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Estudo experimental da interação CO2 - rocha - fluido nas Formações Furnas e Ponta Grossa da Bacia do Paraná

机译:巴拉那盆地富尔纳斯和蓬塔格罗萨地层中二氧化碳与岩石-流体相互作用的实验研究

摘要

The world's dependence on fossil fuels for power generation is causing an increase in the atmosphere CO2 concentration and leading to global warming. Alternatives are being developed to stabilize or even to reduce the CO2 levels in the atmosphere. Among them stands out the Carbon Geological Storage, which consists of storing permanently CO2 in suitable geological reservoirs and thus mitigate climate change. In this sense, the study of CO2 - rock - fluid interactions is essential for the understanding of the processes involved during the storage phase and safety of storage. This work aims to study caprocks and reservoir rocks from the Furnas and Ponta Grossa Formations of the Paraná Basin for carbon geological storage. The interaction between CO2-rock-fluid was studied simulating the geological conditions in laboratory experiments with high pressure (150 bar) reactors. Rock characterization pre-and postexperiments analyzes in Scanning Electron Microscope (SEM) and X-ray Diffractometer (XRD) were performed. Analysis of saline solution before and after the experiment was performed by Optical Emission Spectroscopy Inductively Coupled Plasma (ICP - OES) to identify ions present in solution. The results of this work demonstrated that the tested reservoirs and caprocks have limited interactions with CO2 resulting in limited mineral trapping mechanisms and high mineralogy integrity.
机译:世界对化石燃料发电的依赖正在导致大气中二氧化碳浓度的增加,并导致全球变暖。正在开发替代方案来稳定甚至降低大气中的二氧化碳水平。其中最突出的是碳地质储藏,其中包括将二氧化碳永久存储在合适的地质储层中,从而减轻气候变化。从这个意义上讲,CO2-岩石-流体相互作用的研究对于理解存储阶段涉及的过程和存储安全至关重要。这项工作旨在研究巴拉那盆地Furnas和Ponta Grossa地层的盖层和储集层岩石,以进行碳地质储藏。在模拟高压(150 bar)反应堆的实验室实验中,研究了CO2岩石流体之间的相互作用,以模拟地质条件。在扫描电子显微镜(SEM)和X射线衍射仪(XRD)中进行了岩石表征实验前后的分析。实验前后的盐溶液分析是通过光发射光谱电感耦合等离子体(ICP-OES)进行的,以鉴定溶液中存在的离子。这项工作的结果表明,测试的储层和盖层与二氧化碳的相互作用有限,从而导致有限的矿物捕获机制和较高的矿物学完整性。

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    Bressan Lia Weigert;

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  • 年度 2014
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  • 原文格式 PDF
  • 正文语种 Português
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