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Monitor the process of shale spontaneous imbibition in co-current and counter-current displacing gas by using low field nuclear magnetic resonance method

机译:利用低场核磁共振法监测并流和逆流驱替气体中页岩的自吸过程

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Large scale fracturing fluid is injected into the formation to produce fractures for the effective development of shale reservoir. However, the flow back rate of fracturing fluid is often less than the half of the injected liquid, which causes large number of fracturing fluid retaining in the shale reservoir, thus aqueous phase trapping (APT) appears. But after well was shut in for a period of time, the APT can be auto-removed. The experiments that monitored the process of shale spontaneous imbibition in co-current and counter-current displacing gas combined with nuclear magnetic resonance (NMR) were performed. Results show that no matter whether the spontaneous imbibition of sandstone and volcanic rock happened in co-current or counter-current displacing gas, the water content increases in the whole pores range gradually, and no preferential pores for spontaneous imbibition appear. The water content increases with convex curve in the early period of both conditions. Simultaneously, in the process of the experiments no apparent micro cracks appeared on the surfaces of the sandstone and volcanic rock. However, shale has some special characteristics in spontaneous imbibition of both co-current and counter-current displacing gas, which may contribute to the auto-removal mechanism of shale reservoir APT. During the experiments of shale, lots of micro cracks appeared on the surface of the sample gradually. The liquid absorbed into the shale sample fills the micro pores firstly. Subsequently the water takes up the space of mesopores slowly. The liquid in the large pores of shale is too small to be detected, so the water content change in these pores couldn't be distinguished clearly. In the early period, the water content of shale increases with convex curve in the co-current displacing gas, while the water content of shale increases linearly in the counter-current displacing gas. Thus, the counter-current spontaneous imbibition condition is beneficial to protect the reservoir. The results of our study contribute to not only explaining the auto-removal mechanism of shale reservoir APT, but also fixing the optimal flow-back time after hydraulic fracturing. (C) 2015 Elsevier B.V. All rights reserved.
机译:大规模压裂液被注入到地层中以产生裂缝,以有效地开发页岩储层。但是,压裂液的回流速率通常小于注入液的一半,这导致大量的压裂液保留在页岩储层中,因此出现了水相捕集(APT)。但是在关井一段时间后,可以自动拆除APT。进行了监测并流和逆流置换气中页岩自发吸收过程并结合核磁共振(NMR)的实验。结果表明,无论是顺流还是逆流驱替气体发生砂岩和火山岩的自吸,整个孔隙范围内的含水量都逐渐增加,没有出现自吸的优先孔隙。在这两种情况的早期,含水量均以凸曲线增加。同时,在实验过程中,砂岩和火山岩表面未出现明显的微裂纹。但是,页岩在顺流和逆流驱替气体的自吸过程中都具有一些特殊的特征,这可能有助于页岩储层APT的自动清除机制。在页岩实验中,样品表面逐渐出现许多微裂纹。被页岩样品吸收的液体首先充满了微孔。随后,水慢慢占据了中孔的空间。页岩大孔隙中的液体太小而无法检测到,因此无法清楚地区分这些孔隙中的水分变化。早期,在并流驱替气中,页岩的含水量以凸曲线增加,而在逆流驱替气中,页岩的含水量线性增加。因此,逆流自吸条件有利于保护储层。我们的研究结果不仅有助于解释页岩储层APT的自动清除机理,而且有助于确定水力压裂后的最佳返排时间。 (C)2015 Elsevier B.V.保留所有权利。

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