Laboratory study on the mechanical behaviors of an anisotropic shale rock

Shale gas is becoming an important energy source worldwide. The geomechanical properties of shalerocks can have a major impact on the efficiency of shale gas exploration. This paper studied themineralogical and mechanical characteristics of a typical gas shale in Ohio, USA. Scanning electron microscope（SEM） with energy dispersive X-ray （EDX） analyses was employed to measure the microstructureand material composition of the shale rock. The anisotropic behaviors of shale rock, includingcompressive and tensile strengths, were experimentally measured. The characteristics of shale rock werealso studied by nondestructive wave speed measurements. The shale demonstrated strong anisotropicbehaviors with the tensile strengths perpendicular to the bedding plane around 300e360 times of thatparallel to bedding plane. Results of ultrasonic tests indicated that both compression and shear wavevelocities show strong anisotropic patterns. The compression wave speed was the smallest in the directionperpendicular to the bedding plane; while the shear wave speed was the smallest in the directionparallel to the bedding plane. The ratio of wave speed anisotropy is around 1.3e1.4 for compressionwave; the ratio of shear wave speed anisotropy is larger and more diverse compared with thecompression wave anisotropy. This might be related to the larger variability in the frictional adhesivestrength along bedding plane than the compressive adhesive strength. 2015 Institute of Rock and Soil Mechanics, Chinese Academy of Sciences. Production and hosting byElsevier B.V. All rights reserved.

Evaluation on the anisotropic brittleness index of shale rock using geophysical logging

The brittleness index plays a significant role in the hydraulic fracturing design and wellbore stability analysis of shale reservoirs.Various brittleness indices have been proposed to characterize the brittleness of shale rocks,but almost all of them ignored the anisotropy of the brittleness index.Therefore,uniaxial compression testing integrated with geophysical logging was used to provide insights into the anisotropy of the brittleness index for Longmaxi shale,the presented method was utilized to assess brittleness index of Longmaxi shale formation for the interval of 3155e3175 m in CW-1 well.The results indicated that the brittleness index of Longmaxi shale showed a distinct anisotropy,and it achieved the minimum value at β=45°-60°.As the bedding angle increased,the observed brittleness index(BI_(2_β))decreased firstly and increased then,it achieved the lowest value at β=40°-60°,and it is consistent with the uniaxial compression testing results.Compared to the isotropic brittleness index(β=0°),the deviation of the anisotropic brittleness index ranged from 10%to 66.7%,in other words,the anisotropy of brittleness index cannot be ignored for Longmaxi shale.Organic matter content is one of the main intrinsic causes of shale anisotropy,and the anisotropy degree of the brittleness index generally increases with the increase in organic matter content.The present work is valuable for the assessment of anisotropic brittleness for hydraulic fracturing design and wellbore stability analysis.

Impact of hydraulic perforation on fracture initiation and propagation in shale rocks

To enhance the oil and gas recovery rate, hydraulic fracturing techniques have been widely adopted for stimulation of low-permeability reservoirs. Pioneering work indicates that hydraulic perforation and layout could significantly affect fracture initiation and propagation in low-permeability reservoir rocks subjected to complex in-situ stresses. This paper reports on a novel numerical method that incorporates fracture mechanics principles and the numerical tools FRANC3 D and ANSYS to investigate the three-dimensional initiation and propagation behavior of hydro-fracturing cracks in shale rock. Considering the transverse isotropic property of shale rocks, the mechanical parameters of reservoir rocks attained from laboratory tests were adopted in the simulation. The influence of perforation layouts on the 3D initiation of hydro-fracturing fractures in reservoir rocks under geo-stresses was quantitatively illuminated. The propagation and growth of fractures in three dimensions in different perforating azimuth values were illustrated. The results indicate that: 1) the optimal perforation direction should be parallel to the maximum horizontal principal stress, 2) the crack plane gradually turns toward the direction of the maximum horizontal principal stress when they are not in parallel, 3) compared with the linear and symmetric pattern, the staggered perforation is the optimal one, 4) the proper perforation density is four to six holes per meter, 5) the optimal perforation diameter in this model is 30 mm, and 6) the influence of the perforation depth on the fracture initiation pressure is low.

Sliding friction of shale rock on dry quartz sand particles

The sliding friction of rock, involving all kinds of particles at the contact surface, is relevant to many problems, ranging from those in artificial engineering to earthquake dynamics. In this work, the frictional performance of the shale rock–dry quartz sand contact was investigated using a self-developed testing device. The study showed that the coefficient of friction of the contact increases with nominal stress and that the corresponding friction force increases approximately linearly with nominal stress, which is directly related to the contact stress between each single sand particle and rock shale. An overall dynamic coefficient, γ, reflecting the response of friction force to nominal stress, first decreases and then increases with area ratio, which is determined by not only the contact stress but also the interparticle friction force. These have important repercussions for a preliminary understanding of the frictional properties of the shale rock–dry quartz sand contact in hydraulic fracturing and related industrial applications.

Occurrence of Highly Mature Organic Matter in Marine Black Shale Petroleum Source Rocks of Basal Cambrian from Northern Tarim Basin, China

More and more evidence indicates that organic matter (OM) in immature organic-rich sediments and sedimentary rocks is chemically adsorbed onto the outer surfaces of minerals and into interlayer (inner) surfaces of smectitic clay minerals in the form of amorphous molecular-scale carbon. But there have been few reports about the occurrence of highly mature OM in marine black shales (petroleum source rocks). The occurrence of highly mature OM in the black shales of basal Cambrian from northern Tarim Basin is studied in this paper. Based on the comprehensive analyses of total organic carbon contents (TOC), maximum thermolysis temperatures (T-max) of OM, mineral surface areas (MSA), and scanning electronic microscopic (SEM) and transmission electronic microscopic (TEM) observations of the black shales, it is concluded that the highly mature OM in the marine black shales of the basal Cambrian from northern Tarim Basin occurs in particulates ranging in size from 1 to 5 μm in diameter. Through the contrast of the occurrence of the highly mature OM in the black shales with that of the immature ones in modern marine continental margin sediments, some scientific problems are proposed, which are worth to study further in detail.

A rock physics model for the characterization of organic-rich shale from elastic properties

Kerogen content and kerogen porosity play a significant role in elastic properties of organic-rich shales. We construct a rock physics model for organic-rich shales to quantify the effect of kerogen content and kerogen porosity using the Kuster and Toks6z theory and the selfconsistent approximation method. Rock physics modeling results show that with the increase of kerogen content and kerogen-related porosity, the velocity and density of shales decrease, and the effect of kerogen porosity becomes more obvious only for higher kerogen content. We also find that the Poisson＇s ratio of the shale is not sensitive to kerogen porosity for the case of gas saturation. Finally, for the seismic reflection responses of an organic-rich shale layer, forward modeling results indicate the fifth type AVO re- sponses which correspond to a negative intercept and a positive gradient. The absolute values of intercept and gradient increase with kerogen content and kerogen porosity, and present predictable variations associated with velocities and density.

Characteristics and Evaluation of the High-Quality Source Rocks of Cretaceous Continental Shale Oil in Tonghua Basin, China

The presence of shale oil in the Cretaceous Hengtongshan Formation in the Tonghua Basin, drilled by the well TD-01, has been discussed in this geological investigation for the first time. To evaluate the high-quality source rocks of Cretaceous continental shale oil, the distribution characteristics and the evolution of the ancient environment, samples of shale were systematically analyzed in terms of sedimentary facies, organic geochemistry, and organic carbon isotopic composition. The results demonstrate that a TOC value of 1.5% represents the lower-limit TOC value of the high-quality source rocks. Source rocks have an aggregate thickness of 211 m and contain abundant organic matter, with TOC values of 2.69% on average and a maximum value over 5.44%. The original hydrocarbon-generative potential value(S_1+S_2) is between 0.18 mg/g and 6.13 mg/g, and the Ro is between 0.97% and 1.40%. The thermal maturation of the source rocks is relatively mature to highly mature. The δ^(13)C value range is between -34.75‰ and -26.53‰. The ratio of saturated hydrocarbons to aromatic hydrocarbons is 1.55 to 5.24, with an average of 2.85, which is greater than 1.6. The organic types are mainly type Ⅱ_1, followed by type Ⅰ. The organic carbon source was C_3 plants and hydrophytes. The paleoclimate of the Hengtongshan Formation can be characterized as hot and dry to humid, and these conditions were conducive to the development of high-quality source rocks. A favorable paleoenvironment and abundant organic carbon sources provide a solid hydrocarbon generation base for the formation and accumulation of oil and gas in the shale of the Tonghua Basin.

注热化学流体吞吐解除岩石储层反凝析伤害评价

为长期有效解除凝析气藏反凝析带来的储层伤害,提出了一种注热化学流体吞吐解除凝析油堵塞孔喉的新方法。针对致密砂岩、碳酸盐岩和页岩3类岩石,开展了注热化学流体吞吐岩心驱油实验,评价了热化学流体解除凝析油堵塞的可行性,并基于核磁共振技术分析了吞吐前后3类岩石微观孔隙结构的变化特征,明确了热化学流体解除反凝析伤害机理。实验结果表明,热化学流体(NH_(4)Cl和NaNO_(2))在乙酸溶液催化下能够迅速释放大量气体和蒸汽,提高岩心压力和温度,降低原油黏度,使凝析油由液态转变为气态,减小渗流阻力。致密砂岩、碳酸盐岩和页岩岩心注热化学流体吞吐累积凝析油采出程度分别为65.7%,73.9%和46.3%。其中,致密砂岩和碳酸盐岩岩心仅需2轮吞吐即可有效清除55.5%和67.6%的凝析油堵塞。而页岩岩心需要延长焖井时间及增加吞吐次数方能提高凝析油的采出程度。热化学流体吞吐后,致密砂岩、碳酸盐岩和页岩岩心平均孔径分别由0.37,1.04和0.0021μm增大至0.84,2.04和0.0058μm。热化学流体吞吐效果是注CH_(4)吞吐和注甲醇吞吐效果的1.85和1.32倍。

大庆油田裸眼井测井技术进展与展望

为了提高大庆油田裸眼井测井技术支撑能力和研究成果领先水平,全面回顾了大庆油田测井采集系列及解释技术的创新发展历程,系统总结了特高含水期剩余油解释、火山岩等复杂岩性测井评价、碎屑岩储量参数解释、非常规油气“甜点”分类、缝洞型碳酸盐岩储层测井评价等油田勘探开发测井评价技术。在客观分析大庆油田勘探开发测井解释评价需求和面临瓶颈问题的基础上,结合当前油田测井评价对象规模小、物性差、埋藏深、地层结构复杂、非均质性强的特点。指明了测井解释评价核心技术主攻方向。围绕新阶段测井采集及解释评价技术体系完善与建立,对高分辨率和成像测井采集、后油藏时期和非常规测井解释评价、新一代智能解释技术体系等未来发展进行了展望。

鄂尔多斯盆地南缘华北探区页岩油储层岩石力学特性实验研究

针对鄂尔多斯盆地南部延长组7段页岩储层钻井过程中发生钻头适应性差和井壁垮塌等井下复杂状况,开展了岩石组构特征分析、力学特征分析和可钻性参数等力学特征分析。结果表明,鄂尔多斯盆地南缘页岩油储层中黏土以伊利石和伊/蒙混层为主,岩石结构及力学特性非均质性强。岩石表面层理结构明显,微裂缝和孔隙发育。页岩抗张强度为6.58~18.27 MPa,单轴抗压强度为76.79~169.29 MPa,高温下的内摩擦角为14.67°~36.71°,泊松比为0.167~0.352,主要集中在0.21附近,弹性模量为4 100~17 344 MPa。最小水平主应力梯度为1.89~2.14 MPa/100 m,最大水平主应力梯度为2.37~3.04 MPa/100 m,其中洛河地区最大、最小地应力梯度差值较大。地层可钻性级值为4.36~6.11,主要分布在5.5以下,属于软-中硬度地层,平均地层倾角小,在钻至水平段时,钻进方向与层理相同,与岩石接触面多互层,钻头磨损加重。基于页岩储层岩石力学特性认识,对于鄂南页岩油安全、高效地钻探具有指导意义。

基于地震反演技术的地应力建模方法在江汉新沟嘴组页岩油中的应用

江汉盆地新沟嘴组页岩油地质评价资源量为3.6×108 t,具有良好的勘探潜力,其中地质评价Ⅰ类有利区陈沱口凹陷有多口井在新沟嘴组新下段Ⅱ油组泥质白云岩中获得油流。由于页岩油井通常采用“水平井+分段压裂”工艺实现经济开采,因而地应力研究对该区水平井储层压裂改造具有重要的意义。三维地应力建模研究的核心问题在于提升井间地应力预测效果,传统的有限元方法由于方法本身的限制,井间预测效果较差,有必要利用地震资料反演技术来提升井间地应力预测的效果。针对该区页岩层矿物组分多、局部发育硫酸盐岩、地应力条件复杂的问题,首先对新沟嘴组页岩层开展基于实验室测量值约束的精细测井评价,其结果与岩心全岩X衍射测量结果吻合;在此基础上,选择自相容近似地震岩石物理建模流程,对目标层的弹性参数进行了正演模拟,正演结果与实测曲线基本吻合。然后,基于地层压力、实验室测量的岩石力学性能参数和测井解释结果,依据不同岩性的动静态关系,采用有效应力比值和构造应变法计算井的地应力参数。最后运用基于地震叠前反演技术的三维地应力建模方法,使用与一维地质力学建模相同的相关性和参数约束,建立了新沟嘴组页岩油的三维地应力模型。与一维地质力学研究成果相比,该三维地应力模型提取的伪曲线与工区大部分井一维地应力结果基本吻合,验证了该方法在新沟嘴页岩油地应力评价中的适用性和准确性。

节理化炭质页岩地层隧道围岩大变形及控制技术研究

某高速铁路XHS隧道穿越节理化炭质页岩地层,在施工过程中围岩大变形、失稳坍塌现象显著,现场采用强支护和仰拱加深等措施后围岩变形控制效果不佳。针对XHS隧道节理化炭质页岩地层地质条件,结合现场监测手段、离散-连续耦合数值模拟分析围岩大变形及破坏特征,基于数值模拟提出以采取地层预加固为主的围岩变形控制措施,并通过现场试验探讨该控制措施的应用效果。研究结果表明:隧道开挖后,围岩变形具有变形量大、变形速率快的特点,围岩拱部沉降量大于水平收敛量且变形具有非对称的分布特征;受三台阶法多次开挖扰动影响,围岩卸荷范围动态发育并不断向全环扩展,松动区逐渐由浅部围岩向深部转移,并呈现出非对称的破坏特征,最终引发围岩大变形;采取地层预加固后,模型中围岩变形和松动区范围明显减小,围岩非对称变形破坏也得到了有效控制;在采用地层预加固、管棚超前支护、三台阶临时仰拱法开挖的控制措施后,围岩变形得到控制,施工效果良好,隧道恢复正常施工,保证了隧道的顺利贯通;以地层预加固为主的控制措施是此类节理化炭质页岩地层围岩变形控制的有效手段。

加强油源岩沉积成岩成油模拟实验研究

干酪根热降解生油学说源于油页岩高温热解生成“人造石油”的生产实践,其理论内涵是凡富含干酪根的岩石,经高温热解后其所含的干酪根都可以生成“人造石油”。应用该学说的高温热解实验方法,可以评价油页岩的品质及其热解生成“人造石油”的潜力,因此仅适用于油页岩的评价研究。但该学说的倡导者却认为油页岩和油源岩都是能生成石油的岩石,如果埋藏较浅时就称为油页岩,如果埋藏较深时就是油源岩,因此干酪根热降解生油学说同样适用于油源岩。这种观点并没有被美欧等国家所认可,但遗憾的是,在改革开放之初不甚了解国外同行对该学说如何评价的情况下,中国的石油地质家不仅全盘接受了该学说,而且推广应用了40多年。为彻底改变这种被动局面,唯一可行的就是通过油源岩沉积成岩成油模拟实验,研究油源岩中可溶有机质的生油问题和评价方法。

CO_(2)快速吞吐提高页岩油采收率现场试验

页岩油注CO_(2)吞吐提高采收率技术处于探索阶段,目前面临着CO_(2)与页岩储层及流体相互作用机制不明确、数值模拟技术不成熟、缺乏规模注采及低成本回收工艺等技术难题。为探索页岩油注CO_(2)提高采收率主控机理,以苏北盆地溱潼凹陷古近系阜宁组二段页岩油为对象开展了超临界CO_(2)水岩反应实验,分析了高温高压条件下页岩矿物溶蚀作用及其对孔隙度和渗透率的影响,并通过注CO_(2)恒质膨胀实验、最小混相压力测试评价了地层超压条件下注CO_(2)后原油高压物性变化特征,并在此基础上开展考虑多因素数值模拟研究优化了设计注入参数,最终通过矿场试验验证了技术可行性。研究结果表明:(1) CO_(2)水岩反应以碳酸质矿物溶蚀占主导,长英质矿物部分溶解,生成中大孔隙;(2)在地层原油中注入适量的CO_(2),显著萃取了原油中间烃组分,原油黏度从5.151 mPa·s下降到1.250 mPa·s,且CO_(2)首先萃取轻烃组分,随生产时间增加萃取组分逐渐变为重烃;(3)基于人工压裂与天然缝网混合介质组分数模模型,优化设计单井吞吐注气量1.7×10~4 t,注气速度500~600 t/d,焖井时间50 d;(4)低压侧加热的页岩油CO_(2)吞吐地面工艺,可依据CO_(2)注入地面工艺多参数数据模型,实现精准控温,避免注入管线冻堵及井下油管和套管材料低温脆断问题;(5)产出气CO_(2)浓度高于80%时,采用气相回收直注工艺,实现产出气回收成本降至104元/t。结论认为,CO_(2)快速吞吐有效提高了页岩油采收率,形成的机理认识和技术系列可为页岩油注CO_(2)吞吐开发提供参考和借鉴。

丙烯酰胺类聚合物在储层岩石表面的吸附行为

研究聚合物在油气储层岩石表面的吸附滞留对于工作液配方优化、提升非常规油气藏经济效益具有重大意义。为分析储层岩石与丙烯酰胺类聚合物的吸附作用,采用淀粉-碘化镉法间接测定了部分水解聚丙烯酰胺(HPAM)、部分水解丙烯酰胺/二烯丙基二甲基氯化铵共聚物(HPAD)和丙烯酰胺类疏水缔合聚合物(HAP)在页岩、煤岩和砂岩表面的吸附量,量化了吸附时间、聚合物浓度、温度和矿化度对3种聚合物在岩石表面吸附行为的影响。结果表明,HPAM和HAP在岩石表面的吸附更符合准二级吸附动力学模型,而HPAD则更符合准一级吸附动力学模型。与HPAD和HAP相比,HPAM平衡吸附量更大。3种聚合物在储层岩石上的吸附过程都更符合Freundlich吸附模型。达到吸附平衡所需时间与聚合物、储层岩石种类密切相关。HPAM在3种岩石表面的吸附会达到饱和,而HPAD和HAP的吸附量随着时间推移而增加。温度升高,会导致解吸附加剧,从而导致吸附量下降;溶液矿化度升高,聚合物的溶解度降低,导致吸附量增加。聚合物在储层表面的持续吸附是其在工作液中消耗的主要原因。HPAD和HAP可能会由于其在储层岩石表面的持续吸附,导致有效浓度过低而使工作液失效。

苏北盆地古近系阜宁组二段页岩油储层岩石力学特征及其控制因素

为查明苏北盆地页岩油储层可压性特征及压后孔、缝变化规律,以古近系阜宁组二段(阜二段)为研究对象,对岩石力学特征、压裂效果及其影响因素进行研究。用计算机高分辨断层扫描成像技术(多尺度CT扫描)对岩样进行三维重构,获取孔、缝结构参数;开展地层围压下三轴力学实验,获取岩石力学参数;将压裂后的岩样按相同位置和方向再次进行多尺度CT扫描,获取压裂后三维孔、缝结构图像。根据应力-应变曲线特征,将本区页岩划分为3种类型。①1型页岩,为破裂曲线波浪下降,压后形成复杂网状缝页岩。②2型页岩,为破裂曲线类型多样,具波浪下降和垂直下降形状,压后缝网较发育的页岩。③3型页岩,为破裂曲线垂直下降,破裂后整体较完整,压后多形成纵向劈裂缝、缝网不发育的页岩。这3种类型页岩压后孔隙变化特征是:1型和2型页岩直径10~50μm孔隙占比减少,直径50~100μm孔隙增多,直径300μm以上孔隙孔容贡献增大;3型页岩压裂前、后孔径分布及孔容贡献变化不明显。研究表明,抗压强度与弹性模量、剪切模量具有正相关关系,与泊松比具有V型曲线关系;碳酸盐和黏土矿物含量是控制本区页岩力学性质的主要因素,石英和有机碳含量为次要因素。孔隙度及纹层发育特征是页岩储层可压性特征的重要影响因素。

柴达木盆地英雄岭页岩岩相特征及有利源储组合

柴达木盆地英雄岭页岩油具有良好的形成与富集条件,石油资源量可达44.5×10^(8) t,但英雄岭页岩油纵向分布厚度大(>1000m),页岩岩相及岩相组合变化较大,给页岩油的有效勘探开发带来了巨大挑战。以英雄岭页岩典型井柴2-4、柴906、柴12等12口井578m岩心为研究对象,开展岩石学、有机地球化学和储层特征分析。研究表明,英雄岭页岩混积特征明显,矿物组成以方解石、白云石和黏土矿物为主;沉积构造以厚度小于1cm的纹层为主。根据“二元”命名原则,可将研究区内页岩岩相划分为5类,包括纹层状灰云岩、纹层状云灰岩、层状灰云岩、层状云灰岩、纹层状黏土质页岩。通过对各类岩相有机地球化学和储集性能综合评价,认为纹层状云灰岩为最优烃源岩相类型,层状灰云岩为最优储层相类型,储集空间主要为白云石晶间孔。甜点综合评价结果和生产实践证实,层状灰云岩与纹层状云灰岩互层为最有利的源储组合模式,各甜点段平面上连通性较好,纵向上具有较强的非均质性。

陆相断陷咸化湖盆细粒沉积岩特征及沉积环境——以泌阳凹陷核桃园组H3Ⅲ亚段为例

泌阳凹陷作为国内典型的陆相断陷咸化湖盆,在古近系核桃园组三段广泛发育细粒沉积岩。文中利用长井段连续取心资料以及薄片观察、二维XRF扫描、XRD分析、扫描电镜以及地球化学测试等手段,以矿物组分、沉积构造和粒度作为主要依据,把泌阳凹陷H3Ⅲ亚段细粒沉积岩划分为9种岩相类型,其中纹层状混合质页岩、纹层状长英质页岩是发育类型最多的细粒沉积岩;通过Mg/Ca、Al含量、Ti含量、(Fe+Al)/(Ca+Mg)、P/Ti、Sr/Ba和V/(V+Ni)等地球化学指标的垂向变化及岩相组合来分析沉积环境的演化特征。泌阳凹陷H3Ⅲ亚段沉积环境是半深湖—深湖环境,水体盐度为半咸水—咸水,陆源输入总体较强,气候变化相对较大,从下到上经历了干旱、干湿交替、湿润以及干旱的气候变化。岩相的垂向变化受气候、陆源输入、水深、水体盐度的影响,气候、陆源输入、水深决定了长英质矿物和黏土矿物的含量,而碳酸盐矿物的含量主要受到水体盐度和气候的影响。

川东南页岩气储层的岩石物理特征分析

四川盆地志留系龙马溪组页岩因富含有机质、埋藏深度适中的特点,已成为国内页岩气勘探的主要层位之一。页岩气储层非均质性强,物性参数所表现出的各向异性及脆性特征会受到多种因素的影响,不利于勘探中的测井解释和地震“甜点”的预测。基于以上原因,在四川长宁双河、重庆华蓥山三百梯等野外地质露头剖面采集页岩样品,利用X射线衍射分析页岩的矿物成分及含量,在实验条件下研究围压和温度的变化对地震速度的影响,确定地震速度与矿物成分的关系,以及页岩各向异性参数的变化规律。研究成果在一定程度上揭示了川东南地区含气储层黏土含量对页岩各向异性和脆性的控制作用,并总结出各向异性参数变化的经验关系,从而为岩石物理建模、各向异性参数反演以及脆性评价等提供地质依据。

储层温度对页岩微观力学性质的影响

深部页岩气储层温度较高,为了研究地层温度对页岩宏微观力学性质的影响,采用四川盆地长宁区块寒武系龙马溪组井下页岩岩心,开展了26℃、80℃、150℃条件下的网格式微米压痕实验,分别模拟地表、中深层与深部储层的环境温度。采用去卷积数据统计分析方法量化了温度对页岩微观力学性质的影响,结合能量分析法研究了温度对页岩微观尺度断裂韧性的影响规律,并分析了温度对深部页岩裂缝导流能力影响的作用机制。结果表明,随着深部储层温度的增加,显著削弱了页岩的微观弹性模量、硬度与断裂韧性,而增加了压痕点弹性变形能力;弹性变形能力的增强导致矿物簇受应力作用后具有恢复弹性形变的能力,进一步说明水力裂缝扩展后缝周矿物弹性形变易恢复,压裂裂缝难维持。该研究结果对从岩石微观力学角度理解深部页岩气储层水力裂缝导流能力低提供了理论支持。