TY - JOUR
T1 - Predicting soil loss on moderate slopes using an empirical model for sediment concentration.
AU - Bagarello, V.
AU - Di Stefano, C.
AU - Ferro, V.
AU - Kinnell, Peter
AU - Pampalone, V.
AU - Porto, P.
AU - Todisco, F.
PY - 2011
Y1 - 2011
N2 - The objective of this investigation was to estimate event soilloss per unit area from bare plots in central and southern Italy using an empiricalmodel for sedimentconcentration. The analysis was developed using data collected on bare plots differing in length (11â¿¿44 m) and slope (10â¿¿26%) at three Italian stations (Masse, Umbria; Caratozzolo, Calabria; Sparacia, Sicily). At first, an analysis was carried out, using the experimental data collected at Sparacia, to establish a relationship between sedimentconcentration and hydrological variables, such as runoff, rainfall amount and single storm erosion index. Then, an empiricalmodel to estimate plot soilloss as a function of rainfall amount, single storm erosion index, runoff amount, and slope length was developed. Finally, using the complete data set (Masse, Caratozzolo, Sparacia), the model was extended to include soil erodibility and slope steepness effects on plot soilloss.
AB - The objective of this investigation was to estimate event soilloss per unit area from bare plots in central and southern Italy using an empiricalmodel for sedimentconcentration. The analysis was developed using data collected on bare plots differing in length (11â¿¿44 m) and slope (10â¿¿26%) at three Italian stations (Masse, Umbria; Caratozzolo, Calabria; Sparacia, Sicily). At first, an analysis was carried out, using the experimental data collected at Sparacia, to establish a relationship between sedimentconcentration and hydrological variables, such as runoff, rainfall amount and single storm erosion index. Then, an empiricalmodel to estimate plot soilloss as a function of rainfall amount, single storm erosion index, runoff amount, and slope length was developed. Finally, using the complete data set (Masse, Caratozzolo, Sparacia), the model was extended to include soil erodibility and slope steepness effects on plot soilloss.
KW - Plot soil loss
KW - Sediment concentration
KW - Empirical model
U2 - 10.1016/j.jhydrol.2011.01.029
DO - 10.1016/j.jhydrol.2011.01.029
M3 - Article
SN - 0022-1694
VL - 400
SP - 267
EP - 273
JO - Journal of Hydrology
JF - Journal of Hydrology
IS - 1-2
ER -