鄂尔多斯盆地天然裂缝性碳酸盐岩储层脆性评价研究及应用

Xinxing Ma, J. Kao, Zhou Zhou
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摘要

岩石脆性是影响地层破裂行为的关键因素。因此,在进行水力压裂时,对脆性进行评价是十分重要的。以往的研究提供了各种各样的岩石脆性评价方法。然而,由于这些方法没有综合考虑岩性、天然裂缝和溶洞的影响,因此很少有评价方法可以应用于天然裂缝的碳酸盐岩地层。为此,提出了一种综合评价碳酸盐岩天然裂缝性地层脆性的方法。本研究的岩石来自鄂尔多斯盆地的地层。脆性评价方法要求试验研究包括三轴压缩试验、连续强度试验、Kaiser试验和x射线衍射分析。在此基础上,分析了裂缝性碳酸盐岩中基质性质和缝洞的影响。在此基础上,提出了综合考虑岩石力学试验应力-应变曲线、地质微观特征和裂缝特征的碳酸盐岩脆性评价方法。该方法在鄂尔多斯盆地具有较好的应用前景。结果表明:围压作用下裂隙型碳酸盐岩破坏模式以剪切破坏为主;裂缝对岩石的强度有明显的影响。裂缝性碳酸盐岩的脆性表现为破裂前抗非弹性变形的能力和破裂后承载力的损失率,岩石的矿物成分和裂缝的发育程度都会影响其脆性。随着围压的增大,裂缝趋于闭合,导致脆性增大。而碳酸盐在高围压下表现为塑性,脆性降低。利用脆性系数对鄂尔多斯盆地天然裂缝性碳酸盐岩储层进行水力压裂设计。水力压裂是保证天然裂缝性碳酸盐岩地层成功开发的必要条件。因此,在水力压裂设计中,脆性评价方法值得研究。
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Study on the Brittleness Evaluation in the Naturally Fractured Carbonate Formation and Its Application in the Ordos Basin
Rock brittleness is a key factor to influence the fracture behavior in the formation. Therefore, it is important to evaluate the brittleness when doing the hydraulic fracturing. Previous studies provided various methods for rock brittleness evaluation. Few evaluations, however, could be applied for the naturally fractured carbonate formation because those methods did not integrate the influence from lithology, natural fractures and vugs. Hence, this paper indicated an integration evaluation method to investigate the brittleness in the naturally fractured carbonate formation. The rock in this study was from the formation in the Ordos Basin. The brittleness evaluation method asked the experiment studies that included triaxial compression test, continuous strength test, Kaiser test and X-Ray Diffraction analyze. Based on the results, the influence of substrate properties and fractures-vugs in fractured carbonate rock are analyzed. Then a method to evaluate the brittleness of fractured carbonate rock is raised in which the stress-strain curves of rock mechanics tests, geologic microcharacter and the characteristics of fractures are considered. The method can give a better application in Ordos Basin. The results show that the failure mode of fractured carbonate rock under the effect of confining pressure is mainly the shear failure. The facture will have an obvious effect on the strength of rock. The brittleness of fractured carbonate rock appears as the ability for resisting inelastic deformation before rupture and losing rate of bearing capacity after rupture, besides the minerals of rock and the development of fracture will influence the brittleness. With the increasing of confining pressure, the fractures tend to be closed which leads to the increasing of brittleness. However, the carbonate in high confining pressure is characterized by plasticity, the brittleness would reduce. The brittleness was used to design hydraulic fracturing work in the naturally fractured carbonate formation of Ordos Basin. Hydraulic fracturing is necessary to guarantee a successful development in the naturally fractured carbonate formation. Therefore, the brittleness evaluation method is worth to study when designing the hydraulic fracturing.
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