山林公路沿线山体滑坡的评价:喀麦隆火山线上穿越巴法特和贝方森林的巴门达环线路段。

E. Amah, V. Katte, R. Ghogomu,  V K Kamgang
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引用次数: 1

摘要

目的:山体滑坡给世界各地的社区造成痛苦,扰乱社会经济活动,破坏道路基础设施。本研究的目的是对位于喀麦隆火山线(CVL)沿线喀麦隆西北地区穿过巴夫特和巴方山林的巴门达环路(BRR)段经常性滑坡事件进行综合评估。方法:采用地形图和地质图研究、脚踏调查、水文气象数据分析和土壤渗透性试验进行研究。本研究的结果显示,在巴法特有35个新的滑坡,在北方森林有16个。研究发现:研究区地形高度在670 ~ 1300 m之间,50%以上的斜坡为凸形,其余为凸线状、凹形,少数为线状。自然坡度从35-600不等,而滑坡普遍发生在次垂直路堑路堤上。滑坡被归类为体积小、移动距离短、浅平移而非旋转的泥石流。基岩主要为粗粒白晶花岗岩,含石英、长石、黑云母、白云母等易风化矿物。同时,残余土样品具有渗透性,孔隙水压力增大,粘土含量高,液化倾向强。近期或历史地震的缺失表明,滑坡的致病因素可能与陡峭的坡度、岩性、深层风化剖面、风化物质对水的相当亲和力以及长时间的雨季有关。因此,我们强调山体滑坡灾害的作用,其直接风险是道路的广泛恶化,其特点是道路有多重缺陷,社会经济活动减少,以及与货物和人员流动以及资源管理方面的困难有关的间接风险。建议:本研究建议现任官员改进他们在监测降雨和滑坡灾害以及管理灾害紧急情况方面的文件和技能;提高市民对山崩灾害及相关风险的认识。政府有必要建立一个道路管理局来管理滑坡灾害、救灾和道路内外的土地。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An Assessment of Landslides along Mountain Forest Roads: Bamenda Ring Road Segment through Bafut and Befang Forests on the Cameroon Volcanic Line.
Purpose: Landslides cause distress in communities worldwide, disrupt socio-economic activities and cause damage to roads infrastructure. The purpose of this study was to undertake a comprehensive assessment of the recurrent landslide events along the Bamenda Ring Road (BRR) segment through the Bafut and Bafang mountain forests in the North West Region of Cameroon, located along the Cameroon Volcanic Line (CVL). Methodology: Topographic and geologic map studies, foot-borne surveys, hydro-meteorological data analysis and soil permeability tests were employed to the study. Results at the time of this study reveal 35 new slide scarps in Bafut and 16 along the Befang forests. Findings: The topography culminates between 670-1300 m altitude, while more than 50% of the slopes in the study area are convex, the rest are convexo-linear, concave, while a few of them are linear. Natural slope gradients vary from 35-600, while prevalent number of slides occur on sub-vertical road-cut embankments. The slides are classified as small volume, short distance-travelled shallow translational than rotational debris flows. Base rocks of the study zone are essentially coarse-grained leucocratic granites with quartz, feldspars, biotite and muscovite minerals which appear liable to weathering. Meanwhile, residual soil samples are permeable, have increased pore water pressure and has a high liquefaction tendency due to its high clay content. The absence of recent or historic earthquakes suggests that causative factors of landslides could be linked to steep gradients, lithology, deep weathering profiles, considerable affinity for water of the weathered materials and prolonged rainy seasons. As such we highlight the contribution of the landslide hazard with the direct risk based on the extensive deterioration of the road characterized by multiple road defects and reduced socio-economic activities and the indirect risk linked to difficulties in the movement of goods and persons and management of resources. Recommendations: This study recommend present officials to improve on their documentation and skills in monitoring rainfall and landslide hazard and manage disaster emergency; sensitize the population on landslide hazard and associated risk. There is need for government to establish a road authority for the management of landslide hazard, disaster relief and the land inside and outside the road.
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