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The influence of CO_2 gas and carbonate water on the mechanical stability of chalk

机译:CO_2气体和碳酸盐水对白垩力学稳定性的影响

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The mechanical strength of high porosity chalk is affected by using carbonate water as EOR (Enhanced Oil Recovery) fluid.The water-weakening effect is enhanced due to increased dissolution of chalk in the presence of CO_2(aq).In this study,the mechanical properties of chalk were compared with and without CO_2(aq) present in the injected water.By use of a standard triaxial cell,series of samples with and without pre-flooding at confining pressure of 0.5-1.0 MPa were hydrostatic loaded up to yield point at room temperature or 90 deg C.Then a major part of the samples were exposed to subsequent creep and flooding phases at increased stress levels of about 2 MPa above yield point.In all cases flooding experiments were performed without any backpressure and with flooding pressure varying between 0.2 and 0.8 MPa.Injection of pure CO_2 gas into water-saturated chalk resulted in only marginal weakening of the chalk material.At stress levels below the yield point,the chalk exposed to carbonate water becomes considerably weaker than chalk flooded with pure Eq.Water.At a given flooding pressure of carbonate water,an increase in temperature to 90 deg C improved the chalk stability.Flooding with CO_2 saturated modified seawater,which contained an enhanced concentration of sulfate,increased the strain significantly due to the precipitation of CaSO_4 centre dot 2H_2O(s).The preferential oil-wet cores at S_(or)=0.62 experienced an increased strain of 20% compared to the water-wet test series during flooding with CO_2-saturated Eq.water.Increasing the confining pressure by a factor of 10,strain values of about 10 times higher or even more were observed when flooding with carbonate water.The experimental observations are discussed in terms of chemical and pressure dissolution of chalk.
机译:高孔隙度白垩的机械强度受到碳酸盐水作为EOR(提高采油率)流体的影响。由于在CO_2(aq)存在下白垩的溶解度增加,水的弱化作用得到增强。比较了注入水中是否存在CO_2(aq)的白垩性质。通过使用标准三轴池,在0.5-1.0 MPa的围压下对一系列有或没有预注水的样品进行静水加载直至屈服点然后在室温或90摄氏度下将大部分样品暴露在随后的蠕变和驱替阶段,并在高于屈服点的约2 MPa的应力水平下进行暴露。在所有情况下,均进行了驱替实验,没有任何背压且驱替压力变化在0.2至0.8 MPa之间。将纯CO_2气体注入到水饱和的白垩中只会导致白垩材料的边缘减弱。在低于屈服点的应力水平下,白垩暴露于碳酸盐中水变得比用纯方程式水淹没的白垩弱得多。在给定的碳酸水注水压力下,温度升高到90摄氏度会改善白垩的稳定性。用CO_2饱和的改性海水淹没,其中硫酸盐的浓度增加,由于CaSO_4中心点2H_2O(s)的沉淀,使应变显着增加。与CO_2-驱油过程中的水湿试验系列相比,S_(or)= 0.62处的优先油湿岩心经历了20%的应变增加。用碳酸水注水时,观察到的围压增加了10倍,应变值提高了约10倍甚至更多。从化学和粉笔的溶解度方面对实验观察进行了讨论。

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