Cooling-induced permeability enhancement for networks of microfractures in superhot geothermal environments

IF 2.9 2区 地球科学 Q3 ENERGY & FUELS Geothermal Energy Pub Date : 2023-04-17 DOI:10.1186/s40517-023-00251-9
Ryota Goto, Daisuke Nakayama, Ryota Takahashi, Eko Pramudyo, Kohei Takuma, Noriaki Watanabe
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Abstract

Recent researches have proposed the use of enhanced geothermal system reservoirs consisting of dense networks of microfractures, created by hydraulic and/or thermal fracturing in superhot/supercritical geothermal environments, because of their suitability for thermal energy harvesting. During fracturing and energy extraction, the fracture networks are exposed to cooling due to the injection of cold fluid into the reservoirs. Previous studies showed such cooling enhanced reservoir permeability in conventional geothermal environments. However, the cooling may result in a higher risk of seismicity, owing to decreased normal stress on the fractures. Nevertheless, it is unclear whether cooling-induced permeability enhancement and a higher risk of seismicity occurs within networks of microfractures which consist of numerous interconnected microfractures at various orientations to the in situ triaxial stress. Thus, no dominant fractures have the possibility to cause permeability enhancement/induced seismicity. In this study, results are presented for borehole cooling experiments on a dense network of microfractures in granite, at 400 °C, under true triaxial stress. Permeability and acoustic emissions were measured with decreases in borehole temperature (up to ~ 90 °C). Results showed that permeability increased with increasing temperature drop at relatively low stress levels (15 and 20 MPa). The permeability enhancement occurred without intensive failure, and was reversible. However, permeability was almost constant at a higher stress level (65 MPa). Results showed that permeability enhancement required a thermal stress equivalent to the mean stress, so that the normal stress was reduced to near-zero, for a considerable amount of the microfractures. Additionally, the permeability of dense microfracture networks can be increased by cooling primarily through thermo-elastic deformation (without intensive failure), which may be useful to compensate for the reduction in injectivity due to cooling-induced fluid property changes.

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超高温地热环境中微裂缝网络冷却致渗透率增强研究
最近的研究建议使用由致密微裂缝网络组成的增强型地热系统储层,这些微裂缝网络是在超高温/超临界地热环境中由水力和/或热压裂产生的,因为它们适合热能收集。在压裂和能量提取过程中,由于向储层注入冷流体,裂缝网络暴露在冷却中。先前的研究表明,这种冷却可以提高常规地热环境下储层的渗透率。然而,由于裂缝上的正常应力降低,冷却可能会导致地震活动的风险增加。然而,目前尚不清楚冷却诱导的渗透率增强和地震活动性的增加是否发生在微裂缝网络中,这些微裂缝由许多相互连接的微裂缝组成,在不同的三轴应力方向上。因此,没有优势裂缝有可能引起渗透率增强/诱发地震活动。在这项研究中,给出了在真三轴应力下400°C下花岗岩致密微裂缝网络的钻孔冷却实验结果。渗透率和声发射随井眼温度降低(高达~ 90°C)而测量。结果表明:在相对较低的应力水平(15和20 MPa)下,渗透率随温度下降而增加;渗透性增强发生在没有严重破坏的情况下,并且是可逆的。然而,在较高的应力水平(65 MPa)下,渗透率几乎不变。结果表明,提高渗透率需要一个与平均应力相等的热应力,从而使相当数量的微裂缝的正应力降至接近于零。此外,致密微裂缝网络的渗透率可以通过主要通过热弹性变形(没有严重破坏)进行冷却来提高,这可能有助于弥补由于冷却引起的流体性质变化而导致的注入能力下降。
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来源期刊
Geothermal Energy
Geothermal Energy Earth and Planetary Sciences-Geotechnical Engineering and Engineering Geology
CiteScore
5.90
自引率
7.10%
发文量
25
审稿时长
8 weeks
期刊介绍: Geothermal Energy is a peer-reviewed fully open access journal published under the SpringerOpen brand. It focuses on fundamental and applied research needed to deploy technologies for developing and integrating geothermal energy as one key element in the future energy portfolio. Contributions include geological, geophysical, and geochemical studies; exploration of geothermal fields; reservoir characterization and modeling; development of productivity-enhancing methods; and approaches to achieve robust and economic plant operation. Geothermal Energy serves to examine the interaction of individual system components while taking the whole process into account, from the development of the reservoir to the economic provision of geothermal energy.
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