CARVALHO NETO, J. G.; http://lattes.cnpq.br/7445192462637714; CARVALHO NETO, José Guimarães de.
Resumo:
In the regions where the monitoring network for runoff and erosion is deficient or
inexistent, the use of hydrological models can provide reasonable estimates of surface
runoff and soil loss, for watershed planning. This study deals with the application of the
model SWAT (Soil Water Assessment Tool) in the "Riacho dos Namorados" Watershed
and two of its sub-basins, 1 and 2 in the "Sao Joao do Cariri" Experimental Basin. The
model, with the GIS interface ArcSWAT, requires the "Digital Elevation Model" (DEM) of
the basin. The simulations were carried out using two different DEMs for the purpose of
comparison: one was derived from the interpolation of field data and the other obtained
through remote sensing. The model parameterization was done In the sub-basin 2 and
the validation performed in sub-basin 1 T h e model performance was evaluated by the
determination coefficient (R2) and of the efficiency factor of Nash-Sutcliffe. Riacho dos
Namorados Watershed was simulated by the model under the present conditions of land
use, by considering the presence of storage dams in one case and by ignoring them in
another. These simulations permitted an evaluation of the influence of the dams. In
order to evaluate the effects of changes of land use in the Riacho dos Namorados
Watershed, four other scenarios in which the basin could be found were simulated in
which the soil use considered were: (1) the native vegetation, (2) reforested with
Mesquite (Prosopis Juliflora), (3) with the monoculture of corn, and (4) soil cleared
bare. The influence of the dams in the basin simulated by the SWAT model was the
attenuation of both surface flow and the sediment load. Among the simulated scenarios,
reforestation with Mesquite protected the watershed against erosion better than the
native vegetation "caatinga" and the cultivation of corn was just better than bare soil
surface in terms of erosion. In conclusion, the SWAT model presented itself as a good
tool for hydrosedimentological simulation in the region of Cariri in Paraiba.