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Experimental study on the physical and mechanical variations of hot granite under different cooling treatments

机译:不同冷却处理下热花岗岩物理和机械变化的实验研究

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摘要

Geothermal energy arrested in HDR (hot dry rock) is commonly harvested from the reservoir fractured by artificial stimulations. Understanding the physical and mechanical behaviors of HDR after different cooling treatments is critical for selecting most efficient fluid to fracture the rock mass. Here we experimentally examine the physical and mechanical variations of a typical type of HDR, granite, after natural, water, and liquid-nitrogen cooling treatments, followed by a multi-scale investigation on the evolution of cracks. We find that the effect of cooling treatment on the physical and mechanical properties of heated granite specimens is increasingly remarkable as the peak temperature grows. The difference among the influences of different cooling treatments is unnoticeable when the specimens are heated to peak temperatures of 200 degrees C and 400 degrees C, but becomes highly pronounced as the peak temperature ascends to 600 degrees C and 800 degrees C. Liquid-nitrogen cooling treatment induces most alterations in the granite properties. The cracks in the granite specimens cooled by liquid-nitrogen coalesce together and form complex fracture networks, which are more intensive than those by natural and water cooling treatments. Previous studies claimed that the liquid-nitrogen cooling treatment had weaker influence on the granite specimen than water, possibly due to the Leidenfrost effect that impeded the heat transfer between rock and liquid-nitrogen. Our findings demonstrate that liquid-nitrogen is superior in cracking and thus enhancing the permeability of the granite specimens, particularly for those heated to a temperature over 400 degrees C. The good performance of liquid-nitrogen is attributed to that the granite specimen is easily cracked by the high tensile stress created jointly by the high temperature difference caused by its ultra-low temperature and large convective heat transfer coefficient induced by violent boiling. (C) 2021 Elsevier Ltd. All rights reserved.
机译:在HDR(干热岩)被捕地热能通常由人工刺激裂缝储层收获。了解HDR的物理和力学性能的不同冷却处理后为选择最有效的流体压裂岩体关键的。在这里,我们通过实验检查后自然,水和液氮冷却治疗的典型类型HDR,花岗岩,中,随后的裂纹的发展多尺度调查的物理和机械变型。我们发现,在加热的花岗岩样品的物理和机械性能冷却处理的效果是随着峰值温度的增长日益显着。的不同冷却处理的影响之间的差异是不显着,当试样加热到200℃和400℃的峰值温度,但变得高度发音为峰值温度上升到600℃和800℃液氮冷却处理导致花岗岩性能最为改变。在花岗岩试样的裂纹冷却通过液氮聚结在一起,形成复杂的裂缝网络,这是比由天然和水冷却处理更加密集。以前的研究声称,液氮冷却处理对花岗岩试样比水更弱的影响,这可能是由于该阻碍岩石和液氮之间的热传递的莱顿弗罗斯特效应。我们的研究结果表明,液态氮是在开裂和因此增强了花岗岩试样的渗透性,特别是对那些在400℃液氮的良好性能归因于所述花岗岩试样容易破裂加热到温度优越通过引起其超低温,并通过剧烈沸腾引起的大的对流热传递系数的高温度差共同产生的高的拉伸应力。 (c)2021 elestvier有限公司保留所有权利。

著录项

  • 来源
    《Renewable energy》 |2021年第12期|1316-1328|共13页
  • 作者单位

    Dalian Univ Technol State Key Lab Coastal & Offshore Engn Dalian 116024 Peoples R China;

    Henan Polytech Univ Coll Safety Sci & Engn Jiaozuo 454000 Henan Peoples R China;

    Dalian Univ Technol State Key Lab Coastal & Offshore Engn Dalian 116024 Peoples R China|Sichuan Univ Minist Educ Key Lab Deep Earth Sci & Engn Chengdu 610065 Peoples R China;

    Sichuan Univ Minist Educ Key Lab Deep Earth Sci & Engn Chengdu 610065 Peoples R China;

    Dalian Univ Technol State Key Lab Coastal & Offshore Engn Dalian 116024 Peoples R China;

    Dalian Univ Technol State Key Lab Coastal & Offshore Engn Dalian 116024 Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Hot dry rock; Thermal-treated granite; Cooling treatment; Liquid-nitrogen;

    机译:热干岩;热处理花岗岩;冷却处理;液氮;

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