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Modeling Seafloor Hydrothermal Systems: Integrated Magma-Hydrothermal Processes and Temporal Variability

Modeling Seafloor Hydrothermal Systems: Integrated Magma-Hydrothermal Processes and Temporal Variability
海底热液系统建模:集成岩浆热液过程和时间变化
批准号:
0527208
负责人:
Robert Lowell
金额:
$0.0万
依托单位国家:
美国
项目类别:
Continuing Grant
财政年份:
2005
资助国家:
美国
项目状态:
已结题
起止时间:
2005-11-01 至 2009-10-31

项目摘要

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中文摘要
翻译
该项目是开发海底热液过程的可靠的、创新的数学模型的努力的继续。 该项目的综合过程部分涉及跨越基底边界层的热传递、岩墙扩展及其与热液循环的耦合以及开发包括开放系统岩浆透镜中对流在内的岩浆-热液过程综合模型等基本方面。 时间变化部分讨论了分层介质中渗透率的演变以及集中流和扩散流之间的关系、热液系统对地震的响应以及微生物-热液相互作用。
英文摘要
AbstractLowell 0527208 This project is a continuation of an effort to develop robust, innovative mathematical models of seafloor hydrothermal processes. The Integrated Processes part of the project addresses fundamental aspects of heat transfer across the basal boundary layer, dyke propagation and its coupling to hydrothermal circulation, and the development of an integrated model of magma-hydrothermal processes that includes convection in an open-system magma lens. The Temporal Variability part addresses the evolution of permeability in layered medium and the relationship between focused and diffuse flow, the hydrothermal system response to earthquakes, and microbial-hydrothermal interactions.
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Collaborative Research: Heat Flow and Hydrothermal Transport in the Panama Basin Linked with Geophysical and Oceanographic Data
Collaborative Research: Serpentinization of oceanic crust: Integrated modeling of deformation, fracture, fluid flow, and heat transfer
Collaborative Research: Coupled Thermal-Hydrological-Mechanical-Chemical-Biological Experimental Facility at DUSEL Homestake
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