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Impact of Chemical Osmosis on Brine Imbibition and Hydrocarbon Recoveryin Liquid-Rich Shale Reservoirs

机译:化学渗透对盐水吸收和碳氢化合物回收液液体丰富的页岩储层的影响

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We present an assessment of the impact of low-salinity brine osmosis on oil recovery in liquid-rich shalereservoirs.The paper includes:(1)membrane behavior of shales when contacted by low-salinity brine,(2)numerical model of osmosis mass transport for low-salinity brine,and(3)enhanced oil recovery(EOR)potential of low-salinity osmosis in liquid-rich shale reservoirs.Capillary osmosis causes low-salinity brine to be imbibed into the shale matrix;thus,forcing expulsionof oil from the rock matrix.This oil recovery process is described by a multi-component mass transportmathematical model consisting of advective and molecular transport of water molecules and dissolved ions.In the transport model,the activity-corrected diffusion of the brine solution is used to calculate the volumeof brine imbibed into a shale core sample and the resulting expelled oil.We used the mathematical modelto match oil recovery from two carefully designed brine-imbibition experiments conducted at ColoradoSchool of Mines.We have concluded that,in oil-wet shale reservoirs,low-salinity brine invasion of the rock matrix is byosmosis rather than capillary force.Thus,osmosis is the only imbibing force that drives the low salinitybrine into the reservoir rock matrix.Furthermore,we believe brine osmosis can potentially enhance oilrecovery by expelling oil out of the rock matrix and into the micro-and macro-fractures existing in thestimulated reservoir volume.
机译:我们对低盐度盐水渗透对富含液体的ShalereservoIr中的采油的影响进行了评估。本文包括:(1)在低盐度盐水,(2)渗透量传输的数值模型时,Shales的膜行为对于低盐度盐水,(3)富含液体的页岩储层中低盐度渗透的增强的储存(EOR)潜力。渗透性渗透性导致低盐度盐水被吸收到页岩基质中;因此,强迫油开采该岩石基质。该油回收过程由水分子的平均和分子输送和溶解离子组成的多组分质量转运mathematicalication模型。在运输模型中,盐水溶液的活性校正扩散用于计算盐水吸收到页岩芯样品中,由此产生的排出的油。我们使用了数学模型与在Coloradoschool的两个精心设计的盐水吸入实验中匹配油回收矿山的总结说,在油湿页岩储层中,低盐度盐水侵袭的岩石基质是口鼻肌,而不是毛细管力量。渗透是驱动低盐度进入储层基质的唯一的岩石基质。 ,我们认为盐水渗透可以通过将油从岩石基质中排出并进入存在于模拟的储层体积中的微生物和宏观 - 骨折,静脉渗透可能会增强油脂过激。

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