Data di Pubblicazione:
2010
Citazione:
Soil degradation by land use change in an agropastoral area in Sardinia (Italy) / Zucca, Claudio; Canu, A; Previtali, F.. - In: CATENA. - ISSN 0341-8162. - 83:(2010), pp. 46-54. [10.1016/j.catena.2010.07.003]
Abstract:
In recent decades the clearing of Mediterranean maquis along with the creation of new pastures has been a
major factor of land degradation in Sardinia (Italy). This was due to an inadequate implementation of
agricultural policies. Consequently, tillage and water erosion intensified over a wide area. The present work
assesses the impacts of land use change on soil properties in a representative area of central-eastern Sardinia.
Paired forest and pasture sampling sites were selected in relation to present land use, land suitability, and
land use history. Different soil properties were considered: physical (sand, silt, clay, soil thickness, bulk
density, and penetration resistance), chemical (pH, OC, N, C/N, Ca, Mg, Na, K, CEC, and BS), biological (BQI),
and micromorphological (microporosity and microstructure). The comparison of forest and pasture soils
showed a significant soil loss (in terms of soil thickness, −22%), and a clear decrease in organic carbon
storage (−64% on average). An increase in bulk density (+44%) and a change in microporosity and its
vertical distribution were also observed, respectively by field measurements and micromorphological
quantification on digital images.
major factor of land degradation in Sardinia (Italy). This was due to an inadequate implementation of
agricultural policies. Consequently, tillage and water erosion intensified over a wide area. The present work
assesses the impacts of land use change on soil properties in a representative area of central-eastern Sardinia.
Paired forest and pasture sampling sites were selected in relation to present land use, land suitability, and
land use history. Different soil properties were considered: physical (sand, silt, clay, soil thickness, bulk
density, and penetration resistance), chemical (pH, OC, N, C/N, Ca, Mg, Na, K, CEC, and BS), biological (BQI),
and micromorphological (microporosity and microstructure). The comparison of forest and pasture soils
showed a significant soil loss (in terms of soil thickness, −22%), and a clear decrease in organic carbon
storage (−64% on average). An increase in bulk density (+44%) and a change in microporosity and its
vertical distribution were also observed, respectively by field measurements and micromorphological
quantification on digital images.
Tipologia CRIS:
1.1 Articolo in rivista
Elenco autori:
Zucca, Claudio; Canu, A; Previtali, F.
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