Remote sensing and sig contribution for the identification of the fracturation influence on the drainage network architecture in the High Ziz River basin, Central High Atlas, Morocco

Q3 Environmental Science Limnological Review Pub Date : 2019-12-01 DOI:10.2478/limre-2019-0013
Khadija Diani, I. Kacimi, H. Elbelrhiti, M. Zemzami, H. Tabyaoui, L. Masmoudi
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引用次数: 4

Abstract

Abstract This study aims to contribute to a better estimation of the density of fractures likely to favour the drainage of surface water in the High Ziz River (HZR) basin. The method adopted consists of the use of different airborne image processing techniques (filtering, enhancement and slope analysis) which allow a good discrimination of image discontinuities (lineaments) that can then be used for producing lineament maps. The influence of these lineaments on the underground flow is then studied. Indeed, it was possible to extract the lineament network, following the exploitation of remote sensing and an objectively completed analog analysis using the PCI Geomatica LINE module and its directional filters (Sobel directional filters by the ACP method), and to extract the hydrographic network of the HZR basin, using the ArcHydro tool. After superimposing these data, their thematic maps (of the lineament and hydrographic network) were developed. In addition, this comparison of the two hydrographic networks and lineament maps showed us very varied flow directions influenced by geological structures, particularly fracturing. The topography of the region also has a secondary impact on flows through the presence of slopes generally oriented towards the SE of the basin. The correlation of the results with the different directions of the orders of the hydrographic network allowed us to identify the potential effects of lineaments on the orientations of surface water circulation. In addition to these results, the realization of the Rose diagram indicated that the dominant trend in lineaments is N90–45N° (NE–SW).
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摩洛哥中部高阿特拉斯地区高济兹河流域裂缝对水系结构影响的遥感识别及显著贡献
摘要:本研究旨在更好地估计高孜河(HZR)流域可能有利于地表水排水的裂缝密度。所采用的方法包括使用不同的航空图像处理技术(滤波、增强和坡度分析),这些技术可以很好地区分图像不连续点(线条),然后用于制作线条图。研究了这些地形对地下水流的影响。事实上,利用PCI Geomatica LINE模块及其定向过滤器(采用ACP方法的Sobel定向过滤器),利用遥感技术和客观完成的模拟分析,可以提取线状网络,并使用archhydro工具提取HZR盆地的水文网络。在将这些数据叠加之后,就绘制了他们的专题地图(线线和水文网)。此外,这两个水文网络和线形图的对比显示,受地质构造,特别是压裂影响,流动方向变化很大。该地区的地形也通过通常朝向盆地东南方向的斜坡的存在对流动产生次要影响。结果与水文网阶不同方向的相关性使我们能够确定地形对地表水循环方向的潜在影响。在此基础上,Rose图的实现表明,在N90-45N°(NE-SW)方向上,各剖面的主要趋势为N90-45N°。
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来源期刊
Limnological Review
Limnological Review Environmental Science-Ecology
CiteScore
1.60
自引率
0.00%
发文量
0
审稿时长
16 weeks
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