Geotechnical and GIS-based environmental factors and vulnerability studies of the Okemesi landslide,Nigeria

作     者：Oluwakemi Bolanle AKINTAN Johnson Adedeji OLUSOLA Olaniyi Patrick IMOLE Moyosoluwa Odunayo ADEYEMI Oluwakemi Bolanle AKINTAN;Johnson Adedeji OLUSOLA;Olaniyi Patrick IMOLE;Moyosoluwa Odunayo ADEYEMI

作者机构：Department of Geography and Planning ScienceEkiti State UniversityAdo EkitiNigeria Department of Geology and Mineral SciencesCrawford UniversityIgbesaOgun StateNigeria 

出 版 物：《区域可持续发展(英文)》 (Regional Sustainability)

年 卷 期：2023年第4卷第3期

页      面：249-260页

学科分类：0830[工学-环境科学与工程（可授工学、理学、农学学位）] 081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 

基　　金：the Tertiary Education Fund(TETFUND) Nigeria for funding this project 

主　　题：Rainfall-induced landslide Landslide hazards Slope materials Rainfall Geomorphology Vulnerability zone Okemesi-Ekiti(Okemesi) 

摘      要：Landslide is a geological hazard typically associated with extreme events such as earthquakes,heavy rainfall,volcanic eruptions,changes in groundwater level,*** 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 *** study also aimed to conduct a vulnerability analysis in the study area to identify regions with a probability of landslide *** 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 *** 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 *** 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%,*** analysis suggested that the Okemesi landslide was likely triggered by rainfall,which might have weakened the physical structure of slope *** the causes and impacts of landslides is crucial for policymakers to implement measures to mitigate landslide hazards,protect infrastructure,and prevent the loss of life in the landslide-prone regions.