dc.creatorMuñoz, C.
dc.creatorCruz, B.
dc.creatorRojo, F.
dc.creatorCampos, J.
dc.creatorCasanova, M.
dc.creatorDoetter, S.
dc.creatorBoeckx, P.
dc.creatorZagal, E.
dc.date.accessioned2018-12-20T14:17:33Z
dc.date.available2018-12-20T14:17:33Z
dc.date.created2018-12-20T14:17:33Z
dc.date.issued2016
dc.identifierJournal of Soil Science and Plant Nutrition, Volumen 16, Issue 2, 2018, Pages 461-476
dc.identifier07189516
dc.identifier10.4067/S0718-95162016005000039
dc.identifierhttps://repositorio.uchile.cl/handle/2250/155538
dc.description.abstract© 2016, Sociedad Chilena de la Ciencia del Suelo. All rights reserved.Global warming affects the carbon (C) pools in terrestrial ecosystems, accelerating biological processes that feed back into the phenomenon of climate change. Globally, grassland ecosystems accumulate large quantities of organic C into soils and are considered a corner stone for global warming mitigation. The aim of this study was to evaluate the temperature sensitivity of C decomposition in different soil aggregate fractions in grassland ecosystems across a north-south latitudinal gradient in Chile. Soil samples were collected from Mediterranean semi-arid (MSA; 32°31’ to 34°19’ south latitude), temperate semi-oceanic (TSO; 35°36’ to 36°27’ south latitude), temperate oceanic (TO; 40°36’ to 43°03’ south latitude) and subpolar semi-oceanic (SPSO; 43°57’ to 47°40’ south latitude) climate zones, and water-stable macroaggregates (250-2,000 µm) and free microaggregates (50-250 µm) were isolated. Two experiments were perfor
dc.languageen
dc.publisherSociedad Chilena de la Ciencia del Suelo
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile
dc.sourceJournal of Soil Science and Plant Nutrition
dc.subjectArrhenius equation
dc.subjectEnergy of activation
dc.subjectGrassland ecosystems
dc.subjectQ10
dc.subjectSoil fractionation
dc.titleTemperature sensitivity of carbon decomposition in soil aggregates along a climatic gradient
dc.typeArtículos de revistas


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