首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Computer simulations of lava flow paths in the town of Goma, Nyiragongo volcano, Democratic Republic of Congo
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Computer simulations of lava flow paths in the town of Goma, Nyiragongo volcano, Democratic Republic of Congo

机译:刚果民主共和国尼拉贡戈火山戈马镇熔岩流径的计算机模拟

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The 17 January 2002 fissure eruption of Mount Nyiragongo, Democratic Republic of Congo, produced lava flows which entered and devastated the densely inhabited town of Goma. The 2002 and previous 1977 eruptions demonstrate the high level of volcanic risk in the area. We present an analysis of the susceptibility to lava flow invasion in Goma, by means of computer simulations based on the steepest descent path and probabilistic-computed flow spreading and obstacle overcoming. The DEM is obtained from a topographic map of Goma by using the DEST algorithm. The numerical results show the distribution of probable lava flow paths from possible vents in the investigated topographic domain. Numerical simulations are validated through comparison with the mapped paths of the 2002 lava flows in Goma. The subsequent investigation includes the analysis of (1) hypothetical lava flow paths from ephemeral vents on the edge of the 2002 lava flows, (2) paths from venting along the hypothetical extension of the 2002 fissures, (3) paths in case of lava flow arrival in town from the north, and (4) changes induced by the presence of the solidified 2002 lava field. The results show the susceptibility of the different parts of the town of Goma to be invaded by future lava flows, and reveal the existence of a large area in town with minimum susceptibility and which can be invaded only in case of venting within it. The areas destroyed by the 2002 lava flows are predicted to be characterized by maximum susceptibility to lava flow invasion.
机译:2002年1月17日,刚果民主共和国尼拉贡戈山裂隙喷发,产生了熔岩流,这些熔岩流进入并摧毁了人口稠密的戈马镇。 2002年和1977年以前的火山爆发表明该地区火山爆发的风险很高。我们通过基于最陡下降路径,概率计算的流量扩散和克服障碍的计算机模拟,对戈马地区熔岩流入侵的敏感性进行了分析。通过使用DEST算法从戈马的地形图获得DEM。数值结果表明,在研究的地形域中,可能的熔岩流路径可能来自可能的喷口。通过与2002年戈马熔岩流的映射路径进行比较,对数值模拟进行了验证。随后的研究包括(1)从2002年熔岩流边缘的临时泄洪洞流出的假想熔岩流路径,(2)沿着2002年裂隙假想延伸的泄空路径,(3)发生熔岩流的路径进行分析从北部进入城镇,以及(4)凝固的2002年熔岩田的存在引起的变化。结果表明,未来熔岩流将侵扰戈马镇不同地区的敏感性,并揭示了该镇存在着一个大区域,敏感性最小,只有在其内部通风的情况下才可以侵入。预计2002年熔岩流破坏的地区将以对熔岩流入侵的最大敏感性为特征。

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