干砾石和mata Úmida带之间的层流侵蚀敏感性:以canhoto河流域为例(pe / al)。

Vitor Carlos Vilela dos Santos, Kleber Carvalho Lima, Iaponan Cardins de Sousa Almeida
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引用次数: 0

摘要

层流侵蚀是土壤退化的主要过程之一,主要是因为它不易被察觉。在处理侵蚀时,重要的是要强调这是一个自然的环境过程,但它可以通过人类活动加速。从这个意义上说,本工作的目的是通过对Canhoto河流域(PE/AL)的案例研究,评估在Agreste和Zona da Mata之间的水文盆地中土壤对层流侵蚀的自然敏感性。采用的方法使用土壤可蚀性和坡度数据,以1:10万的比例确定易受层流侵蚀的地区。结果表明:流域面积的75%以上分布在半干旱区的ⅰ类和ⅱ类之间,从侵蚀过程的产生角度来看存在弱点;具有高可蚀性的土壤比例高,坡度百分比变化大,导致易受侵蚀的地区,因此成为该地区研究这一主题的重要对象。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SUSCEPTIBILITY TO LAMINAR EROSION BETWEEN THE DRY AGRESTE AND THE MATA ÚMIDA ZONE: A CASE STUDY OF THE CANHOTO RIVER BASIN (PE/AL).
Laminar erosion is one of the main processes of soil degradation, mainly because it is hardly noticeable. When dealing with erosion, it is important to emphasize that it is a natural environmental process, but it can be accelerated through human actions. In this sense, the aim of this work is to evaluate the natural susceptibility of soils to laminar erosion in hydrographic basins between the Agreste and Zona da Mata, through the case study of the Canhoto river basin (PE/AL). The methodology adopted used data on soil erodibility and slope to identify areas susceptible to laminar erosion, on a scale of 1:100,000. The results showed that more than 75% of the basin area was distributed between classes I and II, which are in the semi-arid area, presenting weaknesses from the point of view of the generation of erosive processes. There are high percentages of soils with high rates of erodibility and a great variability in the percentage of slope, resulting in areas susceptible to erosion, thus becoming an important object of study, given the need for research on this topic in the region.
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