Experimental constraints on the equilibrium hydrogen isotopic composition and rates of hydrogen isotopic exchange of C-H bonds in natural gas

天然气平衡氢同位素组成和C-H键氢同位素交换速率的实验约束

• 批准号: 1911296
• 负责人: Daniel Stolper
• 金额: $ 37.92万
• 依托单位: University of California-Berkeley
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2019
• 资助国家: 美国
• 起止时间: 2019-08-01 至 2024-07-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1911296&HistoricalAwards=false
• 关键词: Experimental; constraints; equilibrium; hydrogen; isotopic

Natural gas is a key part of the US's economy. Methane is also a greenhouse gas and product and food source for life. Tracking methane sources and sinks is used in energy exploration, climate science, and biosciences. One of the main ways that natural gas sources are found is by measurement of carbon and hydrogen stable isotope values but use of isotope ratios to identify gas sources requires that those ratios do not change during gas accumulation and storage in the Earth. But whether this is true is not well known. The proposed work will measure rates of hydrogen isotope exchange and the final equilibrium values under laboratory conditions. This will be used to evaluate conditions where hydrogen isotope ratios could change in the earth. This information will be useful to a variety of groups including earth scientists, energy companies, and atmospheric scientists working to identify natural gas sources. This work will only become more broadly applicable as the US continues to extract natural gas from shale and exports it. The project will train one graduate student and will offer research opportunities to undergraduate students through established programs at UC Berkeley, and the will be highlighted at the annual "Cal" Day event where research on campus is shared with the community.Critical to the use of natural gas hydrogen isotopic compositions as a fingerprint for gas origins is the necessary assumption that isotopic compositions of samples are not modified post formation. This could occur due to hydrogen isotope-exchange reactions occurring in the subsurface after gas formation but before sampling. Problematically, the conditions under which natural gas undergoes hydrogen isotope exchange reactions at relatively low temperatures in Earth's near surface (200oC) is poorly constrained. To be able to evaluate whether such exchange reactions actually occur in nature and influence natural gas hydrogen isotopic compositions requires: (i) Knowledge of the rates of hydrogen isotope exchange of these gases with common hydrogen bearing molecules such as water at relevant natural conditions; and (ii) The equilibrium isotopic composition between alkanes and potential hydrogen-isotope exchange partners, the value of which determines the final isotopic composition of the natural gases undergoing hydrogen isotope exchange. To date, both the rates of hydrogen isotope exchange and the expected equilibrium compositions are poorly known for alkane gases at low temperatures (200oC). But knowledge of such are necessary for a complete understanding of what measured hydrogen isotopic compositions of natural gas in low temperature environments reflect about source vs. post-formational histories. To this end, a series of experiments will be conducted that are designed to establish experimentally: (i) the expected equilibrium dependence of hydrogen isotopic distributions for C1-C4 alkane gases from 25-250oC, including for methane clumped isotopes and (ii) the rates of exchange of C1-C5 alkanes with water at multiple temperatures such that the rates of exchange can be extrapolated to low temperatures for geologically relevant systems. The methodologies that will be used to accomplish these tasks are: (1) The use of catalysts to equilibrate hydrocarbons with H2 gas; (2) Heating of gases with water in gold cell reactors at elevated temperature and pressures; And (3) measurement of the isotopic composition of the hydrocarbons from all experiments. This work will provide the new constraints on what sets the hydrogen isotopic composition of natural gas undergoing isotope exchange reactions with water as well as what the isotopic compositions will be once the gases are in hydrogen isotopic equilibrium.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.

天然气是美国经济的重要组成部分。甲烷也是一种温室气体，也是生命的产物和食物来源。追踪甲烷的来源和汇用于能源勘探、气候科学和生物科学。发现天然气来源的主要方法之一是通过测量碳和氢的稳定同位素值，但使用同位素比率来确定气源要求这些比率在地球的天然气聚集和储存过程中不发生变化。但这是否属实尚不得而知。这项工作将在实验室条件下测量氢同位素交换率和最终平衡值。这将用于评估地球上氢同位素比率可能发生变化的条件。这些信息将对包括地球科学家、能源公司和致力于确定天然气来源的大气科学家在内的各种团体有用。随着美国继续从页岩中提取天然气并将其出口，这项工作只会变得更广泛适用。该项目将培养一名研究生，并将通过加州大学伯克利分校的既定项目为本科生提供研究机会，并将在一年一度的“加州”日活动中得到强调，届时校园研究将与社区分享。使用天然气氢同位素组成作为天然气来源指纹的关键是必要的假设，即样品的同位素组成在形成后没有改变。这可能是由于氢气同位素交换反应发生在天然气形成后的地下，但在采样之前。问题是，在地球近表面相对较低的温度（200摄氏度）下，天然气进行氢同位素交换反应的条件很少受到限制。为了能够评价这种交换反应是否在自然界中实际发生并影响天然气氢同位素组成，需要：(i)了解在相关自然条件下这些气体与水等常见含氢分子的氢同位素交换率；烷烃和潜在氢同位素交换伙伴之间的平衡同位素组成，其值决定了经过氢同位素交换的天然气的最终同位素组成。迄今为止，对于烷烃气体在低温（200℃）下的氢同位素交换速率和预期的平衡组成都知之甚少。但是，要全面了解低温环境下测量的天然气氢同位素组成所反映的来源与后地层历史，这些知识是必要的。为此，将进行一系列实验，旨在通过实验确定：(i) 25-250℃范围内C1-C4烷烃气体氢同位素分布的预期平衡依赖性，包括甲烷团块同位素；（ii） C1-C5烷烃与水在多个温度下的交换速率，以便可以将交换速率外推到地质相关系统的低温。将用于完成这些任务的方法是：(1)使用催化剂使碳氢化合物与H2气体平衡；（二）在高温高压下，在金电池反应器中加水加热气体；(3)测定各实验烃类的同位素组成。这项工作将为天然气与水发生同位素交换反应时的氢同位素组成以及气体达到氢同位素平衡后的氢同位素组成提供新的约束条件。该奖项反映了美国国家科学基金会的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。

项目成果

Experimental determination of hydrogen isotope exchange rates between methane and water under hydrothermal conditions

• DOI: 10.1016/j.gca.2022.04.029
• 发表时间: 2022-05
• 期刊: Geochimica et Cosmochimica Acta
• 影响因子: 5
• 作者: Andrew C. Turner;N. Pester;M. Bill;M. Conrad;K. Knauss;D. Stolper