IDENTIFICATION OF RIVER STYLES OF
THE RIACHO GRANDE HYDROGRAPHIC
BASIN, ALAGOAS
river styles; drylands; fluvial systems.
river styles; drylands; fluvial systems. |
The researches of fluvial systems of drylands is lower in comparison with the studies developed in humid
regions, lacking researches that highlight the particularities of these environments. Thus, the research
brought as issue the investigation of the fluvial dynamics of a hydrographic basin of the semi-arid
environment of Alagoas through associations between the local and regional physical characteristics, their
structural controls, and the interventions resulting from human action. The objective is the characterization
of fluvial typologies that exhibit the above-mentioned set of characteristics in order to know in a more
detailed way the hydrosedimentological dynamics of the main course of the Riacho Grande watershed.
Starting from the hypothesis that the aspects analyzed together can show impacts on the formation and
development of depositional features in the Riacho Grande. With this purpose, it was sought to apply the
first stage of the theoretical-methodological approach of fluvial styles to the main channel of the basin. It
was necessary the application of the Declivity-Extension Ratio (DER) index seeking the plateau ruptures;
the mapping of land use and land cover aiming the anthropic interferences; and the mapping of landscape
units for the investigation of domains of regional topographic controls. It was revealed that plateau ruptures
may be controlling sedimentation processes along the main course along the three landscape units
identified in the basin, being delimited with regions of homogeneous slope and topography. In these units,
land use showed an increase in anthropic intervention coverage over a 20-year period. Finally, four fluvial
typologies were identified: Unconfined, semi-confined with alluvial bed, confined with mixed rock-aluvial
bed, and confined with discontinuous floodplains. Each typology allowed understanding the association of
the data obtained and its expression in sediment deposits along the channel (or its absence). The research
has proven relevant to the development of studies in tropical drylands. Based on the initial phase of the
fluvial styles methodology, the character and behavior of the stretches could be evidenced and correlated in
a way that becomes useful for the management and planning of the study area in relation to water
resources.