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Enhancing the Observation of Above and Below Ground Carbon Sequestration Processes under In Situ Pressure and Temperature Conditions

机译:提高原位压力和温度条件下的上述碳封存过程的观察

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Developing a fundamental understanding of the chemical/geochemical reaction mechanisms associated with above-ground mineral sequestration and below-ground geological sequestration is essential to the development of viable processes for carbon mitigation. In situ observations under the pressure, temperature and activities present during sequestration are of particular interest. We have recently developed a microreaction system to observe sequestration reaction processes in situ via synchrotron X-ray diffraction and radiography, Raman spectroscopy, and optical microscopy. The system has been successfully applied to the investigation of above-ground aqueous mineral carbonation processes and is well suited to the investigation of reaction processes of interest to below ground sequestration as well. To complement the capabilities of the microreaction system, we have developed a novel high pressure NMR (HP-NMR) probe to further explore above and below ground sequestration processes under in situ temperature, pressure, and activity conditions of interest. Combined, these systems can provide insight into a variety of sequestration phenomena, including fluid-solid and fluid-fluid reaction mechanisms and interactions, fluid speciation, dissolution, and diffusion, and sequestration product phase stability and behavior. Initial observations of above ground aqueous mineral sequestration reactions have revealed (ⅰ) the relative carbonation reactivity of activated feedstock minerals, (ⅱ) the relative reactivity of fluid reaction species, and (ⅲ) the ability to identify carbonate phase formation and stability as a function of temperature, pressure, and aqueous solution activity, which is also of inherent interest for below ground sequestration. Extending these capabilities to explore the geochemistry associated with below ground sequestration is discussed, along with our initial observations of fluid speciation and transport of interest to above and below ground sequestration.
机译:制定对与地上矿物封存和低于地质封存相关的化学/地球化学反应机制的根本理解对于开发可加工的碳减缓过程至关重要。在封存期间存在的压力,温度和活性的原位观察特别感兴趣。我们最近开发了一种微孔系统,以通过同步X射线衍射和射线照相,拉曼光谱和光学显微镜观察原位螯合反应过程。该系统已成功地应用于对地面含水矿物质碳化过程的研究,并且非常适合于对低于地螯合的影响的反应过程。为了补充微孔系统的能力,我们开发了一种新的高压NMR(HP-NMR)探针,可进一步探索原位温度,压力和感兴趣的活性条件下的地下螯合过程。组合,这些系统可以提供对多种螯合现象的洞察,包括流体 - 固体和流体流体反应机制和相互作用,流体形状,溶解和扩散以及螯合产物相位稳定性和行为。上述水性矿物螯合反应的初始观察显示(Ⅰ)活性原料矿物的相对碳酸化反应性,(Ⅱ)流体反应物质的相对反应性,(Ⅲ)鉴定碳酸酯相形成和稳定性的能力温度,压力和水溶液活性,这也是低于地隔离的固有利息。讨论了这些能力来探索与地下封存相关的地球化学,以及我们对流体形态的初步观察和对地上封存的初始封存的初步观察。

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