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CO_2 Sequestration: Temperature and Gas compositional effects on the kinetics of mineralogical reactions

机译:CO_2封存:温度和气体成分对矿物学反应动力学的影响

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It may be possible to lower costs of Carbon Capture and Sequestration by keeping constituents such as sulfur dioxide (S02) in the flue gas stream. The reactive behavior of pure CO_2 and CO_2 + SO_2 mixtures within a geologically realistic environment was examined. The experimental apparatus consisted of a series of four high-pressure reactors operated at different conditions and with different feed gas compositions to observe changes in both the rock and water compositions. The rock consisted of equal proportions of quartz, calcite, andesine, dolomite, chlorite and magnesite (constituents in arkose or dirty sand stone). The brine was prepared from laboratory grade sodium chloride and by varying the amount of magnesium concentration in the brine. Several long term batch experiments with pure C0_2 were carried out at different temperatures. Each mineral in the mixture showed evidence of participating in the geo-chemical reactions. Layers of calcite were seen growing on the surface of the arkose. Analcime deposits were omnipresent, either occurring as large connected aggregates or as deposits on the surfaces of other minerals (Quartz). Ankerite and calcite depositions were observed as amorphous masses intergrown with the feed. The CO_2 + SO_2 mixture experiments showed growth of euhedral anhydrite crystals and pronounced dissolution patterns over the examined surfaces. The growth of these new phases would lead to significant changes in the petrophysical properties of the rock. The trends in ionic concentration changes in the aqueous phase complemented the changes in the rock chemistry. The rates of these reactions were computed by measuring the changes in the compositions of the initial and the final samples. The rates of these reactions were computed by computing the changes in the compositions of the initial and the final rock samples (both individual and mixture) provided by the XRD analyses and were observed to be lower than expected.
机译:通过将诸如二氧化硫(SO 2)中的成分保持在烟道气流中,可以降低碳捕获和螯合成本。检查了地质上现实环境中纯CO_2和CO_2 + SO_2混合物的反应性行为。实验装置包括在不同条件下操作的一系列四个高压反应器,并用不同的饲料气体组合物观察岩石和水组合物的变化。岩石由平等的石英,方解石,安肠,白云石,氯酸盐和菱镁矿组成(树脂或脏砂石的成分)。盐水由实验室级氯化钠制备,并改变盐水中的镁浓度的量。在不同的温度下进行几种具有纯CO_2的长期批量实验。混合物中的每种矿物都显示出参与地理化学反应的证据。看到方解石层在树脂表面上生长。 Analcime沉积物是无所不在的,要么在其他矿物质(石英)上发生大连接骨料或沉积物。观察阿基钛矿和方解石沉积作为用饲料楔入的非晶质量。 CO_2 + SO_2混合物实验显示出Euhedral残水石晶体的生长,并在检查表面上进行溶解图案。这些新阶段的生长将导致岩石的岩石物理特性发生重大变化。水相中离子浓度变化的趋势补充了岩石化学的变化。通过测量初始样品和最终样品的组合物的变化来计算这些反应的速率。通过计算由XRD分析提供的初始和最终岩石样品(个体和混合物)的组合物的变化来计算这些反应的速率,并且观察到低于预期。

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