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: Pennsylvania State Univ University Park
• 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
• 起止时间: 2024-05-01 至 2027-04-30
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2348723&HistoricalAwards=false
• 关键词: CAS; Climate; Bubble; generation; ripening

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.

国际能源机构将氢视为本世纪中叶全球能源部门脱碳的关键支柱之一。这是因为风能和太阳能等大多数可再生能源都是间歇性的，需要在高产量期间进行存储，以确保低产量期间的可用性。氢气是一种极好的储存介质，但需要大量的氢气。地面设施和地下盐洞提供了一定的容量，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很有前途的解决方案，因为它们具有很大的容量，并且在储存其他流体（例如二氧化碳）方面已被证明是成功的。目前尚不清楚的是，夏季注入的氢气有多少可以在冬季回收，以及共同注入的流体（称为缓冲气体）的存在如何影响氢气纯度。季节性的注入-回收循环可能会在岩石中产生并捕获许多氢气和缓冲气泡，这些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。两者都会导致氢气的损失和纯度下降。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缓冲气体。氢被广泛认为是全球能源系统脱碳的关键支柱。为了大规模缓冲风能和太阳能的间歇性负担，必须季节性储存大量氢气。现有的解决方案（例如储罐和盐穴）无法提供足够的容量来满足所需。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（称为缓冲气体）相互作用知之甚少。该奖项的目标是了解循环注入的多组分气体如何被困在多孔微观结构中，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。提出了一个综合实验和建模计划，以获得对以下方面的基本见解：（1）在循环注入和回收过程中控制捕获气泡空间分布的因素； (2) 气泡大小、形状和成分如何因成熟而演变； (3)集体气泡平衡如何影响多孔介质的宏观存储容量和流动阻力。该教育计划将培训一名博士生，并通过现场/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。