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

机译:三轴约束应力下热干岩低温压裂试验研究

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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)具有很高的热能潜力,可通过水力压裂加以利用以提取热量并发电。由于深度(2〜6 km)以及随之而来的高温(150〜650°C)和高压,因此难以刺激HDR。这项工作的目的是研究在HDR上进行低温压裂的可行性。在三轴约束应力下,我们对岩石样品进行了一系列的实验室实验。为了产生剧烈的热冲击,在进行刺激测试之前,将高温花岗岩岩石标本(100〜700°C)浸入液氮(LN)(-196°C)中数小时。然后,考虑了两种方案:使用和不使用LN处理的天然气压裂。随后,确定并讨论了断裂模式。最后,针对LN快速冷却和自然冷却刺激,建立了两个相关性,以根据实验数据预测击穿压力。结果表明,与未经处理的试样相比,经LN处理的试样的击穿压力可降低9-51%。特别是,LN在200°C以上的岩石样品上具有出色的压裂效率。主要原因可能归因于LN流体引起的高热梯度和比霜作用力,这可能导致强烈的局部拉伸应力扩展高温岩石样品内部的微孔结构。此外,随着岩石和压裂液之间温度差的增加,特别是在LN快速冷却作用的辅助下,可以生成更复杂的裂缝网络或连接的路径。这项工作的主要发现有益于提供一种有效的方法来探索地热开发中的HDR资源。

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