GEOMORPHOLOGICAL MAPPING OF PART OF THE NIGER DELTA, NIGERIA USING DEM AND MULTISPECTRAL IMAGERY

S. Odunuga, Saheed Adekunle Raji
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引用次数: 2

Abstract

This study utilised geo-information technology to carry out a geomorphological mapping of a part of the Niger Delta. Satellite image analysis was based on bi-annual seasonal approach using a combination of visual analysis of the geometry, site, situation, colour, and season for analysis of the non-topographic features. The study also utilised virtual and onsite fieldworks and existing geomorphologic information to interpret and analyse topographic and bathymetric features. First-order topographic features (elevation) and second level features including slope, aspect, curvature and mathematically exaggerated shaded relief were extracted from DEM. Relief classification was based on average elevation differences, hill shade, slope, and aspect. Three main non-topographic landforms were identified; the permanent rivers with stable meanders, perennially-active systems of creeks and fluvial landforms including scroll bars and oxbows. With the exception of higher elevation values towards the north-western fringe, the elevation ranges between mean sea level and 1 metre above sea level thus establishing a somewhat flat terrain. These areas were filled with meandering streams, sinuous creeks and watercourses flanked by mangrove vegetation.  In the north-western area, elevation rose close to approximately 4 metres in most of the area with a peak of 10 metres.  Generally, the cumulative area-slope analysis yielded a deltaic plain with generalised slope ≤ 20. Overall two elevation-based geographically differentiated morphological units were identified; tidal mudflats and saltmarshes. The study recommends that to provide needed information for resource planning and management, further investigation should be carried out with a view to modelling probable ecological and geomorphological changes in the entire Niger Delta.    
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使用dem和多光谱图像对尼日利亚尼日尔三角洲部分地区进行地貌测绘
本研究利用地理信息技术对尼日尔三角洲部分地区进行了地貌测绘。卫星图像分析是基于两年一次的季节性方法,结合几何形状、地点、情况、颜色和季节的视觉分析来分析非地形特征。该研究还利用虚拟和现场实地考察以及现有的地貌信息来解释和分析地形和水深特征。从DEM中提取一阶地形特征(高程)和二级特征,包括坡度、坡向、曲率和数学上夸张的阴影起伏。地形分类基于平均高差、山阴、坡度和坡向。确定了三种主要的非地形地貌;具有稳定曲流的永久河流,常年活跃的小溪系统和河流地貌,包括滚动条和牛轭。除了西北边缘的海拔较高外,海拔高度介于平均海平面和海拔1米之间,因此形成了一个比较平坦的地形。这些地区充满了蜿蜒的溪流,蜿蜒的小溪和两侧有红树林植被的水道。在西北地区,大部分地区的海拔上升接近4米,最高峰为10米。总的来说,累积面积-坡度分析得出的三角洲平原一般坡度≤20。总体上确定了两个基于海拔的地理分化形态单位;潮汐泥滩和盐沼。该研究建议,为了提供资源规划和管理所需的资料,应进行进一步的调查,以期模拟整个尼日尔三角洲可能发生的生态和地貌变化。
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