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dc.contributor.author
Céspedes Payret, Carlos
dc.contributor.author
Bazzoni, Bruno
dc.contributor.author
Gutiérrez, Ofelia
dc.contributor.author
Panario, Daniel
dc.date.available
2023-01-11T09:50:17Z
dc.date.issued
2017-03
dc.identifier.citation
Céspedes Payret, Carlos; Bazzoni, Bruno; Gutiérrez, Ofelia; Panario, Daniel; Soil Organic Carbon vs. Bulk Density Following Temperate Grassland Afforestation; Springer; Environmental Processes; 4; 1; 3-2017; 75-92
dc.identifier.issn
2198-7505
dc.identifier.uri
http://hdl.handle.net/11336/184236
dc.description.abstract
Afforestation is part of a worldwide strategy to mitigate CO2 emissions. However, afforestation in grassland soils may have the opposite effect by promoting the loss of native carbon. Potential effects of this land use change on the flow of organic carbon to and from the soil can be described through bulk density (Db). Nowadays the suitability of Db for this purpose is being questioned. In order to bring new elements to the discussion, we carried out a comparative study of soil in the western region of Uruguay. Based on the background information and our own data, collected for over a decade, we evaluated the fitness of Db as proxy soil organic carbon (SOC) stocks in grassland converted to tree afforestation. These data were also related to soil pH values. The sampling consisted of five plots afforested with Eucalyptus grandis paired with control plots under grassland. All samples were taken at depth (0–10 cm and 10–20 cm) except for Db samples (0–10 cm). In afforested sites, Db increased (1.62 vs 1.53 g/cm3; p ≤ 0.01) and SOC decreased (0–10 cm: 0.90 vs. 1.22%; p ≤ 0.08). Db values were not significantly correlated with SOC content. As with SOC, pH values decreased after afforestation at both depths (0–10 cm: 4.92 vs. 5.62; p ≤ 0.01; 10–20 cm: 4.76 vs. 5.54; p ≤ 0.01). The high acidity generated in soils following afforestation, is enough to affect the interaction between mineral and organic fractions and, with them, the original Db values. According to a previous study in the same location, there is a change in the predominance of different clay minerals in the topsoil (0–20 cm). This qualitative change in the mineral fraction can affect the ability of the soil to retain organic carbon, and not be reflected in the recorded Db values. The non-reciprocity recorded between Db and SOC values warns about the need for restriction of the generic use of Db in calculation of SOC stocks estimation. In view of these results, we present a discussion of possible causes that explain the disparity between Db values and SOC measurements.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Springer
dc.rights
info:eu-repo/semantics/openAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
BULK DENSITY
dc.subject
GRASSLAND AFFORESTATION
dc.subject
LAND USE CHANGE
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SOIL ACIDIFICATION
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SOIL ORGANIC CARBON
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URUGUAY
dc.subject.classification
Ciencias del Suelo
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Agricultura, Silvicultura y Pesca
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CIENCIAS AGRÍCOLAS
dc.title
Soil Organic Carbon vs. Bulk Density Following Temperate Grassland Afforestation
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2022-11-29T13:04:39Z
dc.journal.volume
4
dc.journal.number
1
dc.journal.pagination
75-92
dc.journal.pais
Países Bajos
dc.description.fil
Fil: Céspedes Payret, Carlos. Universidad de la República. Facultad de Ciencias; Uruguay
dc.description.fil
Fil: Bazzoni, Bruno. Universidad de la República. Facultad de Ciencias; Uruguay. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura. Universidad de Buenos Aires. Facultad de Agronomía. Instituto de Investigaciones Fisiológicas y Ecológicas Vinculadas a la Agricultura; Argentina
dc.description.fil
Fil: Gutiérrez, Ofelia. Universidad de la República. Facultad de Ciencias; Uruguay
dc.description.fil
Fil: Panario, Daniel. Universidad de la República. Facultad de Ciencias; Uruguay
dc.journal.title
Environmental Processes
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/http://link.springer.com/10.1007/s40710-016-0197-4
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1007/s40710-016-0197-4
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