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首页> 外文期刊>Journal of Petroleum Science & Engineering >Relative permeability as a function of temperature,initial water saturation and flooding fluid compositions for modified oil-wet chalk
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Relative permeability as a function of temperature,initial water saturation and flooding fluid compositions for modified oil-wet chalk

机译:相对油渗透率随温度,初始水饱和度和驱油液成分的变化

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This paper addresses the effect of brines,containing sulphate and magnesium(found in sea water)and distilled water as initial saturating and flooding fluids,on relative permeability of modified chalk cores by fatty acids to more oil-wet.A model oil system(n-decane)containing different fatty acids(present in oil)such as 18-phenyloctadecanoic acid(PODA-long chain fatty acid with unsaturated ring),Stearic acid(SA-saturated straight long chain),and brines containing sulphate and magnesium ions(0.03 M SO_4~(2-)and 0.06 M Mg~(2+))dissolved in distilled water are used.Fatty acids alter the wettability of chalk to more oil-wet.PODA shows higher tendency compared to SA,at the same concentration,to alter the chalk to more oil-wet.Relative permeability curves are used as indication of the modified chalk behaviour.It also addressed the effect of the temperature on the relative permeability.A shift in the relative permeability to the right side indicates more water-wet with temperature up to <=80 °C.At a higher temperature of 130 °C,the relative permeability curves indicate more oil-wet tendency.Wettability indicated by the relative permeability curves shows the influence of initially saturated fluid composition and the flooding fluid composition,where the modified cores initially saturated with ion free water(distilled water)and flooded by fluids containing Mg~(2+)or SO_4~(2-)shows a shift indicating more water-wet compared to reference core(initially saturated and flooded by ion free water).However,if the initial saturating and flooding fluids contain 0.06 M Mg~(2+)ions,the wettability tends to be more oil-wet compared to that if the modified cores are saturated and flooded with 0.03 M SO_4~(2-)and distilled water.The calculated pore size distribution index(lambda)using Huang and Honarpour correlation,is used to determine the corrected(actual)relative permeability for capillary end effect.A good agreement between experimental and simulated relative permeability data was also obtained by using the calculated lambda.
机译:本文探讨了盐水,硫酸盐和镁(存在于海水中)和蒸馏水(作为初始的饱和和驱替液)对脂肪酸改性的粉笔芯对更多油润湿的相对渗透率的影响。 -癸烷),其中包含不同的脂肪酸(存在于油中),例如18-苯基十八烷酸(带不饱和环的PODA长链脂肪酸),硬脂酸(SA饱和的直链长链)以及含硫酸盐和镁离子的盐水(0.03使用溶解在蒸馏水中的M SO_4〜(2-)和0.06 M Mg〜(2+))。脂肪酸改变白垩的润湿性使其更油润湿。在相同的浓度下,PODA的趋势比SA高。相对渗透率曲线被用作改进后的白垩特性的指示,还解决了温度对相对渗透率的影响,相对渗透率向右偏移表示更多的水-湿润,最高温度<= 80°在130°C的较高温度下,相对渗透率曲线显示出更多的油湿趋势。相对渗透率曲线表明的润湿性表明了初始饱和流体组成和驱油流体组成的影响,其中改性岩心最初被饱和离子水(蒸馏水)和含Mg〜(2+)或SO_4〜(2-)的流体驱油后,与参考堆芯相比(最初被离子水饱和并注满)表现出位移,表明水更湿。如果初始饱和和驱替液中含有0.06 M Mg〜(2+)离子,则与改性岩心饱和并用0.03 M SO_4〜(2-)和蒸馏水驱替的情况相比,润湿性往往更油润湿。利用黄和Honarpour相关性计算出的孔径分布指数(λ),用于确定校正后的(实际)相对渗透率以达到毛细管作用。实验和模拟相对渗透率数据之间也有很好的一致性通过使用计算出的lambda获得。

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