Collaborative Research: Modeling Coupled Reactive Flow at the TAG Active Hydrothermal Mound

合作研究：模拟 TAG 活跃热液丘的耦合反应流

• 批准号: 1029290
• 负责人: Margaret Tivey
• 金额: $ 12.17万
• 依托单位: Woods Hole Oceanographic Institution
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2010
• 资助国家: 美国
• 起止时间: 2010-08-15 至 2015-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1029290&HistoricalAwards=false
• 关键词: Collaborative; Research; Modeling; Coupled; Reactive

From their first discovery in the late 1970's, seafloor hydrothermal vent systems have been an intensive area of study in terms of characterizing the chemistry of their fluids, the biology that thrives around them, and the unique chimney structures that grow from the minerals precipitating from the fluids coming out of the seafloor. Predicting sub-seafloor fluid flow pathways and the dynamics of how these systems operate and evolve in the subsurface, however, still remains elusive due the paucity of holistic mathematical models of the chemical and physical processes that drive these systems. This research develops 2-D and 3-D mathematical models of fluid flow and reactive transport in high temperature mid-ocean ridge seafloor hydrothermal systems. Resulting models take into account mineral dissolution and precipitation and how these change basement permeability, fluid flow, and flow pathways. Goals are to test various hypotheses about what controls the distribution of focused and diffuse flow in high temperature seafloor hydrothermal systems, the extent of mineral precipitation, and the thermal/chemical conditions in the subsurface. The RST2D software package and modifications to it will be used to model the systems. The codes will permit fully-coupled reactive-flow investigations to be carried out which can examine the sensitivity of mid-ocean ridge hydrothermal vent systems to crustal structure, permeability, thermal conductivity, chemical dispersivity, and other geologic variables. Broader impacts of the work include integration of research and education and training graduate students in computational geoscience. Software that will be created during the course of the project builds infrastructure for science and has crossover potential to other fields, such as geothermal energy production and ore deposits. It will be made publicly available over the web. Results of the project will be presented to the public via lectures by participating faculty. The project will also support a PI from a gender under-represented in the sciences.

自1970年代末首次发现海底热液喷口系统以来，该系统一直是一个深入研究的领域，其研究内容包括其流体的化学性质、在其周围生长的生物以及从海底流出的流体中沉淀出的矿物所形成的独特烟囱结构。 然而，由于缺乏驱动这些系统的化学和物理过程的整体数学模型，预测海底下流体流动路径以及这些系统如何在地下运行和演变的动态仍然是难以捉摸的。 本研究建立了高温洋中脊海底热液系统中流体流动和反应输运的二维和三维数学模型。 由此产生的模型考虑到矿物溶解和沉淀，以及这些如何改变基底渗透性，流体流动和流动途径。 目标是测试有关控制高温海底热液系统中聚焦流和扩散流分布、矿物沉淀程度以及地下热/化学条件的各种假设。 RST 2D软件包及其修改将用于系统建模。 这些守则将允许进行充分耦合的反应流调查，从而可以检查大洋中脊热液喷口系统对地壳结构、渗透性、导热性、化学分散性和其他地质变量的敏感性。这项工作的更广泛的影响包括研究和教育的一体化以及对计算地球科学研究生的培训。 在项目过程中创建的软件将为科学建立基础设施，并具有与其他领域（如地热能生产和矿床）交叉的潜力。 该报告将在网上公布。该项目的结果将通过参与教师的讲座向公众展示。 该项目还将支持来自科学领域代表性不足的性别的主要研究者。