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Evaluation of the stress sensitivity in tight reservoirs

机译:致密油藏应力敏感性评价

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The expressions of three types of stress sensitivity coefficients (S, α, β) are obtained on the basis of analysis of the empirical models and theoretical models on the relationships between permeability and effective stress, and the stress sensitivity evaluation standard is proposed considering experiment data and rock micro-structural features. Then the empirical models and theoretical models were used to fit experiment data of low-permeability and tight sandstones and different types of granites, which promotes the understanding of the empirical models and the physical meanings of the stress sensitivity coefficients. According to the study of the three types of stress sensitivity coefficients and the relationship of effective stress and permeability, it is found that the stress sensitive coefficient S is suitable for evaluating the stress sensitivity (strong stress sensitivity: S>0.40; low stress sensitivity: S<0.25; medium stress sensitivity: 0.25≤S≤0.4). Meanwhile, it is also found that strong-stress-sensitivity cores are more suitable to be characterized by the logarithmic model, while the exponential model (or binomial model) occurred more frequently in low-stress-sensitivity cores, and medium-stress-sensitivity cores are more likely to be described with the power model. Finally, the evaluation standard is discussed based on the micro-structure in the low-permeability and tight sandstones. The results show that the crack-like pores in the strong-stress-sensitivity cores are obvious, but low-stress-sensitivity cores have the characteristics of porous rocks; moreover, the types of cemented clay minerals, the size of rock grain and lithology have impact on stress sensitivity.
机译:在对渗透率与有效应力关系的经验模型和理论模型进行分析的基础上,获得了三种应力敏感性系数(S,α,β)的表达式,并结合实验数据提出了应力敏感性评价标准。和岩石的微观结构特征。然后采用经验模型和理论模型拟合低渗透性致密砂岩和不同类型花岗岩的实验数据,从而促进了对经验模型的理解以及应力敏感性系数的物理意义。通过对三种类型的应力敏感系数以及有效应力与渗透率之间关系的研究,发现应力敏感系数S适用于评估应力敏感度(强应力敏感度:S> 0.40;低应力敏感度: S <0.25;中等应力敏感性:0.25≤S≤0.4)。同时,还发现强应力敏感型岩心更适合用对数模型表征,而指数模型(或二项式模型)在低应力敏感型岩心和中应力敏感型岩心中更常见。内核更可能用功率模型来描述。最后,基于低渗致密砂岩的微观结构讨论了评价标准。结果表明,强应力敏感性岩心中的裂缝状孔隙明显,而低应力敏感性岩心具有多孔岩性。此外,胶结粘土矿物的类型,岩粒的大小和岩性对应力敏感性有影响。

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