Please use this identifier to cite or link to this item: https://open.uns.ac.rs/handle/123456789/4318
DC FieldValueLanguage
dc.contributor.authorĆirić, Vladimiren
dc.contributor.authorBelić, Milivojen
dc.contributor.authorNešić, Ljiljanaen
dc.contributor.authorSrđan, Šeremešićen
dc.contributor.authorPejić, Borivojen
dc.contributor.authorBezdan, Atilaen
dc.contributor.authorManojlović, Miaen
dc.date.accessioned2019-09-23T10:33:24Z-
dc.date.available2019-09-23T10:33:24Z-
dc.date.issued2016-12-01en
dc.identifier.issn03650340en
dc.identifier.urihttps://open.uns.ac.rs/handle/123456789/4318-
dc.description.abstract© 2016 Informa UK Limited, trading as Taylor & Francis Group. Soil organic carbon (SOC) has a high impact on the sustainability of ecosystems, global environmental processes, soil quality and agriculture. Long-term tillage usually leads to SOC depletion. The purpose of this study was to determine the impact of different land uses on water extractable organic carbon (WEOC) fractions and to evaluate the interaction between the WEOC fractions and other soil properties. Using an extraction procedure at 20°C and 80°C, two fractions were obtained: a cold water extractable organic carbon (CWEOC) and a hot water extractable organic carbon (HWEOC). The results suggest that there is a significant impact from different land uses on WEOC. A lower relative contribution of WEOC in SOC and a lower concentration of labile WEOC fractions are contained in arable soil compared to forestlands. Chernozem soil was characterized by a lower relative contribution of WEOC to the SOC and thus higher SOC stability in contrast to Solonetz and Vertisol soils. Both CWEOC and HWEOC are highly associated with SOC in the silt and clay fraction (<53 µm) and were slightly associated with SOC in the macroaggregate classes. The WEOC fractions were highly and positively correlated with the SOC and mean weight diameter.en
dc.relation.ispartofArchives of Agronomy and Soil Scienceen
dc.titleThe sensitivity of water extractable soil organic carbon fractions to land use in three soil typesen
dc.typeJournal/Magazine Articleen
dc.identifier.doi10.1080/03650340.2016.1165345en
dc.identifier.scopus2-s2.0-84961927050en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/84961927050en
dc.relation.lastpage1664en
dc.relation.firstpage1654en
dc.relation.issue12en
dc.relation.volume62en
item.fulltextNo Fulltext-
item.grantfulltextnone-
crisitem.author.deptPoljoprivredni fakultet, Departman za ratarstvo i povrtarstvo-
crisitem.author.deptPoljoprivredni fakultet, Departman za ratarstvo i povrtarstvo-
crisitem.author.deptPoljoprivredni fakultet, Departman za ratarstvo i povrtarstvo-
crisitem.author.deptPoljoprivredni fakultet, Departman za uređenje voda-
crisitem.author.orcid0000-0003-4467-9601-
crisitem.author.orcid--
crisitem.author.orcid0000-0003-3713-3002-
crisitem.author.parentorgPoljoprivredni fakultet-
crisitem.author.parentorgPoljoprivredni fakultet-
crisitem.author.parentorgPoljoprivredni fakultet-
crisitem.author.parentorgPoljoprivredni fakultet-
Appears in Collections:POLJF Publikacije/Publications
Show simple item record

SCOPUSTM   
Citations

21
checked on May 3, 2024

Page view(s)

20
Last Week
4
Last month
0
checked on May 10, 2024

Google ScholarTM

Check

Altmetric


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.