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Experimental and Theoretical Study of Calcium Sulphate Precipitation in Porous Media Using Glass Micromode

机译:玻璃微模在多孔介质中硫酸钙沉淀的实验和理论研究

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Experimental and Theoretical Study of Calcium Sulphate Precipitation in Porous Media Using Glass Micromodel - Mixing of two incompatible waters in water injection projects is usually associated with mineral scale formation and deposition in porous media. Deposition process dramatically affects the performance of water injection scenarios by reduction of porosity and mainly permeability of the rock. In this study, a series of experiments has been conducted to investigate the effect of different parameters on the gradual process of Calcium Sulphate precipitation. These include temperature, concentration of mixing brines, pressure, and flow rate. Due to the visual nature of the glass micromodel, a glass sandstone pattern with water-wet characteristics was used as porous medium to easily observe the scaling formation and distribution. In addition, tracing the movement of the solid particles is highly facilitated in this newly suggested experimental setup. The captured photos in microscopy scanning show that the deposition is initiated from the walls of the pores and throats and extend toward the middle space of porous medium and solid crystals look like chicken roost. For better understanding of the effect of any aforementioned parameter, the related permeability reduction curve versus injected pore volume of the brine solutions was plotted. The results indicated that as the temperature, brine concentration, and flow rate increase the scaling tendency increases as well. The pressure has a minor role on the process development. Deposition of CaSO4 manifests a functional form of permeability reduction due to the effect of different parameters. Therefore, an exponential functionality (correlation) was proposed which incorporates all physical parameters that affect the behavior of the system in dimensionless form. Reynolds number, scaling index, and deviation from equilibrium conditions are the backbone of this correlation. The adjustable exponents of the equation was determined and optimized by means of Genetic Algorithm optimization scheme. This meaningful correlation can also predict the core extracted data with reasonable accuracy.
机译:用玻璃微模型对多孔介质中硫酸钙沉淀的实验和理论研究-注水项目中两种不相容水的混合通常与矿物垢的形成和在多孔介质中的沉积有关。沉积过程会通过降低孔隙率(主要是降低岩石的渗透率)而极大地影响注水方案的性能。在这项研究中,进行了一系列实验,以研究不同参数对硫酸钙沉淀逐渐过程的影响。这些包括温度,混合盐水浓度,压力和流速。由于玻璃微模型的视觉特性,使用具有水润湿特性的玻璃砂岩图案作为多孔介质,可以轻松观察结垢的形成和分布。另外,在这种新建议的实验装置中,追踪固体颗粒的运动非常方便。在显微镜扫描下捕获的照片显示,沉积是从孔和喉的壁开始的,并朝着多孔介质的中间空间延伸,固体晶体看起来像鸡的栖息地。为了更好地理解任何上述参数的影响,绘制了相关的渗透率降低曲线与盐水溶液的注入孔体积的关系。结果表明,随着温度,盐水浓度和流速的增加,结垢趋势也随之增加。压力对工艺开发的影响很小。由于不同参数的影响,CaSO4的沉积表现出渗透率降低的功能形式。因此,提出了一种指数功能(相关性),它以无量纲形式结合了影响系统行为的所有物理参数。雷诺数,缩放指数和偏离平衡条件是这种相关性的基础。利用遗传算法优化方案确定并优化了方程的可调整指数。这种有意义的关联还可以以合理的准确性预测核心提取的数据。

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