http://www.cnr.it/ontology/cnr/individuo/prodotto/ID70333
Validating SEdiment Delivery Distributed (SEDD) model in a small Calabrian basin. (Articolo in rivista)
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- Validating SEdiment Delivery Distributed (SEDD) model in a small Calabrian basin. (Articolo in rivista) (literal)
- Anno
- 2008-01-01T00:00:00+01:00 (literal)
- Alternative label
1 CALLEGARI G.,2 CATONA F., 3 FERRO V., 2 PORTO P. (2008)
Validating SEdiment Delivery Distributed (SEDD) model in a small Calabrian basin.
in Catena (Cremling.)
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- 1 CALLEGARI G.,2 CATONA F., 3 FERRO V., 2 PORTO P. (literal)
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- 1 CNR - Istituto per i Sistemi Agricoli e Forestali del Mediterraneo, Unità Operativa di Supporto di Cosenza, Rende (CS)
2 Dipartimento di Scienze e Tecnologie Agro-Forestali e Ambientali - Università degli Studi Mediterranea di Reggio Calabria
3 Dipartimento di Ingegneria e Tecnologie Agro-Forestali - Università di Palermo (literal)
- Titolo
- Validating SEdiment Delivery Distributed (SEDD) model in a small Calabrian basin. (literal)
- Abstract
- Validation of soil erosion and sediment yield models is very important in several
environmental contexts, such as the assessment of soil loss from agricultural
lands and the estimation of water pollution risk for humans and aquatic ecosystems.
In southern Italy, where soil loss associated with extreme rainfall events can
reach annual values of 100 t ha-1, soil erosion has become a serious
environmental problem and there is a need to validate some theoretical models
so that they can be used with confidence for predicting soil loss in different
contexts.
In this paper, the SEdiment Delivery Distributed model based on the USLE
and the sediment delivery ratio of each morphological unit into which the basin
is divided, is validated in a small basin (W2) located in Calabria (southern Italy).
In previous contributions, the SEDD model was calibrated over the same
basin using 52 events for the recording period 1978-1994.
The model is now applied at the event and annual scale using sediment yield
data collected during the period 2005-2007 at the basin outlet.
In particular the median value of the specific parameter ?e,m, which was
estimated at the event scale with an inverse modelling approach during the
calibration phase is now introduced into the model and the calculated sediment
yield values, associated with the new events, have been compared with the
measured ones.
The parameter ?e of each event was also estimated with an independent
relationship that relates ?e to runoff coefficient RCe at event scale. The reliability
of the comparison between estimated and measured values of sediment yield
encourages the use of SEDD to predict sediment yield at the event scale in small
basins.
The validation of the SEDD model was also carried out at the annual scale. In
this case, a median annual value of the specific parameter ?a,m was available.
This median value, estimated in the previous analysis using the sediment yield
measurements carried out between 1978-1994, was used to calculate the totalsediment yield during the year 2006 and to compare it with the measured one.
The same relationship between ?a and runoff coefficient RCa was applied at the
annual scale in order to obtain a suitable estimate of the representative value of
?a,m for long-term prediction of sediment yield.
Using this approach, the parameter ?a,m was recalibrated using all available
measurements at an annual scale (1978-1994 and 2006) and allowed the
application of the SEDD model at the mean annual scale to determine the spatial
distribution of the sediment yield into the basin.
These estimates of sediment yield were compared with the rates of net soil
loss provided by 137Cs measurements carried out in 1998 and 1999. The reasonable
agreement between the two sets of sediment yield estimates confirmed the
applicability of the Sediment Delivery Distributed model if the specific parameter
?a,m is calibrated using measured data. (literal)
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