Soil carbon sequestration of mollisols and oxisols under grassland and tree plantations in South America a review

Our objective was to determine how biophysical drivers impact on C sequestration and dynamics in Mollisols and Oxisols under grassland of South-America. We performed a literature review to obtain data on soil C stocks in grasslands and tree plantations on Mollisols and Oxisols and combined it with i...

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Detalles Bibliográficos
Autor principal: Berhongaray, Gonzalo
Otros Autores: Alvarez, Roberto
Formato: Artículo
Lenguaje:Inglés
Materias:
Acceso en línea:http://ri.agro.uba.ar/files/intranet/articulo/2019berhongaray.pdf
LINK AL EDITOR
Aporte de:Registro referencial: Solicitar el recurso aquí
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024 |a 10.1016/j.geodrs.2019.e00226 
040 |a AR-BaUFA 
100 1 |9 32180  |a Berhongaray, Gonzalo  |u CONICET. Buenos Aires, Argentina.  |u Universidad Nacional del Litoral. Facultad de Ciencias Agrarias. Santa Fe, Argentina. 
245 0 0 |a Soil carbon sequestration of mollisols and oxisols under grassland and tree plantations in South America  |b a review 
520 |a Our objective was to determine how biophysical drivers impact on C sequestration and dynamics in Mollisols and Oxisols under grassland of South-America. We performed a literature review to obtain data on soil C stocks in grasslands and tree plantations on Mollisols and Oxisols and combined it with information from a local soil survey. A simple estimate of the C retention efficiency (CRE) was calculated as the ratio between soil C pool size data and modeled C inputs. Although soil C inputs were higher in tree plantations than in grasslands, this only translated to higher soil C stocks in temperate climates. The CRE was generally much lower in tree plantations as compared to grasslands, and this difference was strongest in tropical sites The CRE was much higher in the subsoil than in the topsoil, probably associated with a more effective physico-chemical protection of soil C by minerals. Our analysis suggests that a combination of trees and grasses in silvopastoral systemmight be a solution for soil C sequestration in tropical soils. 
653 |a SOIL ORGANIC MATTER 
653 |a CARBON TURNOVER 
653 |a VERTICAL DISTRIBUTION 
653 |a CARBON RETENTION EFFICIENCY 
653 |a TEMPERATE 
653 |a TROPICAL 
653 |a MOLLISOLS 
653 |a OXISOLS 
700 1 |9 7830  |a Alvarez, Roberto  |u CONICET. Buenos Aires, Argentina.  |u Universidad de Buenos Aires. Facultad de Agronomía. Buenos Aires, Argentina. 
773 |t Geoderma Regional  |g vol.18 (2019), e00226, 8 p., tbls., grafs., mapas 
856 |f 2019berhongaray  |i en reservorio  |q application/pdf  |u http://ri.agro.uba.ar/files/intranet/articulo/2019berhongaray.pdf  |x ARTI201908 
856 |z LINK AL EDITOR  |u http://www.elsevier.com 
942 |c ARTICULO 
942 |c ENLINEA 
976 |a AAG