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Enhanced Heavy Oil Recovery by Thermal-Different Aqueous Ionic Solutions-Low Salinity Water Flooding

机译:通过热 - 不同的水性离子溶液 - 低盐水泛滥增强重油回收

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In this study, we propose to quantify a control of water chemistry on water-rock interactions and wettability alteration during Lo-Sal water-flooding of sandstone cores containing heavy oil. We intended to identify the dominant process of wettability alteration through considering all possible water-rock interaction mechanisms simultaneously. Water chemistry partially determines the dominant wettability alteration. This includes salinity, type of ions, and possibly pH. The effect of the potential determining ion towards sandstone ‘calcium ion’ is presented in this work. The ultimate oil recovery for the core saturated in normal Ca~(2+) concentration at higher temperature was higher than the core saturated with double Ca~(2+) at the same temperature. The divalent cation (Ca~(2+) ) concentration was then doubled in the aging water, resulting in a lower oil recovery. The thermal technique seems to be related to the chemistry of the water, meaning that the injected hot water must be tuned to the proper chemical composition. Desorption of Ca~(2+) is associated with pH jump and thereby increased microscopic sweep efficiency, and it seems to have a large impact on LS water EOR heavy oil.
机译:在这项研究中,我们建议量化含有重油砂岩芯的水岩相互作用和润湿性改变的水化学控制。我们旨在通过考虑所有可能的水岩相互作用机制同时识别润湿性改变的主导过程。水化学部分决定了主导的润湿性改变。这包括盐度,离子类型,并且可能是pH值。在这项工作中提出了潜在的确定离子对砂岩'钙离子'的影响。在较高温度下饱和在正常Ca〜(2+)浓度下饱和的核心的最终的油回收率高于同一温度下用双Ca〜(2+)饱和的芯。在老化水中加倍二价阳离子(Ca〜(2+))浓度,导致较低的溢油率。热技术似乎与水的化学有关,这意味着注入的热水必须被调节到适当的化学成分。 Ca〜(2+)的解吸与pH跳跃有关,从而增加显微扫描效率,并且似乎对LS水EOR重油产生了很大的影响。

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