dc.creatorKlein, Daniel
dc.creatorFuentes Espoz, Juan
dc.creatorSchmidt, Andreas
dc.creatorSchmidt Van Marle, Harald
dc.creatorSchulte, Andreas
dc.date2010-01-27T16:19:59Z
dc.date2018-10-23T16:00:38Z
dc.date2010-01-27T16:19:59Z
dc.date2018-10-23T16:00:38Z
dc.date2010-01-27T16:19:59Z
dc.date2008-05-30
dc.date.accessioned2020-09-21T15:29:09Z
dc.date.available2020-09-21T15:29:09Z
dc.identifierFOREST ECOLOGY AND MANAGEMENT Volume: 255 Issue: 10 Pages: 3549-3555 Published: MAY 30 2008
dc.identifier0378-1127
dc.identifier10.1016/j.foreco.2008.03.002
dc.identifierhttp://www.repositorio.uchile.cl/handle/2250/120355
dc.identifierhttps://bibliotecadigital.infor.cl/handle/20.500.12220/26127
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3171693
dc.descriptionThis study evaluates the effect of silvicultural and exploitative interventions on soil organic carbon (SOC) in Chilean Lenga (Nothofagus pumilio (Poepp et Endl.) Krasser) forests in south Patagonia. We analyzed SOC and the organic soil horizons in five stands at different stages of development: intact native forest (NI); a 3-year-old shelterwood stand (S3); an 8-year-old shelterwood stand (S8); a 14-year-old stand that was initially treated with shelterwood and subsequently final cut (10 years after the first intervention) (S14), and a 25-year-old stand subject to a exploitative intervention (E25). The SOC under the forest stands, down to a depth of 50 cm(including the Oi horizon), was 60, 55, 71, 85, and 67 Mg ha(-1) for the NI, S3, S8, S14, and E25 forest stands, respectively. A significant decrease in SOC occurred 3 years after an intensive shelterwood cut (S3), particularly in the first 5 cm of the mineral soil. Slightly higher carbon contents were observed in the upper horizons of the mineral soil in both the S8 and S14 stands. Consequently, the applied shelterwood system appears to generate only short-term losses of SOC in the Lenga forest. Soil organic carbon increased over the medium term but decreased to the level observed in intact native forests over the long term. Regeneration, which influences stand microclimate (a factor in SOC storage) and provides an important source of organic soil material, was identified as one of the most important factors influencing SOC.
dc.languageen
dc.publisherELSEVIER
dc.subjectTIERRA-DEL-FUEGO
dc.titleSoil organic C as affected by silvicultural and exploitative interventions in Nothofagus pumilio forests of the Chilean Patagonia
dc.typeArtículo de revista


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