This work investigated the role of land cover and land use change as a soil’s ability to store carbon and reduce carbon dioxide emission in a Mediterranean area. Using both historic records and land cover crop maps we estimated the effect of land cover change on the carbon stock from 1972 to 2008 in a natural reserve (Grotta di S. Ninfa) in the West of Sicily. Five paired sites in different soil types were selected and five land use classes (arable land, vineyard, olivegrove, gariga, eucalyptus afforestation) were analyzed. We studied the effect of land use on soil organic carbon (SOC) content in bulk soil and 1000-2000 m, 500-1000 m, 250-500 m, 63-250 m, 25-63 m and <25 m size fractions. Furthermore, laboratory incubation of th...
The increasing atmospheric CO2 concentration is a consequence of human activities leading to severe ...
The aim of this work was to quantify the soil organic C (SOC) stock in the top 30 cm of mineral soi...
This research aimed at testing the use of present and past climosequences to estimate soil organic c...
This work investigated the role of land cover and land use change as a soil\u2019s ability to store ...
This work investigated the role of land cover and land use change (LUC) as a soil ability to store c...
This work investigated the effects of land cover and land-use change (LUC) on the ability of a soil ...
Soil organic carbon (SOC) pool is the largest among the terrestrial pool and it plays a key role to ...
The knowledge about land management effects on soil capacity to store carbon is necessary to plannin...
In terrestrial biosphere, soil represents the largest organic carbon pool, and a small change of soi...
In the last decades, in Europe large agricultural areas have been abandoned. In absence of disturban...
In agro-ecosystems, land use change and the associated management practices exert a strong impact on...
The recent abandonment of marginal agricultural areas in the Mediterranean has caused an increase of...
The aim of this chapter was to quantify the soil organic carbon (SOC) stock in the top 30 cm of mine...
To evaluate the mitigation potential provided by the SOC pool, we investigated the impact of woody e...
Soils are the biggest carbon store in theworld (1500 Gt, e.g. 1.5 71021 g). The European Commission ...
The increasing atmospheric CO2 concentration is a consequence of human activities leading to severe ...
The aim of this work was to quantify the soil organic C (SOC) stock in the top 30 cm of mineral soi...
This research aimed at testing the use of present and past climosequences to estimate soil organic c...
This work investigated the role of land cover and land use change as a soil\u2019s ability to store ...
This work investigated the role of land cover and land use change (LUC) as a soil ability to store c...
This work investigated the effects of land cover and land-use change (LUC) on the ability of a soil ...
Soil organic carbon (SOC) pool is the largest among the terrestrial pool and it plays a key role to ...
The knowledge about land management effects on soil capacity to store carbon is necessary to plannin...
In terrestrial biosphere, soil represents the largest organic carbon pool, and a small change of soi...
In the last decades, in Europe large agricultural areas have been abandoned. In absence of disturban...
In agro-ecosystems, land use change and the associated management practices exert a strong impact on...
The recent abandonment of marginal agricultural areas in the Mediterranean has caused an increase of...
The aim of this chapter was to quantify the soil organic carbon (SOC) stock in the top 30 cm of mine...
To evaluate the mitigation potential provided by the SOC pool, we investigated the impact of woody e...
Soils are the biggest carbon store in theworld (1500 Gt, e.g. 1.5 71021 g). The European Commission ...
The increasing atmospheric CO2 concentration is a consequence of human activities leading to severe ...
The aim of this work was to quantify the soil organic C (SOC) stock in the top 30 cm of mineral soi...
This research aimed at testing the use of present and past climosequences to estimate soil organic c...