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基于损伤理论的水力压裂人工裂缝应力场研究
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摘要
水力压裂施工是一个产层岩石中的各种孔洞和微裂纹等在强烈的压裂液作用下不断生长交叉并最终贯通汇合成宏观水力裂缝的过程,宏观裂纹以及岩石内生长的微裂纹组在一定程度上增加了储层的渗流体积进而提高了油气的渗流能力,同时也对整个岩石的力学性能造成了不可逆的损伤劣化。因此,完全可以借助损伤力学的研究方法和理论成果来对水力压裂施工过程中压裂液对地层岩体的这种劣化效果进行分析描述,进而能准确计算水力压裂裂缝的有效波及范围。
     本文结合使用损伤力学和断裂力学的研究方法和理论成果来描述压裂过程中压裂裂缝对储层岩体的损伤劣化效果,对深入研究裂缝的产生机制,解决实际工程问题有一定的指导意义和创新性。
     首先针对本文所使用的损伤力学的概念和理论进行简单介绍,重点论述了损伤变量的概念以及不同损伤变量的表述方法,对损伤力学的等效原理,尤其是等效应变原理进行分析和阐述;其次描述了压裂施工中裂缝周围岩石的受力特点,分析了岩石损伤的形成演化机理,在合理简化岩石的σ-ε曲线基础上,以此为前提并结合适当的假设推导出了基于损伤理论的地层岩石本构关系模型;假定岩体为双孔双渗介质,在综合考虑地应力场,渗流场的作用下,结合断裂力学理论,推导裂缝全场应力表达式,分析微元体受力,得出微分平衡方程;建立人工裂缝的损伤力学模型,将裂缝周围岩体划分为无损区、损伤区和破坏区,分别对各个区域的边界方程和应力状态进行计算求解,确定不同区域的延伸半径和岩体的应力分布,计算实际施工状态下裂缝的损伤应力状况并加以分析。
Hydraulic fracturing is a process in which a variety of holes and micro-crack growsunder the strong fracturing fluid cross and eventually through, into macro-hydraulic fractureand macroscopic crack growth within a rock micro crack group thereby increasing the seepa-ge of oil and gas reservoir seepage volume increased to a certain extent, but also cause irrev-ersible damage deterioration of the mechanical properties of the whole rock. With the researchmethods and theoretical results of the damage mechanics to hydraulic fracturing fracturingfluid in the construction process to analyze the effect of this degradation of the stratigraphicrock description, and thus can accurately calculate the effective spread range of hydraulicfractures.
     In this paper, the author used methods and theoretical results in damage mechanics andfracture mechanics to describe the fracturing process of fracturing the reservoir rock damagedeterioration effect on the mechanism of in-depth study of cracks, to solve practical engineer-ing problems with some guiding significance and innovation.
     First, a brief introduction to the concepts and theories of damage mechanics used in thisarticle, focusing on the formulation of the concept of the damage variable and damagevariable, the equivalence principle of damage mechanics, especially the analysis andelaboration of the equivalent strain principle; Second, it describes the mechanicalcharacteristics of the cracks in the rock surrounding the fracturing operation, a rock formationand evolution mechanism of injury, reasonable simplification σ-ε curve of rock on the basisof this premise, combined with appropriate assumptions derivation out based on the damagetheory of the formation rock constitutive model; assumed rock holes dual-permeability media,inthe considered stress field, seepage field effect, combined with fracture mechanics theoryderived expression of the cracks in the audience stress analysis element by the force, obtaineddifferential balance equations; damage mechanics model of artificial cracks, cracks thesurrounding rock mass is divided into non-destructive zone, damage zone and destruction zo-ne, all regions of the boundary equations and the stress state is calculated solving to determinethe different regions of extension of the radius and the stress distribution of the rock mass tocalculate the crackdamage stress conditions in the state of actual construction and analysis.
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