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Humus accumulation and humification during soil development in post-mining soil. / Abakumov, Evgeny; Frouz, Jan.

Soil Biota and Ecosystem Development in Post Mining Sites. Taylor & Francis, 2013. p. 19-37.

Research output: Chapter in Book/Report/Conference proceeding › Chapter › Research › peer-review

Harvard

Abakumov, E & Frouz, J 2013, Humus accumulation and humification during soil development in post-mining soil. in Soil Biota and Ecosystem Development in Post Mining Sites. Taylor & Francis, pp. 19-37. https://doi.org/10.1201/b15502

APA

Abakumov, E., & Frouz, J. (2013). Humus accumulation and humification during soil development in post-mining soil. In Soil Biota and Ecosystem Development in Post Mining Sites (pp. 19-37). Taylor & Francis. https://doi.org/10.1201/b15502

Vancouver

Abakumov E, Frouz J. Humus accumulation and humification during soil development in post-mining soil. In Soil Biota and Ecosystem Development in Post Mining Sites. Taylor & Francis. 2013. p. 19-37 https://doi.org/10.1201/b15502

Author

Abakumov, Evgeny ; Frouz, Jan. / Humus accumulation and humification during soil development in post-mining soil. Soil Biota and Ecosystem Development in Post Mining Sites. Taylor & Francis, 2013. pp. 19-37

BibTeX

@inbook{858bf812406a4411a0ed9e76aae1e73a,
title = "Humus accumulation and humification during soil development in post-mining soil",
abstract = "Soil formation is a result of an interaction of five factors: climate, biota, relief, parent material and time (Dokuchaev 1949). Accumulation of organic matter and its downward migration in the soil profile play major roles in soil formation (Abakumov 2008, Cerli et al. 2008). Accumulation of organic matter leads to formation of an organic layer and affects many soil properties such as water holding capacity, C or N content, soil biota, etc. The humification process involves the main agents of soil weathering, chelatization and complexation of soil mineral compounds, and migration and translocation of organo-mineral compounds. The quality of organic matter (Kononova 1966, Ponomareva and Plotnikova 1980, Andreux 1996) and the soil biota (Ponomareva and Plotnikova 1980, Emmer and Sevink 1994, Androkhanov et al. 2000, Abakumov 2008) determine soil formation.",
keywords = "почвы, биота, горные разработки",
author = "Evgeny Abakumov and Jan Frouz",
year = "2013",
month = jan,
day = "1",
doi = "10.1201/b15502",
language = "English",
isbn = "9781466599314",
pages = "19--37",
booktitle = "Soil Biota and Ecosystem Development in Post Mining Sites",
publisher = "Taylor & Francis",
address = "United Kingdom",

}

RIS

TY - CHAP

T1 - Humus accumulation and humification during soil development in post-mining soil

AU - Abakumov, Evgeny

AU - Frouz, Jan

PY - 2013/1/1

Y1 - 2013/1/1

N2 - Soil formation is a result of an interaction of five factors: climate, biota, relief, parent material and time (Dokuchaev 1949). Accumulation of organic matter and its downward migration in the soil profile play major roles in soil formation (Abakumov 2008, Cerli et al. 2008). Accumulation of organic matter leads to formation of an organic layer and affects many soil properties such as water holding capacity, C or N content, soil biota, etc. The humification process involves the main agents of soil weathering, chelatization and complexation of soil mineral compounds, and migration and translocation of organo-mineral compounds. The quality of organic matter (Kononova 1966, Ponomareva and Plotnikova 1980, Andreux 1996) and the soil biota (Ponomareva and Plotnikova 1980, Emmer and Sevink 1994, Androkhanov et al. 2000, Abakumov 2008) determine soil formation.

AB - Soil formation is a result of an interaction of five factors: climate, biota, relief, parent material and time (Dokuchaev 1949). Accumulation of organic matter and its downward migration in the soil profile play major roles in soil formation (Abakumov 2008, Cerli et al. 2008). Accumulation of organic matter leads to formation of an organic layer and affects many soil properties such as water holding capacity, C or N content, soil biota, etc. The humification process involves the main agents of soil weathering, chelatization and complexation of soil mineral compounds, and migration and translocation of organo-mineral compounds. The quality of organic matter (Kononova 1966, Ponomareva and Plotnikova 1980, Andreux 1996) and the soil biota (Ponomareva and Plotnikova 1980, Emmer and Sevink 1994, Androkhanov et al. 2000, Abakumov 2008) determine soil formation.

KW - почвы

KW - биота

KW - горные разработки

UR - http://www.scopus.com/inward/record.url?scp=84976262642&partnerID=8YFLogxK

U2 - 10.1201/b15502

DO - 10.1201/b15502

M3 - Chapter

SN - 9781466599314

SP - 19

EP - 37

BT - Soil Biota and Ecosystem Development in Post Mining Sites

PB - Taylor & Francis

ER -

ID: 4634457