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首页> 外文期刊>Advances in Water Resources >Evolution of pore-shape and its impact on pore conductivity during CO_2 injection in calcite: Single pore simulations and microfluidic experiments
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Evolution of pore-shape and its impact on pore conductivity during CO_2 injection in calcite: Single pore simulations and microfluidic experiments

机译:方解石CO_2注入过程中孔隙形状的演变及其对孔隙电导率的影响:单孔模拟和微流体实验

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Injection of CO2 into carbonate rocks causes dissolution and alters rock transport properties. The extent of the permeability increases, due to the increased pore volume and connectivity, strongly depends on the regimes of transport and dissolution reactions. Identification of these regimes and their parametrization at the microscopic scale is required for an understanding of the injection processes, and, afterward, for calculating the effective macroscopic parameters for field-scale simulations. Currently, a commonly used approach for calculating the rock effective parameters is the Pore Network Method, PNM, but a better understanding of the validity of its basic assumptions and their areas of applicability is essential. Here, we performed a combined microscopic experimental and numerical study to explore pore-shape evolution over a wide range of transport and dissolution reaction regimes. Experiments were conducted by flowing an acidic solution through a microscopic capillary channel in a calcite crystal at two different flow rates. The experimental results were used to validate our pore-scale reactive transport model that could reproduce the measured effluent composition as well as pore shape changes. Two key stages in pore shape evolution were observed, a transient phase and a quasi-steady-state phase. During the first stage, the shape of the single pore evolved very fast, depending on the flow regime. Under advective-dominant flow, the pore shape remained nearly cylindrical, while under diffusive-dominant transport, the pore shape developed into a half-hyperboloid shape. During the quasi-steady-state stage, the pore volume continued to increase, however, without or with diminutive change of the pore shape. In this stage, only a long period of injection may result in a significant deviation of the pore shape from its original cylinder shape, which is a common assumption in PNMs. Furthermore, we quantitatively evaluated the impact of evolved pore shape spectrum on the conductance calculations and compared it to the formulations currently used for pore network modeling of reactive transport. Under low flow rates, neglecting the developed non-uniform pore shape during the non-steady stage may lead to an overestimation of pore conductance up to 80%.
机译:将CO2注入碳酸盐岩石中会导致溶解并改变岩石的输送特性。由于增加的孔体积和连通性,渗透性的增加程度很大程度上取决于运输和溶解反应的方式。为了了解注射过程,以及随后为计算现场规模模拟的有效宏观参数,需要在微观尺度上识别这些状态及其参数化。当前,一种常用的计算岩石有效参数的方法是孔隙网络法(PNM),但必须更好地理解其基本假设的有效性及其适用范围。在这里,我们进行了组合的微观实验和数值研究,以探索在广泛的运输和溶解反应机制中孔隙形状的演变。通过使酸性溶液以两种不同的流速流过方解石晶体中的微观毛细管通道进行实验。实验结果被用来验证我们的孔尺度反应性传输模型,该模型可以重现所测量的废水成分以及孔的形状变化。观察到了孔形演化的两个关键阶段,一个过渡阶段和一个准稳态阶段。在第一阶段,取决于流动方式,单个孔的形状发展非常快。在对流占优势的流动下,孔的形状几乎保持圆柱形,而在扩散占优势的运输下,孔的形状发展为半双曲面形状。在准稳态阶段,孔体积继续增加,但是孔形状没有或没有微小变化。在此阶段,只有很长的注入时间可能会导致孔形状与原始圆柱形状发生明显偏差,这是PNM中的常见假设。此外,我们定量评估了演化的孔形谱对电导率计算的影响,并将其与当前用于反应性传输的孔网建模的配方进行了比较。在低流速下,在非稳定阶段忽略所形成的不均匀孔形状可能会导致高估孔导率,最高可达80%。

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