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Multi-fractured stimulation technique of hydraulic fracturing assisted by the DTH-hammer-induced impact fractures

机译:潜孔锤引起的冲击裂缝辅助水力压裂的多裂缝增产技术

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摘要

Hydraulic fracturing is one of the key technologies in geothermal development of hot-dry-rock (HDR) geothermal energy. How to reduce the fracturing pressure and enhance the fractures connectivity of HDR has become a hot issue. In this paper, we propose to use a down-the-hole (DTH) hammer to impact granite, which assist to create new artificial fractures similar to natural fractures or widen the existing fractures near the wellbore, consequently enhancing the connectivity of fractures during hydraulic fracturing. A series of experiments were conducted to verify the feasibility of this stimulation technique, including the observation and quantification of impact fractures, and the determination of fracturing pressure. In addition, numerical simulation of impact stress wave was carried out to explain the distribution of fractures. The results showed that the granite rock mass damage caused by percussive rotary drilling was about 5-7 times larger than that caused by diamond rotary drilling. Meanwhile, the distribution of fractures was characterized by regionalization, which was mainly attributed to the attenuation of impact stress wave, and the numerical results were consistent with the experimental observations. Laboratory experiment results of hydraulic fracturing indicated that the fracturing pressure of granite samples near the wellbore after percussive drilling had been greatly reduced, which was nearly 50% lower than that of conventional drilling. It indicates that the proposed multi-fractured stimulation technique of hydraulic fracturing assisted by the impact fractures induced by a DTH hammer can be a potential solution to solve the problems of hydraulic fracturing.
机译:水力压裂是热干岩(HDR)地热能开发的关键技术之一。如何降低压裂压力,增强HDR的裂缝连通性已经成为一个热门问题。在本文中,我们建议使用潜孔锤(DTH)冲击花岗岩,这有助于产生类似于天然裂缝的新人工裂缝或扩大井眼附近的现有裂缝,从而增强水力压裂过程中裂缝的连通性压裂。进行了一系列实验以验证该增产技术的可行性,包括观察和量化冲击裂缝以及确定压裂压力。此外,进行了冲击应力波的数值模拟,以解释裂缝的分布。结果表明,冲击钻造成的花岗岩岩体破坏是金刚石钻造成的约5-7倍。同时,裂缝的分布以区域化为特征,其主要归因于冲击应力波的衰减,数值结果与实验结果吻合。水力压裂的室内实验结果表明,冲击钻后井筒附近花岗岩样品的压裂压力大大降低,比常规钻井低了近50%。这表明,本文提出的DTH锤头冲击裂缝辅助的水力压裂多裂口增产技术可能是解决水力压裂问题的潜在解决方案。

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