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Labile fractions of soil organic carbon in mollisols from different climatic regions
dc.creator | Saljnikov, Elmira | |
dc.creator | Cakmak, Dragan | |
dc.creator | Kostić Kravljanac, Ljiljana | |
dc.creator | Maksimović, Srboljub | |
dc.date.accessioned | 2022-04-05T14:20:19Z | |
dc.date.available | 2022-04-05T14:20:19Z | |
dc.date.issued | 2009 | |
dc.identifier.issn | 0002-1857 | |
dc.identifier.uri | http://rimsi.imsi.bg.ac.rs/handle/123456789/326 | |
dc.description.abstract | Characterization of Labile Fractions of Soil Organic Carbon in Mollisols from different climatic regions. The research studied the potential mineralization and characterization of labile SOM of different types of Mollisols: Hapludolls, Argiudolls, Calciustolls, and Haplustolls. Labile C fractions distributed oppositely than total SOC and were the greatest in Calciustolls and the lowest in Hapludolls. The amount of soil microbial biomass C (MBC) was significantly higher in dry than in wet regions. The highest amount of light fraction C was in dry-thermic followed by dry-frigid, and the least amount was in wet regions. Dry regions were able to retain a higher level of labile C than the moist regions, due to a slower annual decomposition rate. | en |
dc.publisher | Pisa Univ Press, Pisa | |
dc.rights | restrictedAccess | |
dc.source | Agrochimica | |
dc.subject | temperature | en |
dc.subject | mollisols | en |
dc.subject | moisture | en |
dc.subject | Labile organic matter | en |
dc.title | Labile fractions of soil organic carbon in mollisols from different climatic regions | en |
dc.type | article | |
dc.rights.license | ARR | |
dc.citation.epage | 385 | |
dc.citation.issue | 6 | |
dc.citation.other | 53(6): 376-385 | |
dc.citation.rank | M23 | |
dc.citation.spage | 376 | |
dc.citation.volume | 53 | |
dc.identifier.rcub | https://hdl.handle.net/21.15107/rcub_rimsi_326 | |
dc.identifier.wos | 000274505800003 | |
dc.type.version | publishedVersion |
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