040301.33

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Samofalova Iraida. Genetic Characteristics of Brown Forest Soils on the Middle Urals. Am. J. Environ. Prot. 2015, 4(3-1), 148-156. doi: 10.11648/j.ajep.s.2015040301.33

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Samofalova Iraida. Genetic Characteristics of Brown Forest Soils on the Middle Urals. Am J Environ Prot. 2015;4(3-1):148-156. doi: 10.11648/j.ajep.s.2015040301.33

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@article{10.11648/j.ajep.s.2015040301.33,
  author = {Samofalova Iraida},
  title = {Genetic Characteristics of Brown Forest Soils on the Middle Urals},
  journal = {American Journal of Environmental Protection},
  volume = {4},
  number = {3-1},
  pages = {148-156},
  doi = {10.11648/j.ajep.s.2015040301.33},
  url = {https://doi.org/10.11648/j.ajep.s.2015040301.33},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajep.s.2015040301.33},
  abstract = {Feature of mountain soil formation is that the soils on the mountain slopes are formed in different bioclimatic and orogeomorfological conditions. The purpose of research is to study genetic properties of the brown forest soils in the Middle Urals. Features of the morphological structure: truncated profile (35-75 cm), weakly expressed in the differentiation of the soil profile into individual Horizons, detritus (20-65%), loamy fine earth, the signs of podzolization in the soil profile is not found. Feature granulometric size distribution of the soil - a gradual increase in weight on the profile into Sandy Loam to Silty Clay and Clay, the dominant factions are either big Silt or Sand. Soils are characterized by a very acidic environment and high hydrolytic acidity. The soils are enriched in organic matter and humus profile characterized by prolixity. Group composition humus shows mobility, high degree of humification of organic substances to fulvic acids. Gross composition shows that the processes of soil formation on Mount, North Basegi aren’t leading to a distinctly different profile. Coefficients of geochemical accumulation, subsurface weathering, eluviation, oxidation calculated and helped define the features of the gross composition of soils. Character of distribution in profile and correlation of forms of iron help to diagnose physical processes of weathering and soil formation (burozemic pedogenesis et al.); signs Podzolization not revealed. Weathering and soil formation processes that occur with varying intensity, creating a diversity of soil cover and the spatial heterogeneity of soils, even within the same type. Thus, in the mountains of the Middle Urals brown forest soils form a number of subtypes: raw organic (900 m) - ferruginized (655 m) - metamorphosed (590 m) - clay-illuvial (577 m) - eluvial (565 m) - clay-illuvial (315 m).},
 year = {2015}
}

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TY  - JOUR
T1  - Genetic Characteristics of Brown Forest Soils on the Middle Urals
AU  - Samofalova Iraida
Y1  - 2015/06/25
PY  - 2015
N1  - https://doi.org/10.11648/j.ajep.s.2015040301.33
DO  - 10.11648/j.ajep.s.2015040301.33
T2  - American Journal of Environmental Protection
JF  - American Journal of Environmental Protection
JO  - American Journal of Environmental Protection
SP  - 148
EP  - 156
PB  - Science Publishing Group
SN  - 2328-5699
UR  - https://doi.org/10.11648/j.ajep.s.2015040301.33
AB  - Feature of mountain soil formation is that the soils on the mountain slopes are formed in different bioclimatic and orogeomorfological conditions. The purpose of research is to study genetic properties of the brown forest soils in the Middle Urals. Features of the morphological structure: truncated profile (35-75 cm), weakly expressed in the differentiation of the soil profile into individual Horizons, detritus (20-65%), loamy fine earth, the signs of podzolization in the soil profile is not found. Feature granulometric size distribution of the soil - a gradual increase in weight on the profile into Sandy Loam to Silty Clay and Clay, the dominant factions are either big Silt or Sand. Soils are characterized by a very acidic environment and high hydrolytic acidity. The soils are enriched in organic matter and humus profile characterized by prolixity. Group composition humus shows mobility, high degree of humification of organic substances to fulvic acids. Gross composition shows that the processes of soil formation on Mount, North Basegi aren’t leading to a distinctly different profile. Coefficients of geochemical accumulation, subsurface weathering, eluviation, oxidation calculated and helped define the features of the gross composition of soils. Character of distribution in profile and correlation of forms of iron help to diagnose physical processes of weathering and soil formation (burozemic pedogenesis et al.); signs Podzolization not revealed. Weathering and soil formation processes that occur with varying intensity, creating a diversity of soil cover and the spatial heterogeneity of soils, even within the same type. Thus, in the mountains of the Middle Urals brown forest soils form a number of subtypes: raw organic (900 m) - ferruginized (655 m) - metamorphosed (590 m) - clay-illuvial (577 m) - eluvial (565 m) - clay-illuvial (315 m).
VL  - 4
IS  - 3-1
ER  -

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Samofalova Iraida

Perm State Agricultural Academy, The Faculty of Soil Science, Agrochemistry, Ecology and Commodity research, Perm, Russia

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Samofalova Iraida. (2015). Genetic Characteristics of Brown Forest Soils on the Middle Urals. American Journal of Environmental Protection, 4(3-1), 148-156. https://doi.org/10.11648/j.ajep.s.2015040301.33

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ACS Style

Samofalova Iraida. Genetic Characteristics of Brown Forest Soils on the Middle Urals. Am. J. Environ. Prot. 2015, 4(3-1), 148-156. doi: 10.11648/j.ajep.s.2015040301.33

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Samofalova Iraida. Genetic Characteristics of Brown Forest Soils on the Middle Urals. Am J Environ Prot. 2015;4(3-1):148-156. doi: 10.11648/j.ajep.s.2015040301.33

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@article{10.11648/j.ajep.s.2015040301.33,
  author = {Samofalova Iraida},
  title = {Genetic Characteristics of Brown Forest Soils on the Middle Urals},
  journal = {American Journal of Environmental Protection},
  volume = {4},
  number = {3-1},
  pages = {148-156},
  doi = {10.11648/j.ajep.s.2015040301.33},
  url = {https://doi.org/10.11648/j.ajep.s.2015040301.33},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajep.s.2015040301.33},
  abstract = {Feature of mountain soil formation is that the soils on the mountain slopes are formed in different bioclimatic and orogeomorfological conditions. The purpose of research is to study genetic properties of the brown forest soils in the Middle Urals. Features of the morphological structure: truncated profile (35-75 cm), weakly expressed in the differentiation of the soil profile into individual Horizons, detritus (20-65%), loamy fine earth, the signs of podzolization in the soil profile is not found. Feature granulometric size distribution of the soil - a gradual increase in weight on the profile into Sandy Loam to Silty Clay and Clay, the dominant factions are either big Silt or Sand. Soils are characterized by a very acidic environment and high hydrolytic acidity. The soils are enriched in organic matter and humus profile characterized by prolixity. Group composition humus shows mobility, high degree of humification of organic substances to fulvic acids. Gross composition shows that the processes of soil formation on Mount, North Basegi aren’t leading to a distinctly different profile. Coefficients of geochemical accumulation, subsurface weathering, eluviation, oxidation calculated and helped define the features of the gross composition of soils. Character of distribution in profile and correlation of forms of iron help to diagnose physical processes of weathering and soil formation (burozemic pedogenesis et al.); signs Podzolization not revealed. Weathering and soil formation processes that occur with varying intensity, creating a diversity of soil cover and the spatial heterogeneity of soils, even within the same type. Thus, in the mountains of the Middle Urals brown forest soils form a number of subtypes: raw organic (900 m) - ferruginized (655 m) - metamorphosed (590 m) - clay-illuvial (577 m) - eluvial (565 m) - clay-illuvial (315 m).},
 year = {2015}
}

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TY  - JOUR
T1  - Genetic Characteristics of Brown Forest Soils on the Middle Urals
AU  - Samofalova Iraida
Y1  - 2015/06/25
PY  - 2015
N1  - https://doi.org/10.11648/j.ajep.s.2015040301.33
DO  - 10.11648/j.ajep.s.2015040301.33
T2  - American Journal of Environmental Protection
JF  - American Journal of Environmental Protection
JO  - American Journal of Environmental Protection
SP  - 148
EP  - 156
PB  - Science Publishing Group
SN  - 2328-5699
UR  - https://doi.org/10.11648/j.ajep.s.2015040301.33
AB  - Feature of mountain soil formation is that the soils on the mountain slopes are formed in different bioclimatic and orogeomorfological conditions. The purpose of research is to study genetic properties of the brown forest soils in the Middle Urals. Features of the morphological structure: truncated profile (35-75 cm), weakly expressed in the differentiation of the soil profile into individual Horizons, detritus (20-65%), loamy fine earth, the signs of podzolization in the soil profile is not found. Feature granulometric size distribution of the soil - a gradual increase in weight on the profile into Sandy Loam to Silty Clay and Clay, the dominant factions are either big Silt or Sand. Soils are characterized by a very acidic environment and high hydrolytic acidity. The soils are enriched in organic matter and humus profile characterized by prolixity. Group composition humus shows mobility, high degree of humification of organic substances to fulvic acids. Gross composition shows that the processes of soil formation on Mount, North Basegi aren’t leading to a distinctly different profile. Coefficients of geochemical accumulation, subsurface weathering, eluviation, oxidation calculated and helped define the features of the gross composition of soils. Character of distribution in profile and correlation of forms of iron help to diagnose physical processes of weathering and soil formation (burozemic pedogenesis et al.); signs Podzolization not revealed. Weathering and soil formation processes that occur with varying intensity, creating a diversity of soil cover and the spatial heterogeneity of soils, even within the same type. Thus, in the mountains of the Middle Urals brown forest soils form a number of subtypes: raw organic (900 m) - ferruginized (655 m) - metamorphosed (590 m) - clay-illuvial (577 m) - eluvial (565 m) - clay-illuvial (315 m).
VL  - 4
IS  - 3-1
ER  -

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