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The Impact of Salinity on Water Dynamics, Hydrocarbon Recovery and Formation Softening in Shale: Experimental study

机译:盐度对页岩水动力学,碳氢化合物回收和形成软化的影响:实验研究

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The low reocvery of Slick water used in hydraulic fracturing treatments and the better performance observed for low salinity floods reveal the impact of water dynamics on well and reservoir performance. The focus of this study has been to develop and implement an experimental workflow to investigate the impact of water salinity on wettability, hydrocarbon recovery and formation softening in shale rock samples varying in mineralogy. We are trying to provide a better understanding of the mechanisms of water dynamics and entrapement along with the driving forces associated with these mechanisms. Samples from Woodford and Caney outcrops in the Unites States of America were obtained. The mineralogy of the cores was measured using the FTIR technique. While the Woodford samples turned out to be Dolomite rich, the Caney samples were Quartz and clay rich. Spontaneous imbibition and contact angle measurements were conducted for these samples using slickwater with an added KCl weight percentage of 0, 5 and 10. Both the rock-water-gas and the rock-water-oil systems were examined. The formation softening was quantified by recording the rock mechanical parameters before and after the imbibition and soaking tests. The results were analyzed in terms of the capillary suction characteristics for each formation. According to the experimental results, a positive correlation was observed between water salinity and imbibition in Caney formation. However, the opposite was observed for Woodford samples. The formation mineralogy was identified to be the major factor in this reversal of wettability. Similar trends were observed for the recovery of both oil and gas where the low salinity imbibition yielded a higher recovery factor for the Caney formation samples and a lower recovery factor for Woodford. In addition, tangible increase in the compressive strength of Caney formation was reported with the increase in KCl concentration. However, a non-monotonic trend was observed for Woodford samples. This study provides insights into the water dynamics in ultra-low permeability reservoirs. The formation mineralogy is a key factor for properly describing the water dynamics whether in fracturing treatments or in low salinity flooding projects. Low salinity flooding does not always imply better hydrocarbon recovery, based on what we observed in Woodford samples.
机译:用于液压压裂处理中使用的光滑水和低盐度洪水的更好表现的低回合揭示了水动力学对井和储层性能的影响。本研究的重点是开发和实施实验工作流程,以研究水上盐度对矿物学中变化不同的润湿性,碳氢化合物回收和形成软化的影响。我们正在努力提供与与这些机制相关的驱动力的水动力学和养雏机制更好地了解。获得了来自美国单位国家的伍德福德和甘甘露头的样本。使用FTIR技术测量芯的矿物学。虽然伍德福德样本原来是白云岩丰富的,但甘米样品是石英和粘土富含。使用光滑剂对这些样品进行自发性涂覆和接触角测量,其中克拉水的加入百分比为0,5和10。岩石 - 水 - 气体和岩石水 - 油系。通过在吸入和浸泡试验之前和之后记录岩石机械参数来定量形成软化。以每种形成的毛细吸力特性分析结果。根据实验结果,在水上盐度与甘蓝形成中的吸收之间观察到阳性相关性。然而,对于伍德福德样本观察到相反。鉴定了地层矿物学是这种逆转性的主要因素。观察到类似的趋势,用于恢复油气和气体,其中低盐度吸收产生甘米形成样品的更高恢复因子以及伍德福德的较低恢复因子。此外,据报道,KCl浓度的增加,报告了甘豆形成抗压强度的切实增加。然而,对于Woodford样品,观察了非单调趋势。本研究提供了对超低渗透储层中水动力学的见解。该形成矿物学是正确描述水动力学的关键因素,无论是压裂治疗还是低盐度泛滥项目。低盐度洪水并不总是暗示更好的碳氢化合物恢复,基于我们在伍德福德样本中观察到的。

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