首页> 外文会议>International Technical Conference on Coal Utilization amp; Fuel Systems vol.1; 20050417-21; Clearwater,FL(US) >Enhancing the Observation of Above and Below Ground Carbon Sequestration Processes under In Situ Pressure and Temperature Conditions
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Enhancing the Observation of Above and Below Ground Carbon Sequestration Processes under In Situ Pressure and Temperature Conditions

机译:在现场压力和温度条件下加强对地面和地下碳固存过程的观察

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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:对与地上固存和地下地质固存有关的化学/地球化学反应机理有基本的了解对于开发可行的减碳工艺至关重要。在隔离过程中存在的压力,温度和活动下的现场观测尤为重要。我们最近开发了一种微反应系统,可通过同步加速器X射线衍射和射线照相,拉曼光谱和光学显微镜原位观察螯合反应过程。该系统已成功应用于地上含水矿物碳酸化过程的研究,也非常适合于对地下螯合感兴趣的反应过程的研究。为了补充微反应系统的功能,我们开发了一种新型的高压NMR(HP-NMR)探针,以进一步探索在感兴趣的原位温度,压力和活性条件下的地面和地下螯合过程。这些系统结合在一起,可以洞察各种螯合现象,包括液固和液流反应机理和相互作用,流体形态,溶解和扩散,以及螯合产物相的稳定性和行为。对地上水矿物螯合反应的初步观察表明(ⅰ)活性原料矿物的相对碳酸化反应性,(ⅱ)流体反应物种的相对反应性,以及(ⅲ)识别碳酸盐相形成和稳定性的函数温度,压力和水溶液的活性,这对于地下隔离也是固有的兴趣。讨论了扩展这些功能以探索与地下隔离相关的地球化学的方法,以及我们对流体形态和感兴趣的地下隔离和地下运输的初步观察。

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