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首页> 外文期刊>Journal of natural gas science and engineering >Effect of water and nitrogen fracturing fluids on initiation and extension of fracture in hydraulic fracturing of porous rock
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Effect of water and nitrogen fracturing fluids on initiation and extension of fracture in hydraulic fracturing of porous rock

机译:水和氮压裂液对多孔岩石水力压裂骨折启动及裂缝的影响

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摘要

An improved fracture initiation pressure criterion based on the initiation criterion of the mode I crack is proposed to interpret the different phenomena induced by water and nitrogen fracturing fluids. Hydraulic fracturing experiments on sandstone, coal and shale cores are performed using water and nitrogen to investigate the effects of the rock type and fracturing fluid type on the fracture initiation pressure and to verify the improved initiation pressure criterion. The crack propagation process and extended fracture complexity are also investigated based on hydraulic fracturing experiments. The sensitivity of the key parameter to the crack initiation pressure is explored using the improved initiation pressure criterion. The results show that the improved initiation pressure criterion is reliable. Nitrogen fracturing fluid can effectively reduce the fracture initiation pressure of rock compared with water, especially for low permeability shale. Micro-crack initiation occurs more easily before failure and the crack extension process is more violent in nitrogen fracturing. In water fracturing, a single fracture is induced, but complex fractures including tortuous and multiple fractures are produced in nitrogen fracturing. The extended fracture complexity in nitrogen fracturing is more likely to be affected by the lithologic character of rock compared with water fracturing. From the parameter sensitivity study, there are upper and lower limits on the permeability of shale causing pressurization rate to have a significant impact on the fracture initiation pressure. The upper and lower limits of permeability for nitrogen are four orders of magnitude greater than those for water. In the affected range of permeabilities, whether the fracturing fluid is water or nitrogen, changes in the fracture initiation pressure with the increase of the pressurization rate show an approximately logarithmic increase, linear increase and exponential increase in order of increasing permeability. (C) 2017 Elsevier B.V. All rights reserved.
机译:提出了一种改进的裂缝起始压力标准,其裂纹的启动标准被提出解释水和氮压裂液引起的不同现象。使用水和氮来进行砂岩,煤和页岩芯的液压压裂实验,以研究岩石型和压裂流体型对骨折起始压力的影响,并验证改进的启动压力标准。基于液压压裂实验,还研究了裂缝繁殖过程和延长的断裂复杂性。利用改进的启动压力标准探索了关键参数对裂缝启动压力的灵敏度。结果表明,改进的发起压力标准是可靠的。与水相比,氮压裂液可以有效地降低岩石的断裂引发压力,特别是对于低渗透性页岩。在失败前更容易发生微裂纹引发,并且在氮压裂中裂缝延伸过程更剧烈。在水压裂中,诱导单一骨折,但在氮气压裂中产生包括曲折和多个骨折的复杂骨折。与水压裂相比,氮压裂中的延长骨折复杂性更可能受到岩石岩性特征的影响。从参数敏感性研究中,对页岩的渗透性导致加压率对骨折起始压力产生显着影响的渗透性和下限。氮的渗透率的上下限制比水为大小的四个数量级。在受影响的渗透范围内,压裂液是否为水或氮气,断裂引发压力的变化随着加压率的增加显示了近似对数增加,线性增加和指数增加的渗透性。 (c)2017 Elsevier B.v.保留所有权利。

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  • 作者单位

    China Univ Min &

    Technol State Key Lab Geomech &

    Deep Underground Engn Room 313 1 Daxue Rd Xuzhou 221116 Jiangsu Peoples R China;

    China Univ Min &

    Technol State Key Lab Geomech &

    Deep Underground Engn Room 313 1 Daxue Rd Xuzhou 221116 Jiangsu Peoples R China;

    China Univ Min &

    Technol State Key Lab Geomech &

    Deep Underground Engn Room 313 1 Daxue Rd Xuzhou 221116 Jiangsu Peoples R China;

    China Univ Min &

    Technol State Key Lab Geomech &

    Deep Underground Engn Room 313 1 Daxue Rd Xuzhou 221116 Jiangsu Peoples R China;

    China Univ Min &

    Technol State Key Lab Geomech &

    Deep Underground Engn Room 313 1 Daxue Rd Xuzhou 221116 Jiangsu Peoples R China;

    China Univ Min &

    Technol State Key Lab Geomech &

    Deep Underground Engn Room 313 1 Daxue Rd Xuzhou 221116 Jiangsu Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 石油、天然气工业;
  • 关键词

    Hydraulic fracturing; Water; Nitrogen; Porous rock; Fracture initiation pressure; Crack extension;

    机译:水力压裂;水;氮;多孔岩;骨折起始压力;裂缝延伸;

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