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Insights into Salinity Variations for Waterfloods,Frac-Fluids and Drilling Mud in Clay-Hosted Pores using Molecular Simulations

机译:使用分子模拟,粘土宿主毛孔中的水料,弗拉克流体和钻井泥浆的盐度变化的见解

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Clays,with their charged surfaces,are characterized by strong interactions with dissolved ions in brines,injected water,frac-fluids,and drilling mud-filtrate.While we do have strong evidence and science to address clay swelling,little to no progress has been made on fluid distributions and their impact on transport through clay-pores when exposed to fluids of varying salinity.In this work,we use a molecular dynamics approach to characterize fluid distributions when oil and water are present in clay-hosted pores and to finally provide guidelines for optimal salinities in our drilling mud,frac-fluid,and injected water.This work considers the distribution of oil and water at varying salinities in illite slit-pore systems because illite is the most common clay mineral.We use a wide range of concentrations(0-37000ppm NaCl)in these pores and quantify the surface electric potentials,electric double layers(EDL),mean square displacement(MSD),and ion hydration shells to model the interaction between clays,water,oil,and salts.The results indicate that at high salinity(above 16000ppm)Na+ and Cl-ions primarily adsorb on the clay surface due to the charge screening effect.The unabsorbed Na+ and Cl-ions appear as aggregates or within their hydration shell,which impedes oil flow.At low salinity(below 8100ppm),water bridges across the pore due to a strong surface potential that is not neutralized by the low salt concentration.These water bridges severely hamper the flow of any free water and oil.At intermediate values of salinity(8500-12400ppm),ionic aggregates are largely absent and water molecules merely adsorb on the surface of the pore.At these intermediate values of salinity,the mobility of the oil phase is the highest and constitutes the best range of salinity for the pore surface chemistry that we consider.This paper extends our understanding of the effect of salinity variations on fluid distribution and its impact on oil transport in clay pores.Prior work has largely focused on the impact of swelling but little has been done to understand the microscale phenomena such as water bridging and ion aggregation on fluid flow and storage.Our work provides optimal values of salinity that enhance oil mobility and therefore,provides insights into the design of low salinity waterfloods,frac-fluid,and drilling mud compositions for formations where clay may be present.
机译:带有带电表面的粘土,其特征在于盐水中溶解离子的强烈相互作用,注射水,弗拉克流体和钻井泥滤液。我们确实有强有力的证据和科学来解决粘土肿胀,而且没有进展则没有进展在暴露于不同盐度的流体的流体时,在流体分布和它们对通过粘土孔的影响。在这种工作中,我们使用分子动力学方法来表征油和水在托盘托管孔隙中并最终提供我们钻井泥浆,富污水和注射水中最佳盐水指南。本工作考虑了Illite Slit-Mystems的不同盐水中的石油和水的分布,因为伊利石是最常见的粘土矿物质。我们使用了广泛的这些孔隙中的浓度(0-37000ppm NaCl)并量化表面电位,电双层(EDL),平均方位(MSD)和离子水合壳,以模拟相互作用赌注威恩粘土,水,油和盐。结果表明,在高盐度(高于16000ppm)Na +和Cl-离子引起由于电荷筛选效果引起的粘土表面。未吸收的Na +和Cl-ions出现聚集体或在它们的水合壳内,其阻碍了油流量。低盐度(低于8100ppm),由于低盐浓度未被中和的强表面电位,孔穿过孔的水桥。这些水桥严重妨碍任何自由水的流动和油。盐度的中间值(8500-12400ppm),离子聚集体大大不存在,水分子仅吸附在孔隙的表面上。该中间值的盐度,油相的迁移率最高,构成了我们认为的孔隙表面化学的最佳盐度范围。本文延伸了我们对盐度变化对流体分布的影响的理解及其对粘土毛孔中的油运输的影响。有效的工作主要集中于关于肿胀的影响,但很少地了解微量现象,如水桥和流体流动和储存的离子聚集。我们的工作提供了增强油动性的最佳盐度,因此提供了对低盐度设计的见解用于粘土可以存在的地层的水灌木,弗拉克流体和钻井泥浆组合物。

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