基于岩土和gis的尼日利亚Okemesi滑坡环境因素和脆弱性研究

Q1 Social Sciences Regional Sustainability Pub Date : 2023-09-01 DOI:10.1016/j.regsus.2023.08.001
Oluwakemi Bolanle Akintan , Johnson Adedeji Olusola , Olaniyi Patrick Imole , Moyosoluwa Odunayo Adeyemi
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引用次数: 0

摘要

滑坡是一种地质灾害,通常与地震、强降雨、火山爆发、地下水位变化等极端事件有关。这项研究在尼日利亚西南部的Okemesi Ekiti(也称为Okemesi)进行,目的是利用遥感和GIS技术分析导致Okemesi滑坡发生的环境因素(粒度、抗直剪强度、降雨数据、湿密度、地表和坡度)。该研究还旨在对研究区域进行脆弱性分析,以确定有可能发生滑坡的区域。Okemesi滑坡区土壤的粒度分析表明,边坡材料中砾石17.14%,砂59.31%,细粒19.48%,因此土壤类型可归类为级配不良的砾砂,滑坡发生的可能性很高。研究区地貌特征为0.00°~49.00°的斜坡,而区内大部分斜坡小于8.00°。坡向主要为南部(157.51°~202.50°)、西南部(202.51°~247.50°)、西部(247.51°-292.50°),高地主要以北(0.00°-22.50°和337.51°-360.00°)、东北(22.51°-67.50°)、东(67.51°-112.51°)和东南(112.51°-157.50°)的斜坡方向为界。研究区可分为三个脆弱区:高、中、低,面积百分比分别为9.00%、61.80%和29.20%。分析表明,Okemesi滑坡很可能是由降雨引发的,这可能削弱了边坡材料的物理结构。了解滑坡的原因和影响对于决策者在滑坡易发地区实施减轻滑坡危害、保护基础设施和防止生命损失的措施至关重要。
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Geotechnical and GIS-based environmental factors and vulnerability studies of the Okemesi landslide, Nigeria

Landslide is a geological hazard typically associated with extreme events such as earthquakes, heavy rainfall, volcanic eruptions, changes in groundwater level, etc. This study was carried out in Okemesi-Ekiti (also known as Okemesi), Southwest Nigeria, with the purpose of using remote sensing and GIS technologies to analyze the environmental factors (grain size, direct shear strength resistance, rainfall data, wet density, surface, and slope) resulting in the occurrence of the Okemesi landslide. The study also aimed to conduct a vulnerability analysis in the study area to identify regions with a probability of landslide occurrence. The grain size analysis of the soil in the Okemesi landslide area showed that slope materials comprised 17.14% gravel, 59.31% sand, and 19.48% fines, thus the soil type could be classified as poorly graded gravely sand with a high possibility of landslide occurrence. The geomorphic characteristics of the study area was characterized by slopes ranging from 0.00° to 49.00°, while most slopes in the area were less than 8.00°. The slope aspect direction was mainly in south (157.51°–202.50°), southwest (202.51°–247.50°), west (247.51°–292.50°), and north (0.00°–22.50° and 337.51°–360.00°). The highlands were primarily bounded by the slope directions of north (0.00°–22.50° and 337.51°–360.00°), northeast (22.51°–67.50°), east (67.51°–112.51°), and southeast (112.51°–157.50°), which indicated the potential direction of mass movement. The study area can be divided into three vulnerability zones: high, medium, and low, with the area percentages of 9.00%, 61.80%, and 29.20%, respectively. The analysis suggested that the Okemesi landslide was likely triggered by rainfall, which might have weakened the physical structure of slope materials. Understanding the causes and impacts of landslides is crucial for policy-makers to implement measures to mitigate landslide hazards, protect infrastructure, and prevent the loss of life in the landslide-prone regions.

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来源期刊
Regional Sustainability
Regional Sustainability Social Sciences-Urban Studies
CiteScore
3.70
自引率
0.00%
发文量
20
审稿时长
21 weeks
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