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Experimental study of thermal-crack characteristics on hot dry rock impacted by liquid nitrogen jet

机译:液氮射流冲击热干岩石热裂纹特性的实验研究

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Liquid nitrogen jet fracturing is a novel stimulation technology, which is expected to be suitable for hot dry rock (HDR) reservoirs. Due to the large temperature difference between hot rock and cryogenic fluid, a great number of thermal cracks would be created during fracturing process, which is conductive to improve the penetration capacity of formation. In this study, a set of experiments were conducted to investigate the characteristics of thermal cracks. In these experiments, granite specimens with temperatures ranging from 200 degrees C to 300 degrees C were impacted by the low-pressure liquid nitrogen jet. The complexity and connectivity of cracks were quantitatively analyzed by a fractal method. The permeability and ultrasonic velocity of the granite specimens were tested in order to evaluate the damage conditions caused by thermal stress. Additionally, scanning electron microscope was adopted to analyze the microscopic characteristics of the thermal cracks. The results show that the heating process has a slight effect on thermal-crack generation compared with the liquid-nitrogen impact. The cracks mainly concentrate in the region near the impingement surface, due to the large temperature gradient there. The impacted rock breaks as the effects of tensile stress and shear stress. With an increase of initial rock temperature, the number of thermal cracks increases, and a more complex crack-network is formed in each specimen. Transient pulse evaluation and ultrasonic velocity measurements indicate that the impact of liquid nitrogen jet can improve the permeability and cause the damage of hot rock noticeably. This study demonstrates the important effect of thermal stress on crack generation during liquid nitrogen jet fracturing for HDR reservoirs, and the results shed light on the exploitation of HDR energy.
机译:液氮射流压裂是一种新颖的增产技术,有望适用于干热岩(HDR)储层。由于热岩与低温流体之间的温差较大,在压裂过程中会产生大量的热裂纹,有利于提高地层的渗透能力。在这项研究中,进行了一组实验以研究热裂纹的特征。在这些实验中,温度范围从200摄氏度到300摄氏度的花岗岩试样受到低压液氮射流的影响。用分形方法定量分析了裂纹的复杂性和连通性。测试了花岗岩样品的渗透率和超声速度,以评估由热应力引起的破坏条件。此外,采用扫描电子显微镜分析热裂纹的微观特征。结果表明,与液氮冲击相比,加热过程对热裂纹的产生影响较小。裂纹主要集中在冲击表面附近的区域,这是因为那里的温度梯度很大。受冲击的岩石由于拉伸应力和剪切应力的作用而破裂。随着初始岩石温度的升高,热裂纹的数量增加,并且在每个试样中形成更复杂的裂纹网络。瞬态脉冲评估和超声速度测量表明,液氮射流的冲击可以提高渗透率,并引起热岩石的破坏。这项研究证明了热应力对HDR储层液氮射流压裂过程中裂纹产生的重要影响,这一结果为开发HDR能量提供了启示。

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