Please use this identifier to cite or link to this item: http://earsiv.odu.edu.tr:8080/xmlui/handle/11489/4345
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dc.contributor.authorAskin, Tayfun-
dc.contributor.authorKizilkaya, Ridvan-
dc.date.accessioned2024-03-15T08:44:33Z-
dc.date.available2024-03-15T08:44:33Z-
dc.date.issued2009-
dc.identifier.citationAskin, T., Kizilkaya, R. (2009). SOIL BASAL RESPIRATION AND DEHYDROGENASE ACTIVITY OF AGGREGATES: A STUDY IN A TOPOSEQUENCE OF PASTURE SOILS. Zemdirbyste, 96(1), 98-112en_US
dc.identifier.issn1392-3196-
dc.identifier.urihttps://www.webofscience.com/wos/woscc/full-record/WOS:000271523500007-
dc.identifier.urihttp://earsiv.odu.edu.tr:8080/xmlui/handle/11489/4345-
dc.descriptionWoS Categories: Agriculture, Multidisciplinaryen_US
dc.descriptionWeb of Science Index: Science Citation Index Expanded (SCI-EXPANDED)en_US
dc.descriptionResearch Areas: Agricultureen_US
dc.description.abstractThe objective of this study was to determine changes in soil basal respiration (BR) and dehydrogenase activity (DHA) in soil aggregates along a pasture slope. Soil samples from 0-50 mm depth were taken from three landscape positions (crest, midslope and footslope) of a pasture in Samsun, Turkey. For each landscape position, soil aggregates were separated into eight aggregate size classes using a dry sieving method and then microbiological properties and organic carbon content (C(org)) were analysed. At all positions, the contents of macroaggregates (especially 841-1190 pm and 1190-1680 mu m) were higher than microaggregates. The contents of C(org) varied between 0.65-2.08%. The highest C(org) contents were found in footslope positions, and the lowest in midslope. All microbiological properties were higher at footslope position than at the other positions. Generally, BR and DHA were higher in microaggregates < 250 mu m, in macroaggregates of 250-420, 420-841, 841-1190 pm than in the other aggregate size classes at all positions, whereas C(org):C(mic) BR:C(mic) and DHA:C(mic) ratios were higher in macroaggregates of 1190-1680, 1680-2380, 2380-4760 mu m than the other macro- and microaggregate size. Consequently, macroaggregates had relatively more C(org) than the microaggregates, even if the absolute values of BR and DHA were the lower.en_US
dc.language.isoengen_US
dc.publisherLITHUANIAN INST AGRICULTURE-KEDAINIU Ren_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectpasture, soil aggregates, microbial biomass carbon, soil basal respiration, organic carbon, landscape positionen_US
dc.subjectMICROBIAL BIOMASS CARBON, ORGANIC-MATTER, STRUCTURAL STABILITY, METABOLIC QUOTIENT, CULTIVATED SOILS, ARABLE SOILS, MECHANISMS, NITROGEN, SYSTEMS, FUNGALen_US
dc.titleSOIL BASAL RESPIRATION AND DEHYDROGENASE ACTIVITY OF AGGREGATES: A STUDY IN A TOPOSEQUENCE OF PASTURE SOILSen_US
dc.typearticleen_US
dc.relation.journalZEMDIRBYSTE-AGRICULTUREen_US
dc.contributor.departmentOrdu Üniversitesien_US
dc.contributor.authorID0000-0001-9352-2710en_US
dc.contributor.authorID0000-0001-7475-9851en_US
dc.identifier.volume96en_US
dc.identifier.issue1en_US
dc.identifier.startpage98en_US
dc.identifier.endpage112en_US
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