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Alteration process during the post-agricultural restoration of Luvisols of the temperate broad-leaved forest in Russia. / Kalinina, O.; Chertov, O.; Frolov, P.; Goryachkin, S.; Kuner, P.; Küper, J.; Kurganova, I.; Lopes de Gerenyu, V.; Lyuri, D.; Rusakov, A.; Kuzyakov, Y.; Giani, L.

в: Catena, Том 171, 01.12.2018, стр. 602-612.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Kalinina, O, Chertov, O, Frolov, P, Goryachkin, S, Kuner, P, Küper, J, Kurganova, I, Lopes de Gerenyu, V, Lyuri, D, Rusakov, A, Kuzyakov, Y & Giani, L 2018, 'Alteration process during the post-agricultural restoration of Luvisols of the temperate broad-leaved forest in Russia', Catena, Том. 171, стр. 602-612. https://doi.org/10.1016/j.catena.2018.08.004

APA

Kalinina, O., Chertov, O., Frolov, P., Goryachkin, S., Kuner, P., Küper, J., Kurganova, I., Lopes de Gerenyu, V., Lyuri, D., Rusakov, A., Kuzyakov, Y., & Giani, L. (2018). Alteration process during the post-agricultural restoration of Luvisols of the temperate broad-leaved forest in Russia. Catena, 171, 602-612. https://doi.org/10.1016/j.catena.2018.08.004

Vancouver

Kalinina O, Chertov O, Frolov P, Goryachkin S, Kuner P, Küper J и пр. Alteration process during the post-agricultural restoration of Luvisols of the temperate broad-leaved forest in Russia. Catena. 2018 Дек. 1;171:602-612. https://doi.org/10.1016/j.catena.2018.08.004

Author

Kalinina, O. ; Chertov, O. ; Frolov, P. ; Goryachkin, S. ; Kuner, P. ; Küper, J. ; Kurganova, I. ; Lopes de Gerenyu, V. ; Lyuri, D. ; Rusakov, A. ; Kuzyakov, Y. ; Giani, L. / Alteration process during the post-agricultural restoration of Luvisols of the temperate broad-leaved forest in Russia. в: Catena. 2018 ; Том 171. стр. 602-612.

BibTeX

@article{42d2e11ca9f34389aea22645256193e8,
title = "Alteration process during the post-agricultural restoration of Luvisols of the temperate broad-leaved forest in Russia",
abstract = "This chronosequential study focuses on the vegetation succession, Luvisol pedogenesis, and long-term carbon dynamics during post-agricultural restoration in the temperate broad-leaved forest of European Russia. The study comprises three chronosequences of 37 years (North), 120 years (Middle), and 42 years (South) to cover climatic differences within the study area. The sites of each catena were mostly comparable in terms of climate, soil texture, and land history, but the duration of agricultural abandonment differed between sites. Plant succession developed via a birch forest or a pear-ash woodland to a birch-oak forest with Aegop{\'o}dium podagr{\'a}ria after 120 years, which indicates the plant association is near to a climax oak forest. Former homogenous plow horizons formed a new morphological stratification similar to natural Luvisols, due to the formation of a well rooted Ah horizon and an O horizon of mull; a change in soil structure from coarse blocky to granular; and decreasing bulk densities. However, plow features were identified even after 120 years of Luvisols restoration. During restoration, the former plow horizons showed minor changes of pH 5.4–5.6 (CaCl2). However, a slightly increased pH value within the newly developed Ah and O horizons induced a new pH stratification of the former plow horizon, approaching the natural soils. Compared to the former plow horizons below, soil organic carbon (SOC) and plant available nutrients (P, K) enrichment was observed within the newly developed Ah horizons. The SOC stocks of the 5 cm mineral topsoil increased from 0.8 to 1.7 kg m−2 (North), from 1.3 to 1.7 kg m−2 (Middle), and from 1.4 to 2.3 kg m−2 (South) during restoration. The surface organic layers showed SOC stocks of 0.1–0.2 kg m−2. However, the levels of the near-natural soils were not reached after 37 years (North) and 42 years (South) of restoration. The model predicted a recovery time of about 150 years to achieve a comparatively steady state. A negative effect of mowing was observed for the modelled SOC accumulation. Despite all these alterations, the study showed no full restoration for many parameters within the chronosequential timescale of 120 years.",
keywords = "Carbon stocks, Chronosequence, Luvisol, Post-agricultural restoration, Russia, ARABLE LAND, NITROGEN MINERALIZATION, GLOBAL CHANGE, MATTER DYNAMICS, LAND-USE CHANGE, SELF-RESTORATION, EUROPEAN RUSSIA, SOIL ORGANIC-CARBON, SOVIET CROPLAND ABANDONMENT, AGRICULTURAL SOILS",
author = "O. Kalinina and O. Chertov and P. Frolov and S. Goryachkin and P. Kuner and J. K{\"u}per and I. Kurganova and {Lopes de Gerenyu}, V. and D. Lyuri and A. Rusakov and Y. Kuzyakov and L. Giani",
year = "2018",
month = dec,
day = "1",
doi = "10.1016/j.catena.2018.08.004",
language = "English",
volume = "171",
pages = "602--612",
journal = "Catena",
issn = "0341-8162",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Alteration process during the post-agricultural restoration of Luvisols of the temperate broad-leaved forest in Russia

AU - Kalinina, O.

AU - Chertov, O.

AU - Frolov, P.

AU - Goryachkin, S.

AU - Kuner, P.

AU - Küper, J.

AU - Kurganova, I.

AU - Lopes de Gerenyu, V.

AU - Lyuri, D.

AU - Rusakov, A.

AU - Kuzyakov, Y.

AU - Giani, L.

PY - 2018/12/1

Y1 - 2018/12/1

N2 - This chronosequential study focuses on the vegetation succession, Luvisol pedogenesis, and long-term carbon dynamics during post-agricultural restoration in the temperate broad-leaved forest of European Russia. The study comprises three chronosequences of 37 years (North), 120 years (Middle), and 42 years (South) to cover climatic differences within the study area. The sites of each catena were mostly comparable in terms of climate, soil texture, and land history, but the duration of agricultural abandonment differed between sites. Plant succession developed via a birch forest or a pear-ash woodland to a birch-oak forest with Aegopódium podagrária after 120 years, which indicates the plant association is near to a climax oak forest. Former homogenous plow horizons formed a new morphological stratification similar to natural Luvisols, due to the formation of a well rooted Ah horizon and an O horizon of mull; a change in soil structure from coarse blocky to granular; and decreasing bulk densities. However, plow features were identified even after 120 years of Luvisols restoration. During restoration, the former plow horizons showed minor changes of pH 5.4–5.6 (CaCl2). However, a slightly increased pH value within the newly developed Ah and O horizons induced a new pH stratification of the former plow horizon, approaching the natural soils. Compared to the former plow horizons below, soil organic carbon (SOC) and plant available nutrients (P, K) enrichment was observed within the newly developed Ah horizons. The SOC stocks of the 5 cm mineral topsoil increased from 0.8 to 1.7 kg m−2 (North), from 1.3 to 1.7 kg m−2 (Middle), and from 1.4 to 2.3 kg m−2 (South) during restoration. The surface organic layers showed SOC stocks of 0.1–0.2 kg m−2. However, the levels of the near-natural soils were not reached after 37 years (North) and 42 years (South) of restoration. The model predicted a recovery time of about 150 years to achieve a comparatively steady state. A negative effect of mowing was observed for the modelled SOC accumulation. Despite all these alterations, the study showed no full restoration for many parameters within the chronosequential timescale of 120 years.

AB - This chronosequential study focuses on the vegetation succession, Luvisol pedogenesis, and long-term carbon dynamics during post-agricultural restoration in the temperate broad-leaved forest of European Russia. The study comprises three chronosequences of 37 years (North), 120 years (Middle), and 42 years (South) to cover climatic differences within the study area. The sites of each catena were mostly comparable in terms of climate, soil texture, and land history, but the duration of agricultural abandonment differed between sites. Plant succession developed via a birch forest or a pear-ash woodland to a birch-oak forest with Aegopódium podagrária after 120 years, which indicates the plant association is near to a climax oak forest. Former homogenous plow horizons formed a new morphological stratification similar to natural Luvisols, due to the formation of a well rooted Ah horizon and an O horizon of mull; a change in soil structure from coarse blocky to granular; and decreasing bulk densities. However, plow features were identified even after 120 years of Luvisols restoration. During restoration, the former plow horizons showed minor changes of pH 5.4–5.6 (CaCl2). However, a slightly increased pH value within the newly developed Ah and O horizons induced a new pH stratification of the former plow horizon, approaching the natural soils. Compared to the former plow horizons below, soil organic carbon (SOC) and plant available nutrients (P, K) enrichment was observed within the newly developed Ah horizons. The SOC stocks of the 5 cm mineral topsoil increased from 0.8 to 1.7 kg m−2 (North), from 1.3 to 1.7 kg m−2 (Middle), and from 1.4 to 2.3 kg m−2 (South) during restoration. The surface organic layers showed SOC stocks of 0.1–0.2 kg m−2. However, the levels of the near-natural soils were not reached after 37 years (North) and 42 years (South) of restoration. The model predicted a recovery time of about 150 years to achieve a comparatively steady state. A negative effect of mowing was observed for the modelled SOC accumulation. Despite all these alterations, the study showed no full restoration for many parameters within the chronosequential timescale of 120 years.

KW - Carbon stocks

KW - Chronosequence

KW - Luvisol

KW - Post-agricultural restoration

KW - Russia

KW - ARABLE LAND

KW - NITROGEN MINERALIZATION

KW - GLOBAL CHANGE

KW - MATTER DYNAMICS

KW - LAND-USE CHANGE

KW - SELF-RESTORATION

KW - EUROPEAN RUSSIA

KW - SOIL ORGANIC-CARBON

KW - SOVIET CROPLAND ABANDONMENT

KW - AGRICULTURAL SOILS

UR - http://www.scopus.com/inward/record.url?scp=85051396523&partnerID=8YFLogxK

U2 - 10.1016/j.catena.2018.08.004

DO - 10.1016/j.catena.2018.08.004

M3 - Article

AN - SCOPUS:85051396523

VL - 171

SP - 602

EP - 612

JO - Catena

JF - Catena

SN - 0341-8162

ER -

ID: 35466928