渗透作为低矿化度提高采收率机理的实验研究

Erik Norrud Pollen, C. Berg
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引用次数: 12

摘要

本文的目的是描述研究渗透作为低矿化度提高采收率(EOR)机制的实验。为此,设计了一项实验,旨在通过渗透诱导的原生水膨胀来提高采收率,同时降低其他低盐度机制的贡献。还考虑了实现与水库温度下的预期相媲美的渗透输水率。提高采收率与表面体积比之间的相关性特别令人感兴趣。由于渗透压梯度发生在与孔隙大小相当的距离上,因此由渗透引起的流体重新分配可能会导致相当局部的石油重新分配,从而对油田的总体提高采收率产生很小的影响。然而,在暴露的表面附近,这种局部再分配可能导致石油生产。以前对渗透作为潜在的低盐度机制的研究包括可视化实验,在渗透梯度影响下的水输送和油运动已经被观察到。我们的实验旨在增加对渗透在小规模低盐度实验结果和现场低盐度驱油中的相对重要性的理解。在实验中,不同表面体积比的油湿砂岩样品被高矿化度水和油饱和至不可还原水饱和度。样品首先在高盐度水中自然吸收,然后在低盐度水中自然吸收。记录了低矿化度自发渗吸产生的额外产油量,并与表面体积比进行了比较。实验进行了两次,分别在常温和高温下进行。在常温条件下,通过低矿化度自发渗吸,可使储层的产油量提高8-22%。在提高采收率和表面体积比之间没有发现明显的相关性。然而,增加的产油量与孔隙体积之间存在相关性。因此,低矿化度吸胀所增加的产油量似乎与孔隙体积成正比。高温下的实验结果表明,低矿化度自发渗吸提高产油量的数值较低,且该数值似乎与比表面积或孔隙体积无关。低响应被认为是由于样品在制备过程中反复加热和冷却的热效应引起的。我们的研究结果不能否认渗透是低矿化度提高采收率的重要机制。对于增加的产油量和孔隙体积之间的相关性,可能的解释是整个岩心的滞后和同时的原生水膨胀。
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Experimental Investigation of Osmosis as a Mechanism for Low-Salinity EOR
The objective of this paper is to describe experiments conducted to investigate osmosis as a mechanism for low-salinity enhanced oil recovery (EOR). For this purpose, an experiment was designed to facilitate enhanced oil recovery by osmosis-induced connate water expansion, while at the same time reducing the contributions of other proposed low-salinity mechanisms. Considerations were also made to achieve osmotic water transport rates comparable to what is expected at reservoir temperature. The correlation between enhanced oil recovery and the surface-to-volume ratio was of particular interest. Because the osmotic pressure gradients occur over distances comparable to the pore size, it is plausible that fluid redistribution due to osmosis would lead to a fairly local redistribution of oil, and thereby have a small impact on overall enhanced recovery in the field. However, near exposed surfaces, this local redistribution may result in oil production. Previous investigations of osmosis as an underlying low-salinity mechanism have consisted of visualization experiments, where water transport and oil movement under influence of osmotic gradients have been observed. Our experiments are intended to increase the understanding of the relative importance of osmosis in both small-scale low-salinity experiment results, and for field-scale low-salinity flooding. In the experiments, oil-wet sandstone samples with different surface-to-volume ratios were saturated with high-salinity water and oil to irreducible water saturation. The samples were first left to spontaneous imbibe in high-salinity water and afterward in low-salinity water. Additional oil production from spontaneous imbibition of low-salinity was recorded and compared with the surface-to-volume ratio. The experiment was performed twice, at both ambient and elevated temperatures. The experiments at ambient temperature resulted in increased oil production values of 8-22% of pore volume by low-salinity spontaneous imbibition. No clear correlation was found between increased oil recovery and the surface-to-volume ratio. A correlation was, however, seen between increased oil production and the pore volume. Thus, increased oil production by low-salinity imbibition seems to be proportionate to the pore volume. The experiments at elevated temperature resulted in low values of increased oil production by low-salinity spontaneous imbibition, and the values do not seem to correlate with either surface area or pore volume. The low response is believed to be caused by thermal effects from repeated heating and cooling of the samples during the preparations. Our results cannot dismiss osmosis as an important mechanism for low-salinity EOR. Possible explanations for the correlation between increased oil production and pore volume are hysteresis and simultaneous connate water expansion throughout the core.
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