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Sand mining and morphometric dynamics along Ologe Lagoon

机译:沿OLOGE泻湖的沙坑和形态学动力学

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The study focuses on the sand mining activities and morphometric dynamics of Ologe Lagoon, in Lagos, Nigeria. It determines the sand mining activities and morphometric dynamics of Ologe Lagoon catchment area, the quantity of sand mined per unit time, and the extent of environmental degradation due to the continuous sand mining activities. Topographic maps of the 1985 and 2013 Ikonos satellite imagery were used to identify the morphometric dynamics of the area. Two hypotheses were generated to determine if there are significant differences between the means of the sampled population that lost properties due to flooding, and to determine if there was a correlation between building subsidence and loss of property; it was tested using Analysis of Variance (ANOVA) with a correlation coefficient at 0.05 α significance level. The results of geometric measurement of the Ologe Lagoon between the two years interval show that perimeter width and circularity of the basin had reduced and shrunk, while the form factor remains the same at 0.15 km~2. The basin elongation increased significantly by 0.01 km~2, thus, increasing the rate at which water will be supplied to the lagoon. The ration of the form factor of 0.69/0.5 is close to the unity value R1, which shows a higher peak runoff; the values of the circularity ratio of 3.94/3.13 indicates circularity. This shows that the basin is circular time. The impact of the geometry indicates the development of mud flats and sandy bars, particularly at the lower portion of the lagoon; there is also modification of sediment deposition. The anthropogenic activity of sand mining causes destruction of the riparian forest around the lagoon. There is no significant difference in the means of sampled respondents regarding loss properties due to flooding, while there is a correlation between building subsidence and loss of life. It is recommended that a road map should be developed and implemented by the relevant agency of the government to guide anthropogenic activities around the lagoon to enhance sustainable development.
机译:该研究侧重于尼日利亚拉各斯州奥格泻湖的沙坑活动和形态学动态。它决定了OLOGE泻湖集水区的沙坑活动和形态学动力学,每单位时间开采的沙子数量,以及由于连续的沙坑活动导致的环境降解程度。 1985年和2013年IKONOS卫星图像的地形图用于识别该地区的形态学动态。生成两个假设以确定采样群的手段之间存在显着差异,这些群体因洪水而丧失的属性,并确定建筑物沉降与财产损失之间是否存在相关性;使用差异分析(ANOVA)进行测试,其相关系数为0.05α显着水平。两年间隔内OLOGE泻湖几何测量结果表明,盆地的周边宽度和圆形度降低,而形状因子在0.15 km〜2时保持相同。盆地伸长率明显增加0.01 km〜2,因此增加了水将提供给泻湖的速率。形状因子为0.69 / 0.5的差异接近统一值R1,显示出更高的峰值径流;圆形比为3.94 / 3.13表示圆形。这表明盆地是圆形时间。几何形状的影响表明泥浆和砂杆的开发,特别是在泻湖的下部;还有沉积物沉积的改变。沙坑的人为活性导致泻湖周围的河岸森林破坏。由于洪水导致的损失特性的抽样受访者的手段没有显着差异,而建筑沉降与生命丧失之间存在相关性。建议由政府的有关机构制定和实施路线图,以指导泻湖周围的人为活动,以提高可持续发展。

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