Physiographic Characterization of the Córrego do Perdido River Basin – Ibatiba/ES

IF 0.2 Q4 AGRONOMY
A. H. D. O. Carvalho, Breno Dalcolmo De Almeida Leão, F. D. S. Castro
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Abstract

The use of natural resources has been accompanied by serious problems appearing from inadequate management. Thus, knowing the characteristics of the environmental planning units can contribute to minimizing damage and planning conservationist actions. The morphometric characteristics of the Córrego do Perdido river basin were determined for environmental planning purposes. To this end, we used radar data from the Shuttle Radar Topography Mission (SRTM) to represent the Digital Elevation Model (DEM) and geoprocessing techniques in a Geographic Information System (GIS) environment. To elucidate the hydrological behavior of the basin, we estimated some morphometric parameters. The drainage area obtained corresponds to 31.11 km², and the perimeter measures 33.57 km. With an irregular shape, the basin presented a shape factor equal to 0.12, compactness coefficient of 1.69, circularity index of 0.347 and small flow extension (0.1052 km). The drainage density found was 2.38 km-2, indicating high drainage capacity. The basin had a strong wavy terrain (47.38% of the total basin area), with an average slope of 30.6% and an average altitude of 1,145 meters. The physiographic characterization revealed through the morphometric indices that the basin has an elongated shape and a dendritic drainage network of fourth order and, disregarding the adverse hydrological events, is not very susceptible to flooding. The high drainage capacity contributes to the infiltration of water into the soil, and the vegetation cover of the slopes must be preserved.
Córrego do Perdido河流域——伊巴蒂巴/ES的地理特征
在利用自然资源的同时,也出现了管理不善的严重问题。因此,了解环境规划单位的特征有助于最大限度地减少破坏并规划环保行动。为了环境规划的目的,确定了Córrego do Perdido河流域的形态计量特征。为此,我们使用航天飞机雷达地形任务(SRTM)的雷达数据来表示地理信息系统(GIS)环境中的数字高程模型(DEM)和地理处理技术。为了阐明流域的水文行为,我们估计了一些形态计量参数。获得的流域面积为31.11 km²,周长为33.57 km。该流域形状不规则,形状系数为0.12,压实系数为1.69,圆形指数为0.347,流量较小(0.1052 km)。发现的排水密度为2.38km-2,表明排水能力高。盆地地形起伏较大(占盆地总面积的47.38%),平均坡度30.6%,平均海拔1145米。地貌特征通过形态计量指数显示,该盆地具有细长的形状和四级树枝状排水网络,并且不考虑不利的水文事件,不太容易受到洪水的影响。高排水能力有助于水渗入土壤,必须保留斜坡的植被覆盖。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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自引率
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30
审稿时长
53 weeks
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