H2O Speciation, Reaction Kinetics and Viscosity of Hydrous Silicate Melts

水合硅酸盐熔体的 H2O 形态、反应动力学和粘度

• 批准号: 0537598
• 负责人: Youxue Zhang
• 金额: $ 30万
• 依托单位: Regents of the University of Michigan - Ann Arbor
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2006
• 资助国家: 美国
• 起止时间: 2006-01-01 至 2008-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0537598&HistoricalAwards=false
• 关键词: H2O; Speciation; Reaction; Kinetics; Viscosity

Explosive volcanic eruptions have caused devastations in human history. They are powered by dissolved water in magma, similar to Champagne eruptions powered by dissolved carbon dioxide in alcohol-water liquid. Bubble growth and magma fragmentation are key processes in explosive eruptions. Virtually all magmatic processes, including bubble growth, magma fragmentation, and magma flow are strongly dependent on the viscosity of magmas. In order to understand volcanic eruptions, especially the non-explosive to explosive transition, there is a critical need for viscosity data on wet silicate melts at relatively high viscosity and under pressure. This grant will support new experimental work to obtain such viscosity data. Furthermore, effort will be made to develop a comprehensive model to predict viscosity of all natural silicate melts using newly available data and literature data.Results from the grant will be critical to the understanding and modeling of bubble growth, magma fragmentation that defines explosive volcanic eruptions, and dynamics of volcanic eruptions, helping the mitigation of volcanic hazards. Furthermore, the investigation of the hydrous species equilibrium in silicate melts will lead to better understanding of the thermodynamics of, and water solubility and diffusivity in these hydrous melts, important to volcanology and igneous petrology. Collaboration with foreign scientists will further international scientific networking. Research results will be published in scientific journals, and will be incorporated into teaching and disseminated to the general public when appropriate.

火山爆发在人类历史上造成了巨大的破坏。 它们由岩浆中溶解的水提供动力，类似于香槟喷发由酒精-水液体中溶解的二氧化碳提供动力。 气泡增长和岩浆破碎是爆发性喷发的关键过程。 实际上，所有的岩浆过程，包括气泡生长、岩浆碎裂和岩浆流动，都强烈依赖于岩浆的粘性。 为了了解火山爆发，特别是非爆炸性到爆炸性的转变，有一个关键的需要在相对较高的粘度和压力下的湿硅酸盐熔体的粘度数据。这笔赠款将支持新的实验工作，以获得这样的粘度数据。 此外，将努力开发一个综合模型，预测所有天然硅酸盐熔体的粘度使用新的可用数据和文献数据，从赠款的结果将是至关重要的理解和泡沫的增长，岩浆破碎，定义爆炸性火山爆发，火山爆发的动力学模型，帮助减轻火山灾害。 此外，在硅酸盐熔体中的含水物种平衡的调查将导致更好地了解这些含水熔体的热力学，水溶解度和扩散性，重要的火山学和火成岩学。与外国科学家的合作将进一步促进国际科学网络。 研究结果将在科学期刊上发表，并将纳入教学，并在适当时向公众传播。