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A Three-Phase Study on Pre-Flush Stage in SandstoneAcidizing:Experimental and Modeling Analysis of Evolved CO2 in an Oil andAqueous Environment

机译:砂铝化中的三相研究:油脂环境中进化二氧化碳的实验性和建模分析

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This paper presents a detailed study on the effects of evolved CO2 due to carbonate mineral dissolution,and its ensuing activity,during the preflush phase in matrix acidizing of sandstone reservoirs.Sandstoneacidizing in the presence of different rock saturations conditions is seldom investigated.The presence ofoil during preflush may change the perception of acid with carbonate minerals.The cores were acidized viacoreflood experiments and validated through simulation studies using three-phase numerical model.Theacid was injected into 100% brine saturated rock with 15 wt% hydrochloric acid(HCl)at a temperatureof 150 F and at a back-pressure of 1200 psi.This was done to calibrate and initially test the numericalmodel.The numerical model was able to match the performed coreflood experiments at different saturationconditions to a good level of accuracy.The HCl-calcite and HCl-dolomite chemical reaction parameterswere fixed in all cases to ensure consistency in analyses.Oil production was observed,with an average of25% recovery of the residual oil in place at pore pressures of 1,200 psi.The swelling of oil by the solubleCO2 was inferred as the main mechanism for additional oil production during the 15 wt% HCl injection.Adirect symmetry was observed between the oil recovery and average CO2 moles in the oil phase based on thenumerical model prediction of the conducted experiments.The recovery curve flattened once surroundingoil reached its full-saturation level with CO2.The successful capability of the numerical model to effectivelymimic the preflush stage sets a new bar in the area of sandstone acidizing.The potential of CO2,a by-productof acidizing,towards its contribution in swelling the surrounding oil,and thus mobilizing the trapped oilhas been depicted in this study.
机译:本文提出了对由于碳酸盐矿物溶解的进化二氧化碳的影响的详细研究,及其随后的活性期间在砂岩储层的基质酸化中的前级相期间。在不同岩石饱和条件下,很少调查。存在在预填充过程中,可以改变碳酸盐矿物的酸的感知。核心酸化通过使用三相数值模型通过模拟研究验证。用15wt%的盐酸(HCl)注入100%盐水饱和岩体中的仿真研究。 150 f和1200 psi的后压的温度。完成校准并最初测试数值模型。该数值模型能够将不同的静处理器的核心实验与良好的准确性水平相匹配。HCl-方解石和HCl-Dolomite化学反应参数在所有情况下固定,以确保分析中的一致性。油生产是观察到,平均孔隙压力在1,200 psi的孔隙压力下的25%恢复。溶解槽2的溶胀被推断为在15wt%HCl注射期间额外的油产生的主要机制。观察到对称性基于Doneumerical模型预测的油相的储存和平均CO2摩尔之间进行了进行的实验。随着CO2,恢复曲线扁平达到其全饱和水平。数值模型的成功能力达到了预填充阶段集的成功能力砂岩领域的一个新棒酸化。二氧化碳,酸化的潜力,酸化,促进其膨胀周围油的贡献,从而在本研究中描述了动员被困的油。

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