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Quantifying the Fracture Mechanics Properties of Rock for Fractured Reservoir Characterization

机译:量化岩石的断裂力学特性用于裂缝性储层表征

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Natural fractures are important conduits for fluid-flow and canrncontrol the deformational behavior of rock. The accuraternevaluation of natural fracture geometry in the subsurface isrndifficult because of the sampling problems inherent tornwellbores and indirect investigation methods such as seismic.rnBecause of these limitations in observational capability,rnpredictive models are needed to provide more constraint onrnnatural fracture characteristics. One approach is to look at thernmechanics of fracture propagation in sedimentary rock asrncontrolled by subcritical crack growth (also known as stresscorrosionrncracking). We have measured the subcriticalrnfracture properties of numerous sedimentary rocks, includingrncore samples from petroleum reservoirs, in conjunction withrndetailed petrographic analysis. Our preliminary resultsrnsuggest that carbonates and sandstones tend to have veryrndifferent subcritical fracture properties, and the variation inrnsandstone properties can be linked to grain and cementrnmineralogy and volume fractions.
机译:天然裂缝是流体流动的重要管道,可以控制岩石的变形行为。由于井筒固有的采样问题和诸如地震等间接调查方法的存在,地下天然裂缝几何形状的准确评估是困难的。由于观测能力的这些限制,需要预测模型来对自然裂缝特征提供更多的约束。一种方法是研究受亚临界裂纹扩展(也称为应力腐蚀裂纹)控制的沉积岩中裂缝传播的力学机制。我们结合详细的岩相学分析,测量了许多沉积岩的亚临界断裂特性,包括来自石油储层的岩心样品。我们的初步结果表明碳酸盐岩和砂岩倾向于具有非常不同的亚临界断裂特性,并且砂岩特性的变化可能与颗粒和水泥的矿物学和体积分数有关。

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