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Effect of temperature on the geological sequestration of CO_2 in a layered carbonate formation

机译:温度对二碳酸酯形成中CO_2地质螯合的影响

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Geological sequestration of CO_2 is one of the most promising technologies for large-scale CO_2 mitigation. To assess the suitability of a potential CO_2 storage site, we must understand the thermodynamics and kinetics of the CO_2-brine-rock system under the relevant conditions. Temperature can play a significant role in geochemistry, because it can affect phase equilibria in a multicomponent system and can impact reactive transport processes during geological carbon storage. In this study, we have assessed the effect of formation temperature on geological storage in a heterogeneous carbonate formation. The objectives of the numerical study are to quantitatively estimate the effect of temperature on 1) storage efficiency; 2) solubility trapping of CO_2 3) change in pH of residual brine; 4) changes in the mineralogy and porosity. Using TOUGHREACT 3.3 (a reactive transport simulator), we have estimated the changes in physical and chemical properties of a layered carbonate formation as a function of temperature. Mineralogy and physical properties of the aquifer are based on the Dollar Bay formation, a limestone dolomitic aquifer located within the South Florida Basin. We ran simulations for seven values of temperature, 35, 45, 55, 65, 75, 85 and 95°C. Results from the study suggest that density of supercritical CO_2 decreases with increase in temperature which leads to higher buoyancy at elevated temperatures. Therefore, storage efficiency of the aquifer decreases as temperature increases. For instance, an increase in temperature from 35°C to 95°C results in 65% decrease in storage efficiency. However, solubility trapping of CO_2 increases with an increase in temperature because the interfacial area increases with temperature. After the simulation period, pH drop was slightly more in case of higher temperature conditions. Temperature effect on porosity change was minimal and non-significant. The study can be helpful in screening a reservoir for geological carbon storage based on initial formation temperature.
机译:CO_2的地质封存是大规模CO_2缓解最有前途的技术之一。为了评估潜在的CO_2存储场所的适用性,我们必须在相关条件下了解CO_2-盐水岩系统的热力学和动力学。温度可以在地球化学中发挥重要作用,因为它可以影响多组分系统中的相平衡,并且可以在地质碳储存过程中冲击反应性运输过程。在这项研究中,我们评估了形成温度对非均相碳酸酯形成的地质储存的影响。数值研究的目的是定量地估计温度的储存效率的影响; 2)溶解度诱捕CO_2 3)残留盐水pH值的变化; 4)矿物学和孔隙度的变化。使用抗硬化3.3(反应性运输模拟器),我们估计了作为温度函数的分层碳酸盐形成的物理和化学性质的变化。含水层的矿物学和物理性质基于美元湾形成,位于佛罗里达州南部南部的石灰石白云岩含水层。我们耗尽温度,35,55,55,65,75,85和95°C值的仿真。研究结果表明,超临界CO_2的密度随着温度的增加而降低,导致高温下的浮力更高。因此,随着温度的增加,含水层的储存效率降低。例如,从35℃至95℃的温度的增加导致储存效率降低了65%。然而,由于界面面积随温度增加而增加,CO_2的溶解性俘获随着温度的增加而增加。在仿真期后,在温度较高的情况下,稍微稍微升级。对孔隙率变化的温度效应最小且不显着。该研究可以有助于筛选基于初始形成温度的地质碳储存库。

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