ROW: Application of Fluid Dynamics & Geochemistry: The Essence of Processes in the Earth's Crust. A Learning Experience in Fluid Flow.

ROW：流体动力学的应用

• 批准号: 9011034
• 负责人: Barbara Dutrow
• 金额: $ 5.75万
• 依托单位: University of Iowa
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 1990
• 资助国家: 美国
• 起止时间: 1990-12-01 至 1992-11-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9011034&HistoricalAwards=false
• 关键词: ROW; Application; Fluid; Dynamics; &amp

It is proposed to incorporate principles of fluid dynamics, heat and mass transfer with knowledge of mineral and aqueous chemistry. Ultimately, this will lead to an integrated approach concerning the behavior of minerals and fluids resulting from changes in state conditions caused by fluid flow, and the physical manifestation of such processes. Identification and quantification of the dominate factors involved in fluid circulation allows one to predict and describe where the most vigorous fluid mineral reactions will occur. Integration of fluid dynamics will hopefully lead to new innovative methods of exploration and frontiers of discovery in fluid-mineral systems. The proposed activities are designed to obtain an indepth working knowledge of dynamic fluid systems, to acquire necessary skills to expand the research program into this area, and to develop innovative research methods applicable to these systems. Activities will concentrate on processes and mechanisms associated with fluid motion, emphasis of concepts describing transport theory, the physics of fluid dynamics, the mathematical tools and constructs required to formalize the problem, and the computational and numerical techniques necessary to obtain and visualize the results. Integration of fluid dynamics, with traditional mineralogic approaches and theoretical methods from aqueous geochemistry and irreversible thermodynamics, will more fully permit the explanation and prediction of chemical alteration caused by flow of fluids.

提议将流体动力学，热量和传质的原理与矿物和水性化学知识结合在一起。 最终，这将导致一种综合方法，该方法是关于由于流体流动引起的状态条件变化以及这种过程的物理表现而导致的矿物和流体的行为。 鉴定和定量流体循环中涉及的主导因素可以预测和描述最剧烈的液体矿物质反应发生在哪里。 流体动力学的整合将有望导致流体矿物系统中发现的新创新方法和发现前沿。 拟议的活动旨在获得动态流体系统的深入工作知识，以获取必要的技能，以将研究计划扩展到该领域，并开发适用于这些系统的创新研究方法。 活动将集中在与流体运动相关的过程和机制上，强调描述运输理论的概念，流体动力学的物理学，正式化问题所需的数学工具和构造以及获得和可视化结果所需的计算和数值技术。 流体动力学的整合，传统的矿物学方法以及来自水性地球化学和不可逆热力学的理论方法，将更充分地允许解释和预测流体流动引起的化学改变。