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A thermo-mechanical phase-field model for mixed-mode fracture and its application in rock-like materials 混合模式断裂的热机械相场模型及其在类岩材料中的应用
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-27 DOI: 10.1016/j.ijrmms.2024.105907
Thermally induced fracture is a common phenomenon for concrete and rock-like materials, which presents a significant challenge to numerical modelling. In this work, a thermo-mechanical model for mixed-mode fracture based on phase-field method is proposed. This approach overcomes the difficulties of modelling the thermally induced cracking process when it comes to complex fracture patterns. To simulate different failure modes in thermo-mechanical conditions, the model's constitutive expression includes a unified failure criterion that takes into account both tensile and shear strengths. The proposed formulation provides a length scale insensitive response for brittle materials such as rocks, although other prevalent phase-field theories for purely mechanical fracture can also be involved. The computational results of the representative examples for rock-like materials are highly consistent with prior findings. It demonstrates that the presented model can effectively reproduce the thermally induced cracking process for various cracking patterns, such as tensile, shear, and tensile-shear fractures, indicating the method's remarkable capabilities for further research.
热诱导断裂是混凝土和类岩材料的一种常见现象,这给数值建模带来了巨大挑战。本研究提出了一种基于相场法的混合模式断裂热机械模型。这种方法克服了复杂断裂模式下热致开裂过程建模的困难。为了模拟热机械条件下的不同破坏模式,模型的构成表达式包括一个统一的破坏准则,该准则同时考虑了拉伸强度和剪切强度。所提出的公式为岩石等脆性材料提供了对长度尺度不敏感的响应,尽管也可以涉及其他纯机械断裂的流行相场理论。岩石类材料代表性实例的计算结果与之前的研究结果高度一致。研究表明,所提出的模型可以有效地再现各种裂纹模式(如拉伸、剪切和拉伸剪切断裂)的热诱导裂纹过程,这表明该方法具有卓越的能力,值得进一步研究。
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引用次数: 0
Investigation on the pore size characteristics and mechanical properties of grouting materials scoured by flow water 流水冲刷灌浆材料的孔径特征和力学性能研究
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-25 DOI: 10.1016/j.ijrmms.2024.105923
Investigating the pore size characteristics and mechanical properties of the stone bodies formed by residual grout is crucial for understanding the authentic permeability and load-bearing capacity of grouting materials after being scoured by water flow. In this study, the pore size distribution, porosity, uniaxial compressive strength (UCS), and elastic modulus (E) of stone bodies formed by residual grout from polyacrylate latex-modified cement grouting material (PLMC) were systematically investigated, and pure cement grout (PC) as a control group. First, scouring tests were conducted on grouting materials with various water-to-cement ratios (w/c, 0.6–0.8) and polymer-cement ratios (p/c, 0–0.2) under different flow velocities (0–1 m/s). Subsequently, the pore size characteristics of stone bodies formed by residual grout under various conditions were studied via nuclear magnetic resonance test. Finally, the uniaxial compression tests were conducted to investigate the impact of water scouring on the mechanical properties of grouting materials, and the relationship between pore size characteristics and macro mechanical responses was analyzed. Results show that the stone bodies formed by residual grout compared to the non-scoured state develop mesopores and macropores, and the number of micropores also increased significantly. This porosity escalation results in a reduction in UCS and E. When the flow velocity reaches 1 m/s, the porosity of PLMC with w/c = 0.8 increases by 2.95 %, while UCS decreases by 14.6 % and E decreases by 37.4 %. PC demonstrates more pronounced changes, with a porosity increase of 7.01 %, UCS decreases by 32.9 %, and E decreases by 41.5 %. With the rise in w/c, the deterioration of pore structure and mechanical properties of the stone bodies formed by residual grout is more significant compared to the non-scoured state. Increasing p/c can mitigate the deterioration of the pore structure and mechanical properties. The findings provide meaningful guidance for the grouting reinforcement under dynamic water conditions.
研究残余灌浆料形成的石体的孔径特征和力学性能,对于了解灌浆材料经水流冲刷后的真实渗透性和承载能力至关重要。本研究系统研究了聚丙烯酸酯胶乳改性水泥灌浆材料(PLMC)残留灌浆料形成的石体的孔径分布、孔隙率、单轴抗压强度(UCS)和弹性模量(E),并以纯水泥灌浆料(PC)作为对照组。首先,对不同水灰比(w/c,0.6-0.8)和聚合物水泥比(p/c,0-0.2)的灌浆材料在不同流速(0-1 m/s)下进行了冲刷试验。随后,通过核磁共振测试研究了不同条件下残余灌浆料形成的石体的孔径特征。最后,通过单轴压缩试验研究了水冲刷对灌浆材料力学性能的影响,并分析了孔径特征与宏观力学响应之间的关系。结果表明,与未冲刷状态相比,残留灌浆料形成的石体会产生中孔和大孔,微孔数量也显著增加。当流速达到 1 米/秒时,w/c = 0.8 的 PLMC 的孔隙率增加了 2.95%,而 UCS 减少了 14.6%,E 减少了 37.4%。PC 的变化更为明显,孔隙率增加了 7.01%,UCS 减少了 32.9%,E 减少了 41.5%。与未浇注状态相比,随着 w/c 的增加,残留灌浆料形成的石体的孔隙结构和机械性能的劣化更为显著。提高 p/c 可以缓解孔隙结构和机械性能的恶化。研究结果为动水条件下的灌浆加固提供了有意义的指导。
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引用次数: 0
Effects of crystal orientation, temperature, deviatoric stress, and confining stress on creep of rock salt 晶体取向、温度、偏差应力和约束应力对岩盐蠕变的影响
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-24 DOI: 10.1016/j.ijrmms.2024.105913
The creep of rock salt greatly influences the performance and safety of rock salt caverns when they are used as an underground repository for oil, nuclear waste, or other hazardous materials. Creep may cause shearing of casings of oil wells drilled through thick layers of salt rock formation. The crystallographic structure of salt rock grains, in-situ deviatoric stress changes caused by excavation, confining stress from the surrounding environment, and ambient temperature can have a significant impact on the creep behavior of rock salt. Although the creep behavior of polycrystalline rock salt has been extensively studied by many researchers, the creep behavior of single-crystal natural rock salt is not yet fully understood. This paper investigates the influence of crystal orientation, temperature, deviatoric stress, and confining stress on the creep behavior of single-crystal and polycrystalline rock salt. 42 long-term creep experiments with various temperatures, confining stresses, and deviatoric stresses were conducted on natural single-crystal specimens. The temperatures were 20, 100, and 150 °C, the confining stresses were 0.1, 1.0, and 5.0 MPa, and the various deviatoric stresses were applied in different loading directions with respect to the specimen's crystal orientations. Additionally, 18 long-term creep experiments were performed on synthetic polycrystalline specimens with wet grain boundaries at temperatures of 20, 100, and 150 °C, at confining stresses of 0.1, 1.0, and 5.0 MPa, and various deviatoric stresses. The effects of the mentioned experimental conditions on the accumulated axial strain, transient strain rate, and steady-state strain rate during the creep of rock salt were then examined and discussed in detail. Moreover, the influence of temperature, deviatoric stress, and confining stress on the steady-state creep of single crystal rock salt is examined within the context of existing polycrystalline creep data available in the literature.
当岩盐洞穴用作石油、核废料或其他有害物质的地下贮藏库时,岩盐的蠕变会极大地影响岩盐洞穴的性能和安全。蠕变可能会导致钻过厚盐岩层的油井套管发生剪切。盐岩晶粒的晶体结构、挖掘造成的原位偏差应力变化、周围环境的约束应力以及环境温度都会对岩盐的蠕变行为产生重大影响。虽然许多研究人员已经对多晶岩盐的蠕变行为进行了广泛研究,但对单晶天然岩盐的蠕变行为还没有完全了解。本文研究了晶体取向、温度、偏差应力和约束应力对单晶和多晶岩盐蠕变行为的影响。在天然单晶试样上进行了 42 次不同温度、约束应力和偏差应力的长期蠕变实验。温度分别为 20、100 和 150 °C,约束应力分别为 0.1、1.0 和 5.0 MPa,各种偏差应力施加在与试样晶体方向不同的加载方向上。此外,还对具有湿晶界的合成多晶试样进行了 18 次长期蠕变实验,温度分别为 20、100 和 150 °C,约束应力分别为 0.1、1.0 和 5.0 MPa,并施加了各种偏差应力。然后详细研究和讨论了上述实验条件对岩盐蠕变过程中累积轴向应变、瞬态应变率和稳态应变率的影响。此外,还结合文献中现有的多晶蠕变数据,研究了温度、偏差应力和约束应力对单晶岩盐稳态蠕变的影响。
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引用次数: 0
Acoustic emission and 4D X-ray micro-tomography for monitoring crack propagation in rocks 用于监测岩石裂缝扩展的声发射和 4D X 射线微断层扫描技术
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-22 DOI: 10.1016/j.ijrmms.2024.105917
Acoustic emission (AE) and 4D X-ray computed tomography (4D XCT) were used simultaneously to study crack initiation and propagation in two different types of quartz-rich sandstones during the four-point bending experiments. Statistical analysis of the AE response indicated the failure mechanisms and their dynamics. The characteristic changes observed in the AE response defined the timing of the bending interruptions for XCT scanning to reveal the development of the crack. It was possible to quantitatively describe the developing cracks in their dimensions and volume and relate this information to the rate of decrease in the post-peak region of the material response. It could be concluded that the combination and concurrent use of AE and XCT techniques represents a highly effective and reliable instrument for observation, description, analysis of the crack propagation process, and rock disintegration in detail at a microscale level. With regard to the specific sandstones studied, Mšené sandstone is softer, respectively, less brittle, while Kocbeře sandstone is characterised by a more brittle behaviour accompanied by an AE signal with higher amplitudes compared to those of Mšené.
在四点弯曲实验中,同时使用声发射(AE)和四维 X 射线计算机断层扫描(4D XCT)来研究两种不同类型富含石英的砂岩中裂纹的产生和扩展。对 AE 响应的统计分析显示了破坏机制及其动态变化。在 AE 响应中观察到的特征变化确定了 XCT 扫描显示裂纹发展的弯曲中断时间。可以定量描述裂纹发展的尺寸和体积,并将这些信息与材料响应峰值后区域的下降率联系起来。可以得出结论,AE 和 XCT 技术的结合和同时使用是一种非常有效和可靠的仪器,可用于观察、描述和分析裂纹扩展过程,以及岩石在微观层面上的详细崩解情况。就所研究的特定砂岩而言,Mšené 砂岩较软,脆性较低,而 Kocbeře 砂岩的特点是脆性较高,与 Mšené 砂岩相比,AE 信号的振幅较高。
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引用次数: 0
Grading scalping and sample size effects on critical shear strength of mine waste rock through laboratory and in-situ testing 通过实验室和原位测试,分级标度和样本大小对矿山废石临界剪切强度的影响
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-21 DOI: 10.1016/j.ijrmms.2024.105915

Geotechnical stability analyses of mine waste rock (WR) piles require the critical friction angle (ϕcr) of the coarse blasted rock. However, due to the presence of oversized rock clasts, shear strength can only be characterized on small samples prepared using grading scaling techniques, such as scalping. Thus, considering a testing device able to handle samples of characteristic size D, the material should be scaled down to a maximum particle size dmax given by the minimum sample aspect ratio α = D/dmax. However, a practical concern about how far the size scale can be reduced while keeping representative results remains a matter of debate in the geotechnical community. International standards do not agree on the minimum recommended α, and its effects on the mechanical behavior remain poorly understood. This paper aims to investigate the grading effects and sample size effects on ϕcr of WR materials using the scalping technique, to provide insights on the minimum recommended α. Triaxial tests were conducted on loose and dense samples of diameters D = 150 and 300 mm. Samples were scalped from field material having dmax = 75 mm, to allow a range of α from 4 to 30. Additionally, one of the world largest in-situ direct shear boxes (120 × 120 × 38 cm3) was developed to test the same WR material. The results show that scalping is an appropriate technique to assess the critical shear strength of WR. The minimum α for ϕcr assessment in triaxial testing is not sensitive to grading nor sample size, but it is affected by sample density. The aspect ratio was found to be α ≥ 12 and α ≥ 16 for loose and dense samples, respectively. This finding advocates that α values recommended by worldwide standards, such as ASTM D7181-20, might be too low and should be revisited after comprehensive testing.

矿山废石(WR)桩的岩土稳定性分析需要粗爆破岩石的临界摩擦角(jcr)。然而,由于存在过大的岩石碎块,只能通过分级缩放技术(如缩放)制备的小样本来确定剪切强度。因此,考虑到测试设备能够处理特征尺寸为 D 的样品,材料应按比例缩小到最大粒度 dmax,该粒度由最小样品长宽比 α = D/dmax 给出。然而,在岩土工程界,如何在保持结果代表性的同时缩小粒度仍是一个值得关注的实际问题。国际标准并未就推荐的最小值 α 达成一致,而且人们对其对力学行为的影响仍知之甚少。本文旨在利用剥离技术研究 WR 材料的级配效应和样本大小对 ϕcr 的影响,从而为推荐的最小 α 提供见解。样品是从 dmax = 75 毫米的现场材料中剥取的,因此 α 的范围在 4 到 30 之间。此外,还开发了世界上最大的原位直接剪切箱(120 × 120 × 38 立方厘米)之一,以测试相同的 WR 材料。结果表明,缩放是评估 WR 临界剪切强度的一种适当技术。在三轴测试中评估ϕcr 的最小 α 对级配和样品大小不敏感,但会受到样品密度的影响。研究发现,松散和致密样品的长宽比分别为 α ≥ 12 和 α ≥ 16。这一发现表明,ASTM D7181-20 等世界标准推荐的 α 值可能过低,应在全面测试后重新考虑。
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引用次数: 0
A novel method for evaluating stability and mechanism of flexural toppling based on energy conservation principle and numerical simulation 基于能量守恒原理和数值模拟的新型挠性倾覆稳定性和机理评估方法
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-21 DOI: 10.1016/j.ijrmms.2024.105896
The flexural toppling occurring in anti-dip layered slopes exhibits complex mechanical behaviours and poses a serious threat to human engineering practices. In this paper, a novel method for evaluating the stability of flexural toppling is proposed by combining analytical solution and numerical simulation. The anti-dip rock layers in the slope are regarded as inclined slabs, and the deflection equations of each rock slab are calculated when the slab at the basal plane is restrict and that at the top is free. Critical length of the rock slab is then determined with the energy conservation principle, and it can be employed to evaluate the stability of flexural toppling. Numerical simulations have been conducted to validate the present calculation method and explore the mechanisms of flexural toppling. The simulation results indicate that failure initially occurs at the slope toe due to strong stress concentration, subsequently triggering a domino effect with failures propagate to the upper rock slabs as a result of the loss of support from the lower ones. These simulation results also combined with the analytical solution enhance the calculation accuracy of the method. This innovative approach not only advances our understanding of flexural toppling mechanisms but also provides a method for practical stability assessments.
抗倾覆层状斜坡发生的挠曲倾覆表现出复杂的力学行为,对人类工程实践构成严重威胁。本文通过分析求解和数值模拟相结合的方法,提出了一种新型的挠曲倾覆稳定性评估方法。将斜坡中的抗倾覆岩层视为倾斜岩板,计算基面岩板受限和顶面岩板自由时每块岩板的挠度方程。然后根据能量守恒原理确定岩板的临界长度,并可用于评估挠曲倾覆的稳定性。为了验证本计算方法并探索挠曲倾覆的机理,我们进行了数值模拟。模拟结果表明,由于应力高度集中,崩塌最初发生在坡脚,随后引发多米诺骨牌效应,由于下部岩板失去支撑,崩塌向上部岩板蔓延。这些模拟结果与分析解决方案相结合,提高了该方法的计算精度。这种创新方法不仅加深了我们对挠性倾覆机制的理解,还为实际稳定性评估提供了一种方法。
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引用次数: 0
Supervised domain adaptation in prediction of peak shear strength of rock fractures 岩石裂缝峰值剪切强度预测中的监督域适应
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-20 DOI: 10.1016/j.ijrmms.2024.105921

It is of great importance to determine peak shear strength (PSS) of rock fractures, and data-driven criteria have showed advances in fitting capability in recent years. However, the generalization ability of existing data-driven criteria is limited by dataset size and fracture roughness characterization, which is negative to predictive power and robustness of models. Here we proposed a novel data-driven criterion to predict PSS of rock fractures, with high generalization ability on real experimental data. We first created large-scale low-fidelity dataset by discrete-element modeling, and small-scale high-fidelity dataset by laboratory direct shear tests. The numeric features include normal stress, mechanical properties (including PSS of intact and flat-fracture rock specimens), secondary properties (including internal friction angle, cohesion strength and basic friction angle), and the matrixed feature is topography data. We then established domain adaptation (DA) models for cross-domain knowledge transfer between the low- and high-fidelity datasets, and roughness features were automatically extracted by convolution kernels. The best DA-based model is weighting adversarial neural network, outranking other models by error indicator, and the average relative error on experimental data of new rock types is within 10.0 %. Finally, the sensitivity of input features is investigated, which further proves the promising potential of the developed data-driven PSS criterion of rock fractures in engineering practice.

确定岩石裂缝的峰值剪切强度(PSS)非常重要,近年来数据驱动标准在拟合能力方面取得了进步。然而,现有数据驱动准则的泛化能力受到数据集大小和断裂粗糙度特征的限制,这对模型的预测能力和稳健性不利。在此,我们提出了一种新颖的数据驱动准则来预测岩石裂缝的 PSS,该准则在真实实验数据上具有较高的泛化能力。我们首先通过离散元建模创建了大规模低保真数据集,并通过实验室直接剪切试验创建了小规模高保真数据集。数值特征包括法向应力、力学性质(包括完整和平断裂岩石试样的 PSS)、次要性质(包括内摩擦角、内聚强度和基本摩擦角),矩阵特征为地形数据。然后,我们建立了领域适应(DA)模型,用于低保真和高保真数据集之间的跨领域知识转移,并通过卷积核自动提取粗糙度特征。基于 DA 的最佳模型是加权对抗神经网络,其误差指标优于其他模型,对新岩石类型实验数据的平均相对误差在 10.0% 以内。最后,研究了输入特征的敏感性,这进一步证明了所开发的数据驱动岩石裂缝 PSS 准则在工程实践中的巨大潜力。
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引用次数: 0
Damage quantification and failure prediction of rock: A novel approach based on energy evolution obtained from infrared radiation and acoustic emission 岩石的损伤量化和失效预测:基于红外辐射和声发射能量演变的新方法
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-19 DOI: 10.1016/j.ijrmms.2024.105920

Rock failure under external force is a process of energy conversion between the external environment and the rock system. This study aims to quantify rock damage and predict failure from an energy perspective. Infrared radiation (IR) and acoustic emission (AE) technologies were used to monitor the failure process of red sandstone during uniaxial loading experiments in real time. The energy evolution law during the rock failure process was analyzed. Based on the Stefan–Boltzmann law, a quantitative parameter, average cumulative radiation energy increment (ΔACRE), was proposed for IR indicators. A coupling mathematical model between elastic strain energy and ΔACRE was derived. The correlation between cumulative AE energy and dissipated strain energy was also analyzed. Results reveal that the rock failure process can be divided into four stages according to energy evolution: compaction, elastic, elastic–plastic, and failure stages. The proposed ΔACRE can serve as a basis for dividing these stages. A cubic polynomial relationship was found between ΔACRE and elastic strain energy. AE cumulative energy and dissipated strain energy showed similar variation trends. Furthermore, based on ΔACRE, AE cumulative energy, and energy evolution theory, a failure prediction indicator (IRAEER) was proposed. This indicator can effectively identify precursor points of rock failure. A quantitative indicator for rock damage evolution under combined IR and AE action was created using IRAEER as the characterization parameter of the rock damage variable, demonstrating high reliability. This research provides strong support for estimating rock states and guiding the design of rock engineering structures.

岩石在外力作用下的破坏是外部环境与岩石系统之间的能量转换过程。本研究旨在从能量角度量化岩石破坏并预测破坏情况。利用红外辐射(IR)和声发射(AE)技术实时监测红砂岩在单轴加载实验中的破坏过程。分析了岩石破坏过程中的能量演变规律。基于斯蒂芬-玻尔兹曼定律,提出了红外指标的定量参数--平均累积辐射能量增量(ΔACRE)。得出了弹性应变能和ΔACRE之间的耦合数学模型。此外,还分析了累积 AE 能与耗散应变能之间的相关性。结果表明,根据能量演化,岩石破坏过程可分为四个阶段:压实阶段、弹性阶段、弹塑性阶段和破坏阶段。提出的 ΔACRE 可以作为划分这些阶段的依据。研究发现,ΔACRE 与弹性应变能之间存在立方多项式关系。AE 累积能和耗散应变能表现出相似的变化趋势。此外,基于ΔACRE、AE累积能和能量演化理论,提出了一种故障预测指标(IRAEER)。该指标可有效识别岩石破坏的前兆点。利用 IRAEER 作为岩石破坏变量的表征参数,创建了红外和 AE 联合作用下岩石破坏演化的定量指标,显示出较高的可靠性。这项研究为估计岩石状态和指导岩石工程结构设计提供了有力支持。
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引用次数: 0
Implicit hydromechanical representation of fractures using a continuum approach 利用连续体方法对骨折进行隐含的水力学表示
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-19 DOI: 10.1016/j.ijrmms.2024.105916

Fractures control fluid flow, solute transport, and mechanical deformation in crystalline media. They can be modeled numerically either explicitly or implicitly via an equivalent continuum. The implicit framework implies lower computational cost and complexity. However, upscaling heterogeneous fracture properties for its implicit representation as an equivalent fracture layer remains an open question. In this study, we propose an approach, the Equivalent Fracture Layer (EFL), for the implicit representation of fractures surrounded by low-permeability rock matrix to accurately simulate hydromechanical coupled processes. The approach assimilates fractures as equivalent continua with a manageable scale (≫1 μm) that facilitates spatial discretization, even for large-scale models including multiple fractures. Simulation results demonstrate that a relatively thick equivalent continuum layer (in the order of cm) can represent a fracture (with aperture in the order of μm) and accurately reproduce the hydromechanical behavior (i.e., fluid flow and deformation/stress behavior). There is an upper bound restriction due to the Young's modulus because the equivalent fracture layer should have a lower Young's modulus than that of the surrounding matrix. To validate the approach, we model a hydraulic stimulation carried out at the Bedretto Underground Laboratory for Geosciences and Geoenergies in Switzerland by comparing numerical results against measured data. The method further improves the ability and simplicity of continuum methods to represent fractures in fractured media.

裂缝控制着晶体介质中的流体流动、溶质传输和机械变形。它们可以通过等效连续体进行显式或隐式数值建模。隐式框架意味着较低的计算成本和复杂性。然而,如何将异质断裂属性提升为等效断裂层的隐式表示仍然是一个未决问题。在本研究中,我们提出了一种方法--等效断裂层(EFL),用于隐式表示被低渗透性岩石基质包围的断裂,以精确模拟水力机械耦合过程。该方法将裂缝同化为尺度可控(≫1 μm)的等效连续体,有利于空间离散化,即使是包括多条裂缝的大型模型也不例外。模拟结果表明,相对较厚的等效连续层(约厘米)可以代表断裂(孔径约 μm),并准确再现水力学行为(即流体流动和变形/应力行为)。由于等效断裂层的杨氏模量应低于周围基体的杨氏模量,因此存在一个杨氏模量上限限制。为了验证该方法,我们在瑞士贝德雷托地球科学与地质能源地下实验室模拟了一次水力压裂,并将数值结果与测量数据进行了对比。该方法进一步提高了连续介质方法表示断裂介质中裂缝的能力和简便性。
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引用次数: 0
Fracability evaluation model for unconventional reservoirs: From the perspective of hydraulic fracturing performance 非常规储层可压裂性评价模型:从水力压裂性能的角度
IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL Pub Date : 2024-09-19 DOI: 10.1016/j.ijrmms.2024.105912

Fracability evaluation for unconventional reservoir is critical to the selection of candidate zones for post-frac productivity and plays a key role in fracturing design. Historically, the prevailing models for assessing fracability have been largely relied on brittleness indices. Brittleness indices focus mainly on rock fracture characteristics and offers limited assessment of fracture surface area and the complexity of fracture network, which are more relevant to the practical production. We explored a new fracability evaluation model for unconventional reservoirs from the perspective of fracturing performance, which comprehensively characterizes the rock's ability to generate larger fracture surface areas, more shear fractures and complex fracture networks. The new fracability index considers both the physical processes of rock failure and fracture propagation, and is directly associated with the dynamic production capacities of reservoir. According to the analysis of energy conservation during hydraulic fracturing, we quantify the rock fracture surface area using the KGD and the PKN models. The ability of rock formation to generate shear fractures is mainly influenced by Poisson's ratio and mode II fracture toughness. Brittle mineral content and mineral heterogeneity are two vital criteria that significantly affect the complexity of fracture networks. Based on the logging and production data, this fracability model was applied to two types of unconventional reservoirs. Preliminary results show that this fracability model has an improved correlation with the pay zones and actual production, which is beneficial for optimizing fracturing strategies and identifying production sweet spots.

非常规储层的可压裂性评估对于选择压裂后产能的候选区域至关重要,在压裂设计中也起着关键作用。一直以来,评估压裂性的主流模型主要依赖于脆性指数。脆性指数主要侧重于岩石裂缝特征,对裂缝表面积和裂缝网络复杂性的评估有限,而这与实际生产更为相关。我们从压裂性能的角度探索了一种新的非常规储层可压裂性评价模型,该模型综合表征了岩石产生更大压裂表面积、更多剪切裂缝和复杂裂缝网络的能力。新的压裂性能指标同时考虑了岩石破坏和裂缝扩展的物理过程,与储层的动态生产能力直接相关。根据水力压裂过程中的能量守恒分析,我们利用 KGD 和 PKN 模型对岩石裂缝表面积进行了量化。岩层产生剪切裂缝的能力主要受泊松比和模式 II 断裂韧性的影响。脆性矿物含量和矿物异质性是显著影响断裂网络复杂性的两个重要标准。根据测井和生产数据,该压裂性模型被应用于两类非常规储层。初步结果表明,该压裂性模型与含油层和实际产量的相关性有所提高,有利于优化压裂策略和确定产量甜点。
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International Journal of Rock Mechanics and Mining Sciences
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