O impacto da desertificação na hidrologia: um estudo de modelagem para a bacia do rio Seridó
Land use in the Seridó river basin is the main factor in the intensification of desertification in this region, where desertification interferes with the hydrology of the basin. Among its effects on the soil are the low quality and the change in the availability of water resources. The objective...
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| Formato: | Dissertação |
| Idioma: | pt_BR |
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Universidade Federal do Rio Grande do Norte
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| Endereço do item: | https://repositorio.ufrn.br/handle/123456789/47606 |
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| Resumo: | Land use in the Seridó river basin is the main factor in the intensification of desertification in
this region, where desertification interferes with the hydrology of the basin. Among its effects
on the soil are the low quality and the change in the availability of water resources. The
objective of this study was to evaluate the impacts of desertification on the hydrology of the
Seridó river basin via hydrological modeling. The hydrological model used was the SWAT,
which proved to be an effective tool, as it satisfactorily simulated the seasonality of the monthly
flow in four tributary sub-basins of the Seridó river, simulating the observed flow variance by
more than 60%. In the evaluation of the model, it was observed greater skill in flows equal to
or less than Q5% (maximum flows) and the PBIAS (RMSE) of the simulated flow was ~ 30%
(8,3 m³.s-1) and 50% (11,8 m³.s-1) for the model calibration and validation periods, respectively.
To assess desertification, two land use and land cover scenarios were developed for the
watershed: the control scenario, where the vegetation cover of the basin was that observed in
1985; and the desertification scenario, where desert areas were included from 1985 to 2019.
The historic and gradual advance of the desert (+15,39%) altered the annual water balance,
increasing the total runoff ( ) by 6,95%, due to the increase in surface runoff ( ), which
increased by 12,08%. This change altered the Q5% regime, associated with floods, which were
increased in the desertification scenario. In average absolute terms, the changes in and
were +14 mm.month-1 and +11 mm.month-1 in the wet season, respectively. On the other
hand, the subsurface runoff ( ) decreased by 15,34% in relation to the annual balance,
although it increased by 1,5 mm.month-1 in the rainy season. The annual evapotranspiration
( ) reduced by 4,18%, which corresponded to -5 (-2) mm.month-1 in the rainy season (dry).
The same impact occurred with soil water content ( ) and percolation ( ), in which the
average annual reductions were 3,79% and 1,96%, -45 mm.month-1 and -4 mm.month-1 in the
rainy season, in order. In spatial terms, , and ( , and ) were
significantly reduced (expanded) in the central-west region of the basin. In general, found that
desertification increases the extremes of Q5% and deteriorates the hydrological conditions,
locally and in the areas adjacent to the desert regions, with the reduction of and , and
the increase of . Such effects are expected, as desertification reduces infiltration due to
the degree of compaction of the bare soil, unbalancing the groundwater system. Therefore, the
maintenance of natural and agricultural ecosystems will be harmed. |
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