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Laboratory Investigation on Cryogenic Fracturing of Hot Dry Rock Under Triaxial-Confining Stresses

机译:三轴限制应力下热干岩冷冻压裂的实验室调查

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Hot dry rock (HDR) has high potential of thermal energy, which can be exploited by hydraulic fracturing to extract heat and generate electricity. Because of great depth (2~6 km) and consequent high temperature (150~650 °C) and high pressure, the stimulation of HDR is difficult. Purpose of this work is to study the feasibility of cryogenic fracturing on HDR. We conducted a series of laboratory experiments on rock samples under triaxial-confining stresses. To generate sharp thermal shock, high-temperature granitic rock specimens (100~700 °C) were immersed into liquid nitrogen (LN) (-196°C) for several hours before the stimulation tests. Then, two schemes were considered: gas fracturing with and without LN treatment. Subsequently, fracture patterns were identified and discussed. Finally, two correlations for both LN rapid-cooling and naturally-cooling stimulations were developed to predict the breakdown pressure based on the experimental data. The results show that compared with untreated specimen, the breakdown pressure for LN treated specimen can be reduced by 9~51%. Particularly, LN has superior fracturing efficiency on rock specimens above 200°C. The major reason could be attributed to the high thermal gradient and specific frost force induced by LN fluids, which can cause strong local tensile stress expand the micro-pore structures inside the high-temperature rock samples. Furthermore, with the increasing temperature difference between rocks and fracturing fluid, especially with the assistance of LN rapid-cooling effect, more complex fracture networks or connected pathways can be generated. The key findings of this work are beneficial for providing an efficient approach to explore HDR resources in geothermal development.
机译:热干岩(HDR)具有高热能潜力,可通过液压压裂利用以提取热量并发电。由于深度大(2〜6公里)并因此高温(150〜650°C)和高压,HDR的刺激难。这项工作的目的是研究低温压裂对HDR的可行性。在三轴限制应力下,我们在岩石样品上进行了一系列实验室实验。为了产生急剧的热冲击,在刺激试验之前将高温花岗岩标本(100〜700℃)浸入液氮(-196℃)中的液氮(-196℃)。然后,考虑了两种方案:气体压裂,没有LN处理。随后,鉴定并讨论了骨折模式。最后,开发了用于LN快速冷却和自然冷却刺激的两个相关性以基于实验数据预测击穿压力。结果表明,与未经处理的标本相比,LN处理样品的击穿压力可降低9〜51%。特别是,LN对200℃以上的岩石样品具有卓越的压裂效率。主要原因可归因于由LN流体引起的高热梯度和特定霜力,这可能导致强烈的局部拉应力膨胀高温岩石样品内的微孔结构。此外,随着岩石和压裂流体之间的温差越来越大,特别是在LN快速冷却效果的辅助,可以产生更复杂的裂缝网络或连接的途径。这项工作的主要结果有利于提供一种有效的方法来探索地热发展中的HDR资源。

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