Temperature and glucose effects on soil organic carbon: CO2 evolved and decomposition rate.

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dc.contributorCNPMS.
dc.creatorVASCONCELLOS, C. A.
dc.date2021-12-13T12:00:50Z
dc.date2021-12-13T12:00:50Z
dc.date1997-03-06
dc.date1994
dc.date.accessioned2026-07-07T05:25:08Z
dc.descriptionA study was conducted to determine the effect of glucose on C mineraliztion from soils with different origins at elevated temperature. Soils from Northern Europe showed higher mineralization rate than Brazilian soils for recent energy source at 35oC. At 15oC as incubation temperature, there ws no difference between soils. The addition of glucose tosoil accelerated the turnover of native organic C. That acceleration was higher at 35oC and in soils from temperate regions. Only the pH and total soil organic carbon had significant influence on CO2 mineralization parameters. No significance was found to C/N ratio and clay content.
dc.identifierPesquisa Agropecuária Brasileira, Brasília, v. 29, n. 7, p. 1129-1136, 1994.
dc.identifierhttp://www.alice.cnptia.embrapa.br/alice/handle/doc/474565
dc.identifier.urihttp://hdl.handle.net/123456789/490515
dc.languageeng
dc.rightsopenAccess
dc.subjectTemperatura elevada
dc.subjectFontes
dc.subjectElevated temperature
dc.subjectMineralization rate
dc.subjectEnergy source
dc.subjectIncubation
dc.subjectEnergia
dc.subjectIncubação
dc.subjectMineralização
dc.subjectSolo
dc.subjectsoil
dc.titleTemperature and glucose effects on soil organic carbon: CO2 evolved and decomposition rate.
dc.typeArtigo de periódico

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