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The 2002–03 Etna explosive activity: Tephra dispersal and features of the deposits

机译:2002-03年度Etna爆炸活动:Tephra扩散和矿床特征

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The onset of Mt. Etna's 2002–03 eruption was marked by intense explosive activity beginning on 27 October 2002 and persisting until 30 December. This phase of activity produced abundant ash emission that impacted the local economy and air traffic. Thereafter, explosive activity declined with the eruption ceasing on 28 January 2003. In this paper, we present field data collected during the eruption and use these to obtain input data for tephra dispersal model. This was applied, after validation, to extrapolate the total distribution of the deposits emplaced during the explosive activity. Detailed sampling of fallout deposits was completed on 27, 28, 31 October and 4 November. This enabled construction of isomass maps and calculation of the erupted mass. Grain-size analysis of all collected samples was used to reconstruct the total grain-size distribution which displays a peak at 0.5 Φ. Column height was estimated at 3.3–7 km by combining barometrical altimeter data during over-flights with the analysis of images and videos. This was used to estimate a total erupted mass of 4.4 ± 0.6 × 1010 kg. Simulations showed that the deposit was significantly affected by variations in wind direction and mass eruption rate, with deposits being dispersed mainly on the E sector of the volcano due to a dominant easterly wind. Our study underlines that basaltic volcanoes, such as Etna, can produce huge amounts of ash, as well as lava, and that an improvement in the knowledge of dispersal processes during prolonged explosive activity is required to better mitigate the associated hazards.
机译:山的发作。埃特纳火山(Etna)在2002-03年喷发,其特征是从2002年10月27日开始一直持续到12月30日,发生了强烈的爆炸活动。活动的这一阶段产生了大量的烟灰排放,影响了当地经济和航空运输。此后,爆炸活动随着2003年1月28日爆发的停止而下降。在本文中,我们介绍了爆发期间收集的现场数据,并利用这些数据获得了特非拉扩散模型的输入数据。在验证之后,将其用于推断爆炸活动期间放置的沉积物的总分布。 10月27日,28日,31日和11月4日完成了对沉淀沉积物的详细采样。这样就可以构造等值线图并计算爆发质量。所有收集样品的粒度分析用于重建总粒度分布,该分布在0.5Φ处出现峰值。通过将飞越过程中的气压高度计数据与图像和视频分析相结合,估计柱高在3.3–7 km。这被用来估计总喷发质量为4.4±0.6×1010 kg。模拟表明,沉积物受风向和喷发速率的变化影响很大,由于主要是东风,沉积物主要分散在火山的E区段。我们的研究强调,像埃特纳火山这样的玄武岩火山会产生大量的灰烬和熔岩,并且需要在长时间的爆炸活动中改善散布过程的知识,以便更好地减轻相关的危害。

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