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Characterizing the Geochemistry of the CO_2-Fluid-Shale Interface using In-Situ Infrared Spectroscopy and Feature Relocation Scanning Electron Microscopy

机译:使用原位红外光谱和特征搬迁扫描电子显微镜表征CO_2-流体界面的地球化学的地球化学

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1. CO_2 sorption occurs in: 1.1 Micro-porosity of the organic fraction 1.2 Surfaces and internal layers of clay minerals 2. Carbonate Reactions 2.1 Exposure to CO_2 initiates carbonate precipitation and dissolution until equilibrium is reached 2.2 Possible buffering due to pH changes 3. Surface Effects 3.1 Dry CO_2 exposure 3.1.1 Etching, pitting, and minor precipitation 3.2 Wet CO_2 exposure 3.2.1 Heavy etching and pitting.
机译:1.1℃的含量为:1.1有机级分的微孔隙率1.2表面和粘土矿物的内层2.1碳酸酯反应2.1暴露于CO_2,引发碳酸盐沉淀并溶解直至由于pH变化而达到平衡2.2可能的缓冲。表面效果3.1干CO_2曝光3.1.1蚀刻,点蚀,轻微沉淀3.2湿CO_2曝光3.2.1重型蚀刻和蚀。

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