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DIRECT EXPERIMENTAL EVIDENCE OF WETTABILITY MODIFICATION BY LOW SALINITY

机译:低盐度润湿性改性的直接实验证据

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It has been observed by several parties in the past years that injection of low salinity water leads to the production of additional oil compared to injection of water at reservoir salinity or higher. While this process is already applied in the field, so far the microscopic mechanism is not fully clear. A mechanism proposed by several researchers is that low salinity water leads to a wettability change of the sandstone rock, which then causes release of oil that previously was attached mostly to clay minerals. So far all experimental evidence for this mechanism is macroscopic and indirect, i.e. in the form of an increase in produced oil. The main motivation for this study is to provide direct evidence and to directly visualize detachment of crude oil from clay minerals. In a small lab scale experimental study in a flow cell we observed the release of crude oil from a substrate covered with solidly attached clay particles when changing the brine from high salinity to low salinity. For very low salinity we observed a massive release of crude oil (up to 80%) but also a decomposition of the Montmorillonite clay minerals and release of fines (formation damage). For a brine composition with somewhat higher salinity and in addition presence of divalent ions, we observed release of oil but only insignificant amount of clay swelling ("controlled formation damage").
机译:在过去几年中,若干方面已经观察到,注射低盐度水导致储层盐度或更高的水相比产生额外的油。虽然这个过程已经应用于该领域,但到目前为止,显微镜机制尚不清楚。几种研究人员提出的机制是低盐度水导致砂岩岩的润湿性变化,然后砂岩岩的润湿性变化,然后导致预先附着在粘土矿物上的油的释放。到目前为止这种机制的所有实验证据都是宏观和间接的,即,以生产的油的增加的形式。本研究的主要动机是提供直接证据,直接可视化粘土矿物质的原油分离。在流动细胞中的一个小实验室规模实验研究中,我们观察到在从高盐度到低盐度的盐水到低盐度时,观察到从覆盖的粘土颗粒覆盖的基材中释放原油。对于非常低的盐度,我们观察到大量释放的原油(高达80%),但也是蒙脱石粘土矿物的分解,并释放细粉(形成损伤)。对于具有稍微较高盐度的盐水组合物和除了二价离子的存在,我们观察到释放油,但只有微不足道的粘土溶胀(“受控地层损伤”)。

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