Lake Nyos, a Multirisk and Vulnerability Appraisal

M. Tchindjang
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引用次数: 5

Abstract

Situated at the northern flank of the Oku Massif, Lake Nyos crater epitomizes landscape features originating from volcanic explosions during the Quaternary. The Cameroon Volcanic Line (CVL), to which it belongs, constitutes the most active volcanic region in Cameroon. In 1986, an outgas explosion occurred from beneath the lake and killed 1746 people in several neighbouring villages. The event influenced a radial area of 25 to 40 km wide, particularly in eastern and western direction. This was mainly due to: (1) the rugged nature of the landscape (fault fields), which enabled the heavier gas to follow valleys framed by faults corridors without affecting elevated areas; and (2) the seasonal dominating western wind direction, which channeled the gas along tectonic corridors and valleys. This paper assesses the geological risk and vulnerability in the Lake Nyos before and after several proposal to mitigate future outgas events. Remotely sensed data, together with GIS tools (topographic maps, aerial photographs), helped to determine and assess lineaments and associated risks. A critical grid combining severity and frequency analysis was used to assess the vulnerability of the local population. There is evidence that along the main fault directions (SW–NE), anthropogenic activities are most intensive and they may play an aggravating role for disasters. This requires the local population’s consciousness-raising. The results also show that population around Lake Nyos still remains vulnerable to volcanic hazards and floods. However, the area has been safe since the last degassing and jet grouting through multiple procedures and actions proposed in the National Contingency Plan, and equally by the relief organization plan (DROP or ORSEC plan) for the Menchum Division. Another issue is that the local population is concerned with the idea of returning to the affected areas in order to stay close to their ancestors or the deceased. Therefore, even after jet grouting and degassing, the problem of risk minimization for local residents remains.
尼奥斯湖,一个多风险和脆弱性评估
尼奥斯湖火山口位于奥库地块的北侧,是第四纪火山喷发形成的景观特征的缩影。它所属的喀麦隆火山线(CVL)构成了喀麦隆最活跃的火山地区。1986年,湖下发生了一次瓦斯爆炸,造成邻近几个村庄的1746人死亡。该事件影响了25至40公里宽的径向区域,特别是在东部和西部方向。这主要是由于:(1)断层田地形的崎岖不平,使得较重的天然气沿着断层走廊形成的山谷运移,而不会影响到高架地区;(2)季节主导的西风方向,使天然气沿构造廊道和峡谷输送。本文对尼奥斯湖的地质风险和脆弱性进行了评估,以减轻未来的天然气泄漏事件。遥感数据与地理信息系统工具(地形图、航空照片)一起帮助确定和评估地形和相关风险。一个结合严重程度和频率分析的临界网格被用来评估当地人口的脆弱性。有证据表明,沿主断裂方向(SW-NE),人类活动最为强烈,并可能对灾害起到加重作用。这需要当地民众的意识提高。结果还表明,尼奥斯湖周围的人口仍然容易受到火山灾害和洪水的影响。然而,通过国家应急计划中提出的多种程序和行动,以及Menchum分部的救援组织计划(DROP或ORSEC计划),该地区自上次脱气和喷射注浆以来一直是安全的。另一个问题是,当地居民担心回到受灾地区,以便与他们的祖先或死者保持密切联系。因此,即使在进行了喷射注浆和除气之后,如何将当地居民的风险降到最低的问题仍然存在。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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