枯竭气藏注CO2热致压裂起裂作用的分析方法

T. Huijskes, J. D. de Kok
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引用次数: 0

摘要

在二氧化碳注入过程中,近井冷却和压力积聚可能导致储层岩石破裂。这些裂缝会影响注入能力,并对流动保障产生重大影响。本文提出了一种快速简便的评价热致压裂起裂程度的方法。本文从地质力学理论和衰竭储层最小水平应力表达式入手。描述了热孔弹性应力与热裂起裂判据之间的关系。热应力部分采用了井筒周围应力的简化解析解,考虑了近井冷却和远场原始温度条件的差异。采用类似的方法来适应近井区域和远井区域之间的压力差。利用一组地质力学参数和储层参数建立诊断图进行评价。讨论了耗尽应力路径与注入应力路径差异的后果。最后,将结果与数值油藏模拟结果进行了比较。通过对比分析结果和数值结果,对热应力修正系数进行了校核和调整。初步迹象表明,这一几何因素和推导出的等效冷区半径在许多情况下是成立的。讨论了热压裂对几种储层和岩石参数的敏感性。所建立的解析方法快速、简单,结果与数值模拟结果相当,因此可以准确地估计断裂起裂力矩。由此产生的诊断图提供了一种快速而简单的替代地质力学模拟来评估裂缝起裂的可能性和时刻。这种方法可以帮助早期的可行性工作,并确定是否需要更详细的建模。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An Analytical Method for Estimation of Thermal Fracturing Initiation During CO2 Injection in Depleted Gas Reservoirs
During CO2 injection, cooling and pressure buildup in the near-wellbore may lead to fracturing of the reservoir rock. These fractures affect the injectivity and can have a significant impact on flow assurance. This paper presents the derivation of a quick and simple method to evaluate the onset of thermal fracturing. This paper starts with geomechanics theory and expressions of minimum horizontal stress in depleted reservoirs. It describes the relations between thermo-poro-elastic stress and the criterion for initiation of (thermal) fracturing. The thermal stress part uses a simplified analytical solution of the stresses around the wellbore taking into account differences due to near-wellbore cooling and far-field virgin temperature conditions. A similar methodology is used to accommodate for pressure difference between the near-wellbore area and the far-field. A set of geomechanical and reservoir parameters are used to set-up diagnostic plots for evaluation. Consequences of the difference between the depletion stress path and injection stress path are discussed. Finally, results are compared to numerical reservoir simulation results. A proposed thermal stress correction factor, which accounts for differences between a simple analytical solution and a full-field evaluation, is checked and adjusted by comparing analytical and numerical results. First indications show that this geometrical factor and the derived equivalent cold zone radius holds for many cases. The sensitivity of thermal fracturing for several reservoir and rock parameters is discussed. The analytical method found is quick, simple and generates equivalent results to the numerical simulator and is therefore assumed to be accurate for estimation of the moment of fracture initiation. The resulting diagnostic plots present a quick and simple alternative to geomechanical simulation for evaluating the possibility and moment of fracture initiation. This method can help in early-stage feasibility work and determine if more detailed modelling is needed.
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