Soil carbon pools in two natural grasslands of Serbian highlands

Grasslands are a major player in the global carbon cycle, although carbon stocks in grasslands are influenced by human activities and natural disturbances. The aim of this study is to determine differences in carbon stock on two test areas of grassland ecosystem in the highlands of Stara...

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Main Authors: Saljnikov Elmira, Lukić Sara, Miljković Predrag, Koković Nikola, Perović Veljko, Čakmak Dragan, Belanović-Simić Snežana
Format: Article
Language:srp
Published: Faculty of Forestry, Belgrade 2019-01-01
Series:Glasnik Šumarskog Fakulteta: Univerzitet u Beogradu
Subjects:
Online Access:http://www.doiserbia.nb.rs/img/doi/0353-4537/2019/0353-45371919233S.pdf
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author Saljnikov Elmira
Lukić Sara
Miljković Predrag
Koković Nikola
Perović Veljko
Čakmak Dragan
Belanović-Simić Snežana
author_facet Saljnikov Elmira
Lukić Sara
Miljković Predrag
Koković Nikola
Perović Veljko
Čakmak Dragan
Belanović-Simić Snežana
author_sort Saljnikov Elmira
collection DOAJ
description Grasslands are a major player in the global carbon cycle, although carbon stocks in grasslands are influenced by human activities and natural disturbances. The aim of this study is to determine differences in carbon stock on two test areas of grassland ecosystem in the highlands of Stara Planina and Zlatar Mountains (Serbia). The investigated sites are natural mountain grasslands of the same vegetation community (Agrostietum capillarisPavl. 1955) and soil type (Umbric Leptosol (Dystric) and Haplic Cambisol (Dystric)), but with different grazing intensity. Aboveground and belowground biomasses were measured in each sample plot, and soil was sampled at fixed depths of 0-10, 10-20 and 20-40 cm. The estimation of C stock and the rate of soil C accumulation were determined by the Tier 2 method IPCC (2003). Carbon mineralization potentials were determined via sequential incubation procedure in the laboratory conditions. According to the obtained results, the greater amount of precipitation on Mt. Stara Planina resulted in a greater accumulation of aboveground biomass, which was subjected to a greater decomposition in situ, thus showing a lower amount of PMC in vitro. In addition, potentially mineralizable carbon (PMC) among the sample plots from both sites indicates that the mineralization of soil organic matter was more influenced by the factors related to the soil characteristics, climatic conditions and grazing. [Project of the Serbian Ministry of Education, Science and Technological Development, Grant no. 043007: The Climate Change and Its Impact on the Environment - Monitoring, Adaptation and Mitigation]
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spelling doaj.art-827d8e9a5166488bb3002f5ebc39efdc2022-12-21T17:58:59ZsrpFaculty of Forestry, BelgradeGlasnik Šumarskog Fakulteta: Univerzitet u Beogradu0353-45372217-86002019-01-01201911923325210.2298/GSF1919233S0353-45371919233SSoil carbon pools in two natural grasslands of Serbian highlandsSaljnikov Elmira0Lukić Sara1Miljković Predrag2Koković Nikola3Perović Veljko4Čakmak Dragan5Belanović-Simić Snežana6Soil Science Institute, Belgrade, SerbiaUniversity of Belgrade, Faculty of Forestry, Belgrade, SerbiaUniversity of Belgrade, Faculty of Forestry, Belgrade, SerbiaSoil Science Institute, Belgrade, SerbiaUniversity of Belgrade, Institute for Biological Research “Sinisa Stankovic”, Belgrade, SerbiaUniversity of Belgrade, Institute for Biological Research “Sinisa Stankovic”, Belgrade, SerbiaUniversity of Belgrade, Faculty of ForestryGrasslands are a major player in the global carbon cycle, although carbon stocks in grasslands are influenced by human activities and natural disturbances. The aim of this study is to determine differences in carbon stock on two test areas of grassland ecosystem in the highlands of Stara Planina and Zlatar Mountains (Serbia). The investigated sites are natural mountain grasslands of the same vegetation community (Agrostietum capillarisPavl. 1955) and soil type (Umbric Leptosol (Dystric) and Haplic Cambisol (Dystric)), but with different grazing intensity. Aboveground and belowground biomasses were measured in each sample plot, and soil was sampled at fixed depths of 0-10, 10-20 and 20-40 cm. The estimation of C stock and the rate of soil C accumulation were determined by the Tier 2 method IPCC (2003). Carbon mineralization potentials were determined via sequential incubation procedure in the laboratory conditions. According to the obtained results, the greater amount of precipitation on Mt. Stara Planina resulted in a greater accumulation of aboveground biomass, which was subjected to a greater decomposition in situ, thus showing a lower amount of PMC in vitro. In addition, potentially mineralizable carbon (PMC) among the sample plots from both sites indicates that the mineralization of soil organic matter was more influenced by the factors related to the soil characteristics, climatic conditions and grazing. [Project of the Serbian Ministry of Education, Science and Technological Development, Grant no. 043007: The Climate Change and Its Impact on the Environment - Monitoring, Adaptation and Mitigation]http://www.doiserbia.nb.rs/img/doi/0353-4537/2019/0353-45371919233S.pdfgrasslandsbiomass carbon stocksoil carbon stockcarbon mineralizationpotentially mineralizable carbon
spellingShingle Saljnikov Elmira
Lukić Sara
Miljković Predrag
Koković Nikola
Perović Veljko
Čakmak Dragan
Belanović-Simić Snežana
Soil carbon pools in two natural grasslands of Serbian highlands
Glasnik Šumarskog Fakulteta: Univerzitet u Beogradu
grasslands
biomass carbon stock
soil carbon stock
carbon mineralization
potentially mineralizable carbon
title Soil carbon pools in two natural grasslands of Serbian highlands
title_full Soil carbon pools in two natural grasslands of Serbian highlands
title_fullStr Soil carbon pools in two natural grasslands of Serbian highlands
title_full_unstemmed Soil carbon pools in two natural grasslands of Serbian highlands
title_short Soil carbon pools in two natural grasslands of Serbian highlands
title_sort soil carbon pools in two natural grasslands of serbian highlands
topic grasslands
biomass carbon stock
soil carbon stock
carbon mineralization
potentially mineralizable carbon
url http://www.doiserbia.nb.rs/img/doi/0353-4537/2019/0353-45371919233S.pdf
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AT kokovicnikola soilcarbonpoolsintwonaturalgrasslandsofserbianhighlands
AT perovicveljko soilcarbonpoolsintwonaturalgrasslandsofserbianhighlands
AT cakmakdragan soilcarbonpoolsintwonaturalgrasslandsofserbianhighlands
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