Suppr超能文献

圣海伦斯火山火山灰渗滤液成分的空间分析:对未来采样策略的启示。

Spatial analysis of Mount St. Helens tephra leachate compositions: implications for future sampling strategies.

作者信息

Ayris P M, Delmelle P, Pereira B, Maters E C, Damby D E, Durant A J, Dingwell D B

机构信息

Department of Earth and Environmental Sciences, Ludwig Maximilian University, Thereisenstrasse 41/III, 80333 Munich, Bavaria Germany.

Earth and Life Institute, Université Catholique de Louvain, Croix du Sud 2, bte L7.05.10, 1348 Louvain-la-Neuve, Wallonia Belgium.

出版信息

Bull Volcanol. 2015;77(7):60. doi: 10.1007/s00445-015-0945-8. Epub 2015 Jun 13.

Abstract

Tephra particles in physically and chemically evolving volcanic plumes and clouds carry soluble sulphate and halide salts to the Earth's surface, ultimately depositing volcanogenic compounds into terrestrial or aquatic environments. Upon leaching of tephra in water, these salts dissolve rapidly. Previous studies have investigated the spatial and temporal variability of tephra leachate compositions during an eruption in order to gain insight into the mechanisms of gas-tephra interaction which emplace those salts. However, the leachate datasets analysed are typically small and may poorly represent the natural variability and complexity of tephra deposits. Here, we have conducted a retrospective analysis of published leachate analyses from the 18 May 1980 eruption of Mount St. Helens, Washington, analysing the spatial structure of the concentrations and relative abundances of soluble Ca, Cl, Na and S across the deposits. We have identified two spatial features: (1) concentrated tephra leachate compositions in blast deposits to the north of the volcano and (2) low S/Cl and Na/Cl ratios around the Washington-Idaho border. By reference to the bulk chemistry and granulometry of the deposit and to current knowledge of gas-tephra interactions, we suggest that the proximal enrichments are the product of pre-eruptive gas uptake during cryptodome emplacement. We speculate that the low S/Cl and Na/Cl ratios reflect a combination of compositional dependences on high-temperature SO uptake and preferential HCl uptake by hydrometeor-tephra aggregates, manifested in terrestrial deposits by tephra sedimentation and fallout patterns. However, despite our interrogation of the most exhaustive tephra leachate dataset available, it has become clear in this effort that more detailed insights into gas-tephra interaction mechanisms are prevented by the prevalent poor temporal and spatial representativeness of the collated data and the limited characterisation of the tephra deposits. Future leachate studies should aim to extensively sample across tephra deposit limits whilst simultaneously characterising deposit stratigraphy and tephra chemistry, mineralogy and granulometry, taking steps to ensure the quality and comparability of collected leachate datasets.

摘要

在物理和化学性质不断演变的火山羽流和云层中的火山灰颗粒,将可溶性硫酸盐和卤化物盐携带到地球表面,最终将火山成因化合物沉积到陆地或水生环境中。火山灰在水中浸出时,这些盐会迅速溶解。此前的研究调查了火山喷发期间火山灰渗滤液成分的时空变化,以便深入了解使这些盐就位的气-灰相互作用机制。然而,所分析的渗滤液数据集通常较小,可能无法很好地代表火山灰沉积物的自然变异性和复杂性。在此,我们对华盛顿州圣海伦斯火山1980年5月18日喷发的已发表渗滤液分析进行了回顾性分析,分析了整个沉积物中可溶性钙、氯、钠和硫的浓度及相对丰度的空间结构。我们识别出了两个空间特征:(1)火山北侧爆炸沉积物中浓缩的火山灰渗滤液成分;(2)华盛顿州与爱达荷州边境附近较低的硫/氯和钠/氯比率。通过参考沉积物的整体化学性质和粒度分析以及当前关于气-灰相互作用的知识,我们认为近端富集是隐火山穹丘就位期间喷发前气体吸收的产物。我们推测,低硫/氯和钠/氯比率反映了高温下对硫的吸收以及水凝物-火山灰聚集体对氯化氢优先吸收的成分依赖性的综合作用,在陆地沉积物中通过火山灰沉降和沉降模式表现出来。然而,尽管我们对现有最详尽的火山灰渗滤液数据集进行了研究,但在这项工作中已经清楚地认识到,整理数据普遍较差的时空代表性以及火山灰沉积物有限的特征描述阻碍了对气-灰相互作用机制更详细的深入了解。未来的渗滤液研究应旨在对火山灰沉积物边界进行广泛采样,同时对沉积物地层学以及火山灰的化学性质、矿物学和粒度进行表征,并采取措施确保所收集渗滤液数据集的质量和可比性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/d793/4498446/6377cf6a6306/445_2015_945_Fig1_HTML.jpg

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验