Ecosystem carbon pools of coppice-originated oak forests at different development stages

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dc.contributor.authorMakineci, Ender
dc.contributor.authorÖzdemir, Emrah
dc.contributor.authorÇalışkan, Servet
dc.contributor.authorYılmaz, Ersel
dc.contributor.authorKumbaşlı, Meriç
dc.contributor.authorKeten, Akif
dc.contributor.authorYılmaz, Hatice
dc.date.accessioned2020-05-01T09:11:34Z
dc.date.available2020-05-01T09:11:34Z
dc.date.issued2015
dc.departmentDÜ, Ziraat Fakültesi, Bitki Koruma Bölümüen_US
dc.descriptionOzdemir, Emrah/0000-0001-5051-4753; BESKARDES, VEDAT/0000-0002-7404-6357; Yilmaz, Ersel/0000-0002-8671-7365en_US
dc.descriptionWOS: 000351134600010en_US
dc.description.abstractThe carbon (C) pools of aboveground tree components (leaf, stem, branch, and stem bark), ground cover, organic, and mineral soil were examined and compared with three stand development stages based on the mean tree diameters [diameter at breast height (dbh) in which small-diameter forests (SDF) = 0-8 cm, medium-diameter forests (MDF) = 8-20 cm, and large-diameter forests (LDF) = 20-36 cm] in pure coppice-originated oak stands located in the northwestern Turkey. In tree components, only the stem C concentration differed significantly among the development stages. The total C pools of the total tree biomass changed between 13 and 89 Mg ha(-1) from SDF to LDF. The C content of tree biomass was strongly correlated with dbh (R (2) = 0.83). The C contents of the ground cover differed significantly while the C contents in both organic soil layers were also markedly different and increased from SDF to LDF. The amount of C stored in the soil pedon was 84, 123, and 103 Mg ha(-1), and the total ecosystem (without belowground tree parts) C pools were 97, 177, and 192 Mg ha(-1), for the SDF, MDF, and LDF, respectively. Total ecosystem C content was significantly correlated (R (2) = 0.46) with dbh despite soil pedon C showed very weak correlation. The ratio between the C pool of the total aboveground tree components and total ecosystem C was 13 % in the SDF, 30 % in the MDF, and 46 % in the LDF. These results show that the soil was the main pool of C in the forests for all of the development stages.en_US
dc.description.sponsorshipScientific and Technological Research Council of Turkey (TUBITAK)Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK) [TOVAG-107O750]en_US
dc.description.sponsorshipWe thank to Prof. Dr. Dan Binkley from Department of Ecosystem Science and Sustainability and Natural Resource Ecology Laboratory, Colorado State University, USA, for his valuable suggestions on the manuscript. The authors are grateful to Istanbul Regional Forestry Directorate for their corroboration in the field. This work was supported by The Scientific and Technological Research Council of Turkey (TUBITAK), Project Number: TOVAG-107O750.en_US
dc.identifier.doi10.1007/s10342-014-0854-yen_US
dc.identifier.endpage333en_US
dc.identifier.issn1612-4669
dc.identifier.issn1612-4677
dc.identifier.issue2en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.startpage319en_US
dc.identifier.urihttps://doi.org/10.1007/s10342-014-0854-y
dc.identifier.urihttps://hdl.handle.net/20.500.12684/5665
dc.identifier.volume134en_US
dc.identifier.wosWOS:000351134600010en_US
dc.identifier.wosqualityQ1en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSpringeren_US
dc.relation.ispartofEuropean Journal Of Forest Researchen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectBiomassen_US
dc.subjectdbhen_US
dc.subjectGround coveren_US
dc.subjectMineral soilen_US
dc.subjectTree componentsen_US
dc.titleEcosystem carbon pools of coppice-originated oak forests at different development stagesen_US
dc.typeArticleen_US

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