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岩石水力压裂力学特性劣化试验研究

Experimental study on mechanical properties of rock degraded by hydraulic fracturing

  • 摘要: 岩石水力压裂力学性质劣化程度准确测定是水力压裂卸压机理揭示和压裂效果评估的基础,为揭示岩石水力压裂力学特性劣化规律,分别设计了真三轴水力压裂物模试验和岩石力学测试试验2个阶段方案,利用CT扫描重构裂缝三维形态,通过真三轴水力压裂物模试验,制备含水力压裂裂缝的岩石试件;对制备的含水力压裂裂缝的岩石试件开展了岩石力学性质单轴、三轴压缩试验和巴西劈裂试验。结果表明:刻槽能够有效降低裂缝破裂压力,增大槽的宽度,有利于提高裂缝起裂概率,但槽间距太小,裂缝易合并;压裂液黏度越高,泵注压力起压越快,裂缝破裂压力越高;排量越低,液体滤失所占比例越大,裂缝破裂压力越小,排量升高后,裂缝起裂压力显著增大,起裂所需时间越短。水力压裂后,岩石内摩擦角、黏聚力、抗拉强度的折减系数分别为0.896、0.996、0.295;得到了弹性模量折减系数关系式,随围压增大,2种试样弹性模量均呈增大趋势,且增长速率逐渐减缓,而折减系数随围压增大呈降低趋势,但降低速率减缓;试样抗拉强度压裂后降幅为70.49%,降低量达压裂后试样的2.39倍,试样抗拉强度显著降低,表明压裂使试样内部产生裂隙,发生损伤,压裂前后标准差增大1.87倍,表明压裂过程使试样内部产生大量非均匀分布裂隙,微裂隙数量及分布特征存在较大差异,造成试样力学性能差异较大。

     

    Abstract: The accurate determination of the degree of mechanical property degradation of rock layers after hydraulic fracturing is the basis for revealing the pressure relief mechanism of hydraulic fracturing and evaluating the fracturing effect. To reveal the degradation law of rock hydraulic fracturing mechanical properties, a two-stage scheme of true triaxial hydraulic fracturing physical model experiment and rock mechanics testing experiment was designed separately In order to study the degradation law of mechanical properties of rock layers before and after hydraulic fracturing, a two-stage plan of true triaxial hydraulic fracturing physical model experiment and rock mechanics testing experiment was designed. CT scanning was used to reconstruct the three-dimensional morphology of fractures. Through true triaxial hydraulic fracturing physical model experiment, rock specimens containing hydraulic fracturing fractures were prepared; Uniaxial and triaxial compression tests, as well as Brazilian splitting tests, were conducted on rock specimens containing hydraulic fracturing fractures. The research results indicate that grooving can effectively reduce the pressure of crack rupture, increase the width of the groove, and improve the probability of crack initiation. However, if the groove spacing is too small, cracks are prone to merge; The higher the viscosity of the fracturing fluid, the faster the pumping pressure rises, and the higher the fracture pressure; The lower the displacement, the greater the proportion of liquid filtration, and the lower the crack rupture pressure. After the displacement increases, the crack initiation pressure significantly increases, and the time required for initiation is shorter. After hydraulic fracturing, the reduction coefficients of internal friction angle, cohesion, and tensile strength of the rock are 0.896, 0.996, and 0.295, respectively; The relationship between the reduction coefficient of elastic modulus was obtained. With the increase of confining pressure, the elastic modulus of both samples showed an increasing trend, and the growth rate gradually slowed down. However, the reduction coefficient showed a decreasing trend with the increase of confining pressure, but the rate of decrease slowed down; The tensile strength of the sample decreased by 70.49% after fracturing, which was 2.39 times that of the sample after fracturing. The significant decrease in tensile strength of the sample indicates that fracturing causes cracks and damage inside the sample. The standard deviation before and after fracturing increased by 1.87 times, indicating that the fracturing process generates a large number of unevenly distributed cracks inside the sample, and there are significant differences in the number and distribution characteristics of micro cracks, resulting in significant mechanical differences in the sample.

     

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