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Determination of the largest clast sizes of tephra deposits for the characterization of explosive eruptions: a study of the IAVCEI commission on tephra hazard modelling

机译:确定用于表征爆发性喷发的最大量的提夫拉沉积物:IAVCEI委员会对提夫拉危害建模的研究

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摘要

The distribution of clasts deposited around a volcano\udduring an explosive eruption typically contoured by\udisopleth maps provides important insights into the associated\udplume height, wind speed and eruptive style. Nonetheless,\uda wide range of strategies exists to determine the largest\udclasts, which can lead to very different results with obvious\udimplications for the characterization of eruptive behaviour\udof active volcanoes. The IAVCEI Commission on Tephra\udHazard Modelling has carried out a dedicated exercise to\udassess the influence of various strategies on the determination\udof the largest clasts. Suggestions on the selection of\udsampling area, collection strategy, choice of clast typologies\udand clast characterization (i.e. axis measurement and\udaveraging technique) are given, mostly based on a thorough\udinvestigation of two outcrops of a Plinian tephra deposit from\udCotopaxi volcano (Ecuador) located at different distances\udfrom the vent. These include: (1) sampling on a flat paleotopography\udfar from significant slopes to minimize remobilization\udeffects; (2) sampling on specified-horizontal-area sections\ud(with the statistically representative sampling area depending\udon the outcrop grain size and lithic content); (3) clast characterization\udbased on the geometric mean of its three orthogonal\udaxes with the approximation of the minimum ellipsoid (lithic\udfragments are better than pumice clasts when present); and\ud(4) use of the method of the 50th percentile of a sample of 20\udclasts as the best way to assess the largest clasts. It is also\udsuggested that all data collected for the construction of\udisopleth maps be made available to the community through\udthe use of a standardized data collection template, to assess the\udapplicability of the new proposed strategy on a large number\udof deposits and to build a large dataset for the future development\udand refinement of dispersal models.
机译:通常由\等宽线图勾勒出的火山爆发期间沉积在火山周围的碎屑的分布,对相关的\化石高度,风速和喷发方式提供了重要的见识。尽管如此,仍然存在各种各样的策略来确定最大的\破灭,这可能导致截然不同的结果,并以明显的\重复说明了活火山的喷发行为\ ud。 IAVCEI特发拉\ ud危害模型委员会进行了专门的演习,以\评估各种策略对确定最大碎屑的影响。给出了关于\取样区域选择,收集策略,选择岩屑类型\ ud和岩屑表征(即轴测量和\平均技术)的建议,这些建议主要基于对\ udCotopaxi的一次Tephra沉积物的两个露头的彻底\ ud调查。火山(厄瓜多尔)位于距喷口不同的距离\ ud。这些措施包括:(1)在平坦的古地形上采样/远离明显的斜坡,以最大程度地减少迁移/影响; (2)在指定的水平区域切片上\ ud(具有统计代表性的采样区域取决于\ ud露头的晶粒尺寸和岩屑含量); (3)基于三个正交\ udax的几何均值和最小椭球的近似来对clast进行特征化描述(当存在时,石块碎片比浮石碎片要好); \ ud(4)使用20个破骨细胞样本的第50个百分位数的方法作为评估最大碎屑的最佳方法。也\建议通过使用标准化的数据收集模板\\使使用的\ udisopleth maps的所有收集的数据提供给社区,以评估新提议的策略在大量\ udof存款上的\ udappability并建立一个大型数据集,以用于将来对扩散模型的开发\精炼。

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