2022
DOI: 10.3390/geosciences12040156
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Multidecadal Land-Use Changes and Implications on Soil Protection in the Calore River Basin Landscape (Southern Italy)

Abstract: In Southern Italy, studies dealing with the analysis of multidecadal land-use changes at the basin scale are scarce. This is an important gap, considering the deep interrelationships between land-use changes, soil erosion, and river dynamics, and hazards at the basin scale and the proneness of Southern Italy to desertification. This study provides a contribution in filling this gap by analyzing the land-use changes occurring in an inner area of Southern Italy, i.e., the Calore River basin, between 1960 and 201… Show more

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Cited by 2 publications
(12 citation statements)
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“…Most of the land-use changes in the study area occurred between the 1960s and the 1990s, followed by a period of substantial stability. This likely led to a decrease in soil erosion and sediment supply to the rivers between 1960 and 1990 [42], which is confirmed by recent studies dealing with short-term river channel adjustments [4,5,43], followed by a phase of overall stability since the 1990s [42].…”
Section: Study Areasupporting
confidence: 58%
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“…Most of the land-use changes in the study area occurred between the 1960s and the 1990s, followed by a period of substantial stability. This likely led to a decrease in soil erosion and sediment supply to the rivers between 1960 and 1990 [42], which is confirmed by recent studies dealing with short-term river channel adjustments [4,5,43], followed by a phase of overall stability since the 1990s [42].…”
Section: Study Areasupporting
confidence: 58%
“…The land-use in the Calore River basin [42] is dominated by agricultural lands (64% of the total area) and, subordinately, by forests (23%). In the last 60 years, the studied basin experienced an increase in forested areas at the expense of agricultural lands.…”
Section: Study Areamentioning
confidence: 99%
“…This harmonization was possible only at the third level of the Corine land cover, due to the differences in scope, years, and methods of production between CNR-TC and CLC maps (Table 1). According to Magliulo et al [24,25], the differences in the responses of the LULC classes to soil-erosion processes, widely accepted in the literature ( [38,39], and references therein), were used as additional harmonization criteria. The harmonization also took into account the suggestion by Falcucci et al [40] to reduce the former number of classes and define a few new classes that represent markedly distinct LULC types.…”
Section: Data Source and Methodologymentioning
confidence: 99%
“…The results consisted of digital maps in which each polygon represented areas that experienced LULC changes or persistence. Each polygon, i.e., each LULC change or persistence, was classified according to Di Gennaro et al [37] and Magliulo et al [24,25] (Figure 3). Finally, the extension of each polygon was automatically calculated by means of the "Calculate Geometry" ArcGIS ® tool.…”
Section: Data Source and Methodologymentioning
confidence: 99%
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