IDR: Collaborative Research: A Partnership for Multiscale Experimental Study of CO2 Leakage and Vertical Flow in Geologic Carbon Sequestration

IDR：合作研究：地质碳封存中二氧化碳泄漏和垂直流多尺度实验研究的伙伴关系

• 批准号: 1133849
• 负责人: Catherine Peters
• 金额: $ 54.65万
• 依托单位: Princeton University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-10-01 至 2015-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1133849&HistoricalAwards=false
• 关键词: IDR; Collaborative; Research; Partnership; Multiscale

1134397 Clarens/1133849 Peters Geologic carbon sequestration (GCS) is likely to play an important role in near-term efforts to provide carbon-neutral energy even though it has not yet been definitively demonstrated that CO2 injected into deep geologic formations will stay in place. This project assembles an interdisciplinary partnership to study the conditions that drive or inhibit leakage of CO2 through formation caprocks and the buoyancy-driven transport of CO2 through both caprocks and porous media. This integrated and multidisciplinary effort will generate experimental data to bridge the gap between bench-scale work on geochemical reactions and kilometer-scale simulations of GCS in the real world. Central to the proposed multiscale study are two novel high-pressure experimental test beds: a core-scale (cm-scale) vessel to study reaction and flow in caprock specimens (at Princeton), and a large-scale (6 m) pressurized column in which vertical flow of CO2 will be observed in sedimentary media (at the University of Virginia (UVA)). This approach will integrate experimental observation with two key tools for observation and inference: (1) a suite of lab- and synchrotron-based imaging methods to elucidate and quantify mineral reactions and alterations in pores/fractures (at Brookhaven National Lab (BNL)), and (2) reactive transport modeling to infer reaction rates, build predictive capacity, and conduct numerical experiments. The work is targeted to provide new insight critical to understanding the processes that will ultimately determine the viability of GCS. These processes are poorly understood because it is challenging to study reactions and two-phase flow in an integrated way, under high-pressure conditions, over realistic length scales. Reactions in heterogeneous media are best observed at small spatial scales (nm to μm), while flow is best observed over large scales (m to km). This project will elucidate the interrelation of these processes and provide answers to many of the persistent questions in the field such as: What are the conditions that lead to erosion or self-sealing of caprock flow paths? How do geochemical alterations of mineral surfaces alter CO2 flow? Will long-range buoyant CO2 flow be accelerated or decelerated by complexities in capillarity, viscosity, solubility, and Joule-Thomson cooling? These questions cannot be answered effectively by any single discipline. The project interdisciplinary team combines the expertise of an environmental engineer and expert in high-pressure fluid phase behavior (AFC), a geoenvironmental engineer with over a decade of experience in GCS research (CAP) and a geochemist with over 15 years of experience in advanced x-ray imaging techniques (JPF). This research will achieve broader impacts by identifying critical factors that determine the safe and effective sequestration of CO2 in deep geological reservoirs. The work will provide critical inputs to the effort of the United States to achieve the 2010 Presidential directive of overcoming the barriers to the widespread deployment of CCS within ten years. Furthermore, the experimental test beds constitute an investment in long-term study of CO2 flow and reaction in porous and fractured media. Lessons learned from these experiments can be applied to the design of larger facilities currently under development. The research also represents an effort to introduce global environmental change and carbon-neutral energy into the curricula at UVa and Princeton, and to use Brookhaven?s InSync outreach program to enable high school students to have remote access to experimental time at a synchrotron-based x-ray imaging facility.

1134397克拉伦斯/1133849彼得斯地质碳汇很可能在提供碳中性能源的近期努力中发挥重要作用，尽管目前还没有明确的证据表明，注入深层地质地层的二氧化碳将留在原地。该项目汇集了一个跨学科的伙伴关系，以研究通过地层盖层驱动或抑制二氧化碳泄漏的条件，以及通过盖层和多孔介质的浮力驱动的二氧化碳传输。这一综合和多学科的努力将产生实验数据，以弥合地球化学反应的实验室规模工作与现实世界中千米级的GCS模拟之间的差距。拟议的多尺度研究的中心是两个新的高压实验试验台：一个(厘米尺度)核心容器，用于研究盖层样品中的反应和流动(在普林斯顿)，以及一个大型(6米)加压柱，其中将在沉积介质中观察到二氧化碳的垂直流动(在弗吉尼亚大学(UVA))。这一方法将把实验观察与观察和推断的两个关键工具结合起来：(1)一套基于实验室和同步加速器的成像方法，以阐明和量化孔隙/裂缝中的矿物反应和变化(在布鲁克海文国家实验室(BNL))，以及(2)反应传输建模，以推断反应速率，建立预测能力，并进行数值实验。这项工作的目标是提供新的见解，这对理解最终将决定GCS生存能力的过程至关重要。对这些过程的了解很少，因为在高压条件下，在现实的长度尺度上，以综合的方式研究反应和两相流动是具有挑战性的。非均质介质中的反应最适合在小空间尺度(纳米到纳米)观察，而流动最好在大尺度(米到千米)观察。该项目将阐明这些过程的相互关系，并为该领域中的许多长期存在的问题提供答案，例如：导致盖层流动路径侵蚀或自封闭的条件是什么？矿物表面的地球化学变化是如何改变二氧化碳流动的？在毛细、粘度、溶解度和焦耳-汤姆逊冷却方面的复杂性会加速或减速长期浮力二氧化碳流动吗？任何一门学科都无法有效地回答这些问题。该项目的跨学科团队结合了一名环境工程师和高压流体相态(AFC)专家、一名在GCS研究(CAP)方面拥有十多年经验的地质环境工程师以及一名在先进X射线成像技术(JPF)方面拥有超过15年经验的地球化学家的专业知识。这项研究将通过确定决定深层地质储集层二氧化碳安全有效封存的关键因素来实现更广泛的影响。这项工作将为美国努力实现2010年总统指令，即在十年内克服广泛部署CCS的障碍提供关键投入。此外，实验试验台是对二氧化碳在多孔和裂隙介质中流动和反应的长期研究的投资。从这些实验中学到的经验教训可以应用于目前正在开发的更大设施的设计。这项研究还代表了一项努力，将全球环境变化和碳中性能源引入弗吉尼亚大学和普林斯顿大学的课程，并利用布鲁克海文？S InSync推广计划，使高中生能够远程访问基于同步加速器的X射线成像设备的实验时间。