Hasan N. Al-Saedi, Ariel Williams, R. Flori, P. Brady, Soura K. Al-Jaberi
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引用次数: 4
摘要
最近,我们研究了地层水中Ca2+的影响及其对低盐度(LS)水驱的潜力(al - saedi et al. 2018)。在本文中,我们试图量化含有Ca2+和Mg2+的地层水对LS EOR的影响。Berean砂岩岩心在90℃条件下依次注入高矿化度HS水和LS水。在注入盐水过程中,对出水样品进行ph分析。Ca2+和Mg2+双浓度的采油实验表明,LS水效应较低,意味着岩心变得更水湿;然而,当HS水中Ca2+和Mg2+的含量减少一半时,LS水的效果要大得多。本工作的结果分离出了控制LS水化学机制的最有效因素,并将其与石油采收率联系起来。
Oil Recovery Analyses and Formation Water Investigations for High Salinity-Low Salinity Water Flooding in Sandstone Reservoirs
Recently, we investigated the effect of Ca2+ in the formation water and its potential on low salinity (LS) water flooding (Al-Saedi et al. 2018). In this paper, we pursue to quantify the influence of formation water containing Ca2+ and Mg2+ on LS EOR. Berean sandstone cores were sequentially flooded with high salinity HS water and LS water at 90°C. During injecting brines, samples of the effluent were analyzed for pH. Oil recovery experiments with a double Ca2+ and Mg2+ concentration showed a lower LS water effect, meaning that the cores became more water-wet; however, the LS water effect was much greater when the amount of Ca2+ and Mg2+ in the HS water was decreased by half.
The results of this work isolate and relate oil recovery with the most effective factors that control LS water chemical mechanisms.