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CAS-Climate: Bubble generation and ripening in underground hydrogen storage

CAS-Climate: Bubble generation and ripening in underground hydrogen storage
CAS-气候:地下储氢中气泡的产生和成熟
批准号:
2348723
负责人:
Yashar Mehmani
金额:
$35.2万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2024
资助国家:
美国
项目状态:
未结题
起止时间:
2024-05-01 至 2027-04-30

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中文摘要
翻译
国际能源署(iea)将氢确定为本世纪中叶实现全球能源部门脱碳的关键支柱之一。这是因为大多数可再生能源(如风能和太阳能)都是间歇性的,需要在高产量期间储存,以确保在低产量期间的可用性。氢是一种很好的储存介质,但需要非常大的体积。地面设施和地下盐穴提供了一些容量,但不足以满足需要。由多孔岩石组成的深层地质构造是一种有前途的解决方案,因为它们提供了大容量,并在储存其他流体(例如,二氧化碳)。目前尚不清楚的是,在夏季注入的氢气中有多少可以在冬季回收,以及氢气纯度如何受到共注入流体(称为缓冲气体)的影响。季节性的注入-抽出循环可能会在岩石中产生并捕获许多氢气和甲烷气泡,随后通过称为奥斯特瓦尔德熟化的过程相互交换质量。两者都可能导致氢的损失和纯度降低。该奖项旨在了解控制与储氢相关的多组分气泡的捕获和成熟的基本机制。这种理解将有助于选择合适的地质储存地点和兼容的氢气。氢气被广泛认为是全球能源系统脱碳的关键支柱。为了缓冲风能和太阳能的大规模不稳定性负担,必须季节性地储存大量的氢。现有的解决方案(例如,罐和盐穴)不能提供所需的几乎足够的容量。在深层地层中的地质储氢满足了需求,但人们对氢如何与预先存在的和共同注入的流体(称为垫层气体)相互作用知之甚少。该奖项的目的是了解循环注入的多组分气体如何被困在多孔微结构中,以及它们如何通过扩散质量交换或奥斯特瓦尔德熟化而演变。提出了一个综合的实验和建模计划,以获得基本的见解:(1)在循环注入和取出过程中控制被困气泡的空间分布的因素;(2)气泡的大小,形状和成分如何演变,由于成熟;(3)集体气泡平衡如何影响宏观存储容量和多孔介质的流动阻力。该教育计划将培养一名博士生,并通过面对面/虚拟博物馆展览吸引服务不足的K-12学生。该奖项反映了NSF的法定使命,并通过使用基金会的智力价值和更广泛的影响审查标准进行评估,被认为值得支持。
英文摘要
The international energy agency identifies hydrogen as one of the key pillars for decarbonizing the global energy sector by mid-century. This is because most renewable energy sources such as wind and solar are intermittent, requiring storage during times of high production to ensure availability during times of low production. Hydrogen is an excellent medium for storage, but very large volumes will be required. Surface facilities and underground salt caverns provide some capacity, but not enough for what is needed. Deep geologic formations comprised of porous rocks are a promising solution because they offer large capacity with demonstrated success in storing other fluids (e.g., carbon dioxide). What is not well understood is how much of the hydrogen injected during summertime can be recovered during winter and how hydrogen purity is impacted by the presence of a co-injected fluid, called cushion gas. The seasonal injection-withdrawal cycles will likely generate and trap many hydrogen and cushion-gas bubbles in the rock that subsequently exchange mass with each other through a process known as Ostwald ripening. Both can contribute to the loss and purity degradation of hydrogen. This award aims to understand the basic mechanisms controlling entrapment and ripening of multicomponent bubbles relevant to hydrogen storage. This understanding will help select suitable geologic storage sites and compatible cushion-gasses.Hydrogen is widely regarded as a key pillar for decarbonizing the global energy system. To buffer the intermittency burden of wind and solar at scale, vast quantities of hydrogen must be stored seasonally. Existing solutions (e.g., tanks and salt caverns) do not provide nearly enough capacity for what is needed. Geologic hydrogen storage in deep formations meets the demand, but very little is understood about how hydrogen interacts with pre-existing and co-injected fluids, called cushion gas. The goal of this award is to understand how cyclically injected multicomponent gases become trapped within a porous microstructure and how they evolve through diffusive mass exchange, or Ostwald ripening. An integrated experimental and modeling plan is proposed to gain fundamental insights into: (1) the factors that control the spatial distribution of trapped bubbles during cyclic injections and withdrawals; (2) how bubble sizes, shapes, and compositions evolve due to ripening; and (3) how collective bubble equilibration impacts the macroscopic storage capacity and flow resistance of the porous medium. The educational plan will train one PhD student and engage underserved K-12 students through in-person/virtual museum exhibits.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
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CAREER: An Integrated Computational and Experimental Framework to Understand Deformation and Failure of Porous Materials
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